Environmental magnetic characterization of the sediments from shallow cores of Gulf of Kachchh, Gujarat, India

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Khan, Suvarna Naikuji This is a preprint; it has not been peer reviewed by a journal. https://doi.org/ 10.21203/rs.3.rs-6582332/v1 This work is licensed under a CC BY 4.0 License Status: Posted Version 1 posted You are reading this latest preprint version Abstract This study examines the environmental magnetic properties of 80 subsurface sediment samples from the mudflats along the Gulf of Kachchh coast, Gujarat, India. A 1.04-meter shallow core was obtained from ten distinct locations, considering the impact of anthropogenic activities on coastal sediments. Magnetic parameters were employed as proxies for assessing environmental pollution, particularly in identifying anthropogenic particles. The subsurface sediments in the Gulf of Kachchh (GOK) are primarily dominated by ferromagnetic minerals, likely magnetite. The χfd percentage indicates the presence of superparamagnetic/single-domain (SSD) magnetic minerals, while elevated ARM/SIRM values suggest a significant presence of SSD (magnetite) grains. Additionally, the SIRM/χ ratio indicates an absence of multidomain (MD) grains. This study demonstrates the utility of magnetic proxies in detecting regions with higher pollution levels, potentially associated with heavy metal contamination. Gulf of Kachchh anthropogenic rock magnetics Figures Figure 1 Figure 2 Figure 3 Figure 4 Introduction Environmental magnetism serves as an invaluable tool in the study of palaeoceanographic conditions, primarily because of its sharp sensitivity to both depositional processes and sedimentary diagenesis, particularly through the phenomenon of reductive dissolution, as documented by various studies (Larrasoaña et al., 2003b ; Roberts et al., 1999 ; Robinson et al., 2000 ; Tarduno & Wilkinson, 1996; van Hoof et al., 1993 ). The magnetic minerals present in marine sediments, which largely originate from detrital inputs, biomineralization, or subsequent post-depositional alterations of these sources, respond intricately to environmental fluctuations. This responsiveness not only underscores the utility of magnetic properties and grain size variations in these sediments as proxies for environmental changes but also facilitates the detailed characterization of geochemical environments and depositional regimes, thereby enriching our understanding of paleoceanographic dynamics (Hilgenfeldt, 2000 ; Just et al., 2012 ; Liu et al., 2012 a; Roberts et al., 2013 ; Rowan et al., 2009 ; Thompson & Oldfield, 1986 ). Iron-bearing minerals, known for their sensitivity to environmental changes, offer valuable insights due to their pronounced and indicative signatures, which can be detected even at low concentrations. These minerals are reliably utilized to characterize sediment provenance (Thompson and Oldfield, 1986 ; Dearing, 1999 ; Hatfield and Maher, 2009 ; Hatfield, 2014 ). Mineral magnetic measurements have proven effective across various geo-scientific applications, ranging from the reconstruction of paleoclimate and recent climate changes to foraminifera assemblages and environmental risk assessments. This method not only aids to identify the foraminiferal assemblage in subsurface sediments but also facilitates the exploration of relationships between magnetic domain size and physical particle size of sediments. Such insights are crucial for understanding hydrodynamic conditions, sediment transport and depositional pathways, diagenetic and authigenic changes, as well as anthropogenic impacts (Bloemendal et al., 1992 ; Sangode et al., 2007 ; Hatfield and Maher, 2009 ; Horng and Huh, 2011 ; Chaparro et al., 2008 , 2011 , 2015 ; Kulkarni et al., 2014 ; Sandeep et al., 2011 ; Chen et al., 2017 ; Liu et al., 2018 ; Hatfield et al., 2019 ). In similar way, magnetic particles, recognized for their extensive surface area, serve as efficient absorbers of various toxic metals, thereby enabling magnetic parameters to be employed as proxies in chemical analyses, particularly in environmental studies (Hoffmann et al., 1999; Kapicka et al., 2003 ; Petrovsky et al., 2000). The preferential absorption of heavy metals by iron oxides and hydroxides, as identified by Reimann and Caritat (2005), further emphasizes the utility of magnetic susceptibility (χ) measurements, which, despite their high natural variability, have been widely adopted as indicators of contamination. Moreover, in urban areas, χ measurements have proven particularly effective in assessing pollution from exhaust gases and industrial discharges, with the elevated χ values observed in marine sediments often attributable to fine-grained iron oxides originating from anthropogenic sources (Chan et al., 2001 ). The present work investigates magnetic characteristics of the sediments to determine the mineralogy and grain size of magnetic minerals in subsurface sediments of Gulf of Kachchh coast Study area The GoK (Gulf of Kachchh will here written as GoK )is a semi-closed basin in the northern Arabian Sea lying between 22°15´ to 23°N and 69° to 70°15´E along the west coast of India surrounded by Kachchh mainland in the north and Saurashtra horst in the south (Fig. 1). GoK divides Kachchh and the Kathiawar peninsula regions of Gujarat and is about 99 miles long. GoK exhibits a macro tidal environment with a tidal range of about 7 m at the head to 3 m at the mouth because of its peculiar shape. River Indus is placed at about 100 km north of GoK, which carries about 50 million tons of sediments yearly (Giosan et al ., 2006). GoK presently is a very active industrial hub with many small and large ports along the coasts such as Kandla, Adani, Mundra, Okha along with many pipelines, jetties, shipbuilding work, oil refineries, cement industries, etc. The high tidal flux at GoK covers vast low-lying areas of about 1500 km 2 in inner gulf encompassing a network of creeks, estuaries and mud flats (Govil and Naidu, 2008 ). Three main creeks namely Kandla, Hansthal and Nakti make up the creek system and the little GoK are interconnected through many large and small creeks (Chauhan and Vora, 1990 ). In GoK the intertidal expanse increases towards upstream. The increase is approximately from 0.5 to 2 km from Jakhau to Kandla and from around 1 km at Okha to over 10 km at Navlakhi (Chauhan and Vora, 1990 ). The GoK overall occupies area under low tidal mudflats is 1590 km 2 and high tidal mudflats is 586 km 2 (GIS, 2002). The GoK covers approximately 1500 km2 of low-lying areas, including creeks, estuaries, and mud flats Methodology Total 80 subsurface samples were collected from ten various mudflat localities, GoK namely (1) Salaya, (2) Sikka Port, (3) Bedi Port, (4) Jodiya, (5) Adani Port, (6) Navlakhi Port, (7) Kasampir, (8) Modhva, (9) Kandla Port and (10) Tuna Port. All the locations are from mudflats except Modhva which shows sandy beach. For subsurface sampling, 1m by 1m shallow core of square shaped ditch/trench was excavated with hand shovel. Samples were taken at regular intervals of 13 cm using measuring tape, thus in all total 8 samples were recovered from 1.04 m trench. In the course of laboratory investigations, approximately 9–10 grams of meticulously air-dried sediment were precisely packed into standard non-magnetic styrene containers, subsequently rendered airtight to maintain the physicochemical integrity of the samples throughout the entirety of the magnetic susceptibility measurements. The magnetic susceptibility (χ) assessments were conducted on both bulk sediment matrices and granulometrically segregated sediment fractions utilizing a high-sensitivity MFK1-FA Kappabridge (3×10⁻⁸ SI), operated at a low excitation frequency of 976 Hz and an applied alternating magnetic field intensity of 200 A/m. Anhysteretic remanent magnetization (ARM) was imparted to the bulk sediment specimens employing a Molspin spinner magnetometer under the influence of a unidirectional steady magnetic field of 0.05 mT, superimposed with a decaying alternating field. The ARM intensities were subsequently normalized with respect to the magnitude of the applied steady field and expressed as the anhysteretic remanent magnetization susceptibility (χARM), thereby facilitating inter-sample comparison. Isothermal remanent magnetization (IRM) acquisition was systematically executed on the bulk sediment samples via an ASC Impulse Magnetizer, wherein magnetization was induced in forward-directed magnetic fields of 40 mT and 1 T, followed by stepwise application of reverse (backfield) intensities at − 20, −30, − 40, −100, and − 300 mT. The resultant remanent magnetizations were quantified using the Molspin Spinner Magnetometer, ensuring high-resolution detection of coercivity distributions and magnetic mineralogy. Concomitantly, foraminiferal analysis necessitated a rigorous sample preparation protocol primarily encompassing the disaggregation and sieving of sediments. Each sample was transferred into a pre-labeled 1-liter beaker and subjected to overnight oxidation in hydrogen peroxide. A volume of 15–30 ml of a 15% hydrogen peroxide solution (diluted from a stock 30% concentration) was introduced to facilitate the degradation of organic constituents. Subsequently, the treated sediments underwent wet sieving through a series of ASTM-E11 standard mesh sieves—specifically, mesh numbers 20, 80, 140, and 230—enabling precise granulometric classification for downstream micropaleontological examination. Results and discussion The environmental magnetic parameters for bulk sediments from the Gulf of Kachchh (GOK), summarized in Table 1, are further detailed in Table 2 and graphically illustrated in Fig. 2. At Salaya port, the moderate ARM/χ ratios combined with relatively high SIRM/χ values indicate that the grain size predominantly falls within the single-domain (SD) to pseudo-single-domain (PSD) range, with magnetite likely being the dominant mineral. S. Port exhibits variations in ARM/χ and SIRM/χ ratios, suggesting a mixture of grain sizes from fine to coarse, with a significant presence of low-coercivity minerals. In contrast, B. Port's high ARM/χ ratios point to fine grains, while moderate SIRM/χ values indicate a mix of SD and multi-domain (MD) grains. Jodiya's ARM/χ ratios and SIRM/χ values similarly suggest the presence of fine-grained magnetic minerals, likely in the SD to small PSD range, with magnetite as the dominant mineral. Navlakhi stands out with extremely high χ values coupled with moderate ARM/χ ratios, indicating a large concentration of magnetite with varying grain sizes. Kasampir shows evidence of fine grains, as indicated by high ARM/χ and SIRM/χ values, with significant concentrations of low-coercivity minerals. At Kandla, the ARM/χ values suggest a prevalence of finer grains, likely in the SD range, along with moderate coercivity minerals. Tuna Port's ARM/χ values also indicate finer grains with significant low-coercivity mineral content. Adani Port, on the other hand, shows low to moderate ARM/SIRM values, suggesting a mix of fine and coarse grains with a dominance of magnetite. Lastly, Modhva's low ARM/SIRM values suggest the presence of coarser grains, possibly within the multi-domain range. Table No.1 : Various magnetic mineral parameters used in the present study Parameter Units Description Formula References Low frequency mass specific magnetic susceptibility (χlf) m³ kg⁻¹ Represents the concentration of bulk magnetic minerals in a sample. - Thompson and Oldfield (1986); Dearing (1999) Percentage frequency dependent susceptibility (χfd%) % Used to detect the presence of superparamagnetic (SP) ferrimagnetic particles. χfd% = [(χlf − χhf) / χlf] × 100 Maher (1986); Dearing (1999) Frequency dependent susceptibility (χfd) m³ kg⁻¹ Indicates the presence of ultrafine magnetic grains at the stable single domain (SD)/superparamagnetic (SP) boundary. χfd = (χlf − χhf) Thompson and Oldfield (1986); Maher (1986); Dearing et al. (1996); Dearing (1999) Saturation isothermal remanent magnetization (SIRM) Am² kg⁻¹ Highest level of magnetic remanence induced in a sample by a high magnetic field (commonly at 1 T). - Thompson et al. (1980); Thompson and Oldfield (1986) Susceptibility of anhysteretic remanent magnetization (χARM) m³ kg⁻¹ Sensitive to both concentration and grain size of ferrimagnetic minerals, particularly near the SP/SD boundary. - King et al. (1982); Thompson and Oldfield (1986) Hard isothermal remanent magnetization (HIRM) Am² kg⁻¹ Approximates the concentration of antiferromagnetic minerals in a sample. HIRM = 0.5 × (SIRM + IRM-300mT) Thompson and Oldfield (1986); Liu et al. (2007) S-ratio Dimensionless Indicates the relative abundance of low-coercivity and high-coercivity minerals in bulk samples. Values close to 1 indicate low-coercivity minerals, and values close to 0 or negative indicate high-coercivity minerals. S-ratio = -IRM-300mT / SIRM Stober and Thompson (1979); Thompson and Oldfield (1986); Bloemendal et al. (1992) Table No.2 - Mineral magnetic parameters used for interpretation of magnetic mineral concentration, mineralogy and grain size. Location Name Sample No. Depth (cm) Magnetic Concentration Magnetic Composition Magnetic Grain Size χ 10 − 7 m 3 kg − 1 SIRM 10 − 2 Am 2 kg − 1 ARM 10 − 5 Am 2 kg − 1 Soft IRM 10 − 5 Am 2 kg − 1 Hard IRM 10 − 5 Am 2 kg − 1 S ratio χ fd % ARM / SIRM (10 − 3 ) SIRM/χ 10 2 Am − 1 Salaya 1 0–13 33.61 4.68 34.35 4163.37 1.78 1.00 2.16 7.33 139.37 2 13–26 34.33 4.92 32.89 4161.69 5.91 1.00 1.94 6.69 143.29 3 26–39 44.47 6.56 52.34 5212.19 29.31 1.00 2.14 7.97 147.59 4 39–52 35.50 4.94 38.48 4058.37 65.33 0.99 2.31 7.78 139.26 5 52–65 11.19 1.49 14.12 1175.01 83.21 0.94 2.86 9.50 132.72 6 65–78 28.29 4.49 28.50 3726.24 105.49 0.98 2.32 6.35 158.57 7 78–91 11.30 1.52 13.62 1223.84 68.86 0.95 2.62 8.98 134.15 8 91–104 3.93 0.38 3.91 290.238 36.30 0.90 2.15 10.31 96.50 Sikka P. 9 0–13 26.48 3.34 20.20 2985.01 9.81 1.00 2.31 6.04 126.23 10 13–26 50.49 6.04 35.29 5664.36 164.91 0.97 1.85 5.85 119.54 11 26–39 51.29 6.02 42.72 5928.7 201.83 0.97 2.19 7.10 117.39 12 39–52 86.20 10.42 63.88 10000.5 114.27 0.99 1.98 6.13 120.89 13 52–65 42.84 3.23 28.46 1255.7 12.84 1.00 1.69 8.82 75.30 14 65–78 54.67 4.31 43.23 1223.15 72.67 0.98 1.91 10.03 78.84 15 78–91 55.56 4.42 47.96 825.339 43.86 0.99 2.00 10.85 79.55 16 91–104 48.44 3.98 43.89 834.183 93.30 0.98 1.76 11.02 82.26 Bedi P. 17 0–13 66.63 13.33 52.12 8145.57 247.28 0.98 2.69 3.91 200.02 18 13–26 57.20 13.06 43.66 7224.11 176.78 0.99 2.86 3.34 228.30 19 26–39 33.69 6.31 33.45 3761.16 194.43 0.97 3.12 5.30 187.33 20 39–52 32.39 5.61 31.74 3846.33 19.50 1.00 2.44 5.65 173.34 21 52–65 30.06 5.18 31.55 3812.44 182.31 0.96 3.63 6.09 172.44 22 65–78 4.41 0.64 5.58 314.618 157.70 0.75 6.42 8.73 144.98 23 78–91 1.92 0.28 1.05 53.0491 228.81 0.17 6.19 3.80 144.37 24 91–104 1.99 0.29 0.60 20.4985 156.30 0.46 5.30 2.07 146.45 Jodiya 25 0–13 24.86 2.50 39.01 2284.7 79.62 0.97 3.77 15.58 100.72 26 13–26 21.20 2.24 33.51 2048.33 68.02 0.97 3.41 14.93 105.87 27 26–39 17.70 1.76 24.44 1568.45 70.07 0.96 3.28 13.88 99.48 28 39–52 18.36 1.85 24.98 1645.85 65.29 0.96 3.36 13.52 100.67 29 52–65 15.48 1.54 22.08 1387.27 65.23 0.96 3.14 14.32 99.61 30 65–78 17.33 1.82 23.25 1630.67 82.36 0.95 1.88 12.81 105.17 31 78–91 15.16 1.51 19.83 1396.15 78.04 0.95 2.51 13.14 99.55 32 91–104 3.35 0.33 4.15 251.302 74.40 0.77 2.84 12.58 98.41 Nav. P. 33 0–13 14.23 1.54 22.22 1407.96 130.57 0.91 2.22 14.48 107.88 34 13–26 13.89 1.52 20.94 1353.97 131.75 0.91 2.24 13.74 109.71 35 26–39 13.91 1.48 24.23 1333.76 116.97 0.92 2.29 16.41 106.18 36 39–52 14.11 1.43 28.85 1311.04 114.20 0.92 2.32 20.20 101.25 37 52–65 12.51 1.32 24.49 1192.72 117.23 0.91 2.25 18.57 105.38 38 65–78 10.14 1.01 22.35 966.627 96.95 0.90 2.80 22.14 99.49 39 78–91 9.48 0.91 20.95 894.167 88.73 0.90 2.22 22.92 96.46 40 91–104 12.51 1.27 17.70 1210.46 108.09 0.91 2.09 13.94 101.48 Kasampir 41 0–13 9.19 0.91 17.17 863.664 86.87 0.90 1.52 18.80 99.42 42 13–26 9.57 0.91 16.75 841.158 76.10 0.92 2.35 18.47 94.73 43 26–39 9.51 0.88 18.60 829.254 22.50 0.97 2.27 21.15 92.51 44 39–52 11.08 1.11 24.77 1012.22 83.00 0.93 2.07 22.33 100.15 45 52–65 12.53 1.24 28.26 1151.16 84.54 0.93 2.37 22.79 99.02 46 65–78 12.72 1.27 20.54 1216.66 88.26 0.93 2.44 16.12 100.14 47 78–91 12.32 1.27 17.17 1215.92 92.43 0.93 2.77 13.56 102.81 48 91–104 7.78 0.75 8.62 702.92 48.49 0.94 1.32 11.46 96.71 Kandla 49 0–13 8.91 0.95 16.24 865.023 72.43 0.92 0.86 17.05 106.99 50 13–26 8.87 0.87 15.97 795.426 67.37 0.92 0.89 18.27 98.51 51 26–39 8.55 0.86 18.77 770.089 66.48 0.92 0.20 21.95 100.02 52 39–52 9.80 0.96 22.53 878.756 70.58 0.93 1.18 23.37 98.43 53 52–65 5.27 0.48 13.89 446.22 46.30 0.90 0.23 28.81 91.57 54 65–78 2.43 0.15 4.14 140.712 17.52 0.89 1.16 26.86 63.58 55 78–91 1.39 0.04 0.81 32.0763 6.56 0.85 0.45 18.70 31.27 56 91–104 1.26 0.04 0.74 25.4537 4.48 0.89 0.29 18.29 32.09 Tuna P. 57 0–13 20.52 2.61 22.19 2503.31 283.67 0.89 2.43 8.49 127.31 58 13–26 32.15 3.97 28.47 3597.75 322.05 0.92 2.71 7.17 123.55 59 26–39 12.02 1.47 18.54 1425.66 121.86 0.92 2.02 12.65 121.93 60 39–52 1.81 0.11 1.74 99.8983 12.50 0.89 0.77 15.63 61.58 61 52–65 7.63 0.89 13.83 844.38 76.34 0.91 0.38 15.59 116.31 62 65–78 5.98 0.63 9.35 611.199 50.55 0.92 0.54 14.80 105.72 63 78–91 6.66 0.76 10.92 750.537 59.67 0.92 0.19 14.39 113.93 64 91–104 12.00 1.59 14.16 1510.57 165.27 0.90 0.33 8.90 132.58 Adani P. 65 0–13 9.47 1.08 11.55 1066.89 59.92 0.94 1.48 10.67 114.34 66 13–26 10.15 1.19 11.19 1136.61 60.04 0.95 2.21 9.39 117.37 67 26–39 11.30 1.44 13.47 1372.47 76.64 0.95 2.66 9.36 127.41 68 39–52 13.03 1.73 14.99 1672.29 74.13 0.96 2.40 8.67 132.65 69 52–65 7.12 0.79 8.33 783.68 40.93 0.95 0.31 10.51 111.27 70 65–78 1.97 0.12 1.72 122.629 9.90 0.92 0.73 13.99 62.68 71 78–91 1.34 0.05 1.04 41.9403 5.22 0.89 2.16 21.44 36.10 72 91–104 1.18 0.04 0.76 31.0844 3.09 0.93 1.84 17.58 36.78 Modhva 73 0–13 12.76 2.11 10.97 2001.23 79.24 0.96 1.80 5.19 165.69 74 13–26 9.75 1.57 9.69 1516.98 84.66 0.95 1.03 6.19 160.60 75 26–39 7.35 1.25 7.42 1127.51 50.73 0.96 1.29 5.92 170.52 76 39–52 14.65 2.46 11.59 2258.97 138.93 0.94 0.80 4.71 168.07 77 52–65 10.71 1.70 9.46 1572.04 53.05 0.97 0.89 5.57 158.72 78 65–78 13.56 2.19 11.34 2036.48 69.79 0.97 0.89 5.18 161.49 79 78–91 11.20 1.88 10.36 1783.65 51.41 0.97 0.57 5.51 167.66 80 91–104 10.15 1.73 10.41 1620.83 54.19 0.97 1.05 6.01 170.63 Variations in the content of ferrimagnetic minerals (Magnetite or titanium magnetite) generally can be indicated by changes in χ , ARM and SIRM. Higher magnetic susceptibility significantly shows presence of ferrimagnetic minerals. However, χ can be good indicator of magnetic mineral concentration of samples, whereas concentration of stable single domain ferrimagnetic minerals is shown by ARM and concentration of saturated ferrimagnetic minerals is given by SIRM (Maher et al., 2009 ). The surface sediments of GoK are studied for distinguishing between different source areas of terrigenous sediments to the GoK (Prizomwala et al., 2014 ). Here for the first time the mineral magnetic measurements are studied to observe the magnetic mineral behaviour in the subsurface sediments of GoK, Gujarat. Magnetic susceptibility (Fig. 2a) measurements at various locations in the GoK indicate decreasing magnetic susceptibility with depth in the mudflats. ARM also shows similar trend like magnetic susceptibility, it also decreases with depth (Fig. 2b). ARM decreases with depth at various locations including Salaya, Sikka Port, Bedi Port, Jodiya, Adani Port, Navlakhi Port, Kasampir, Modhva, Kandla Port, and Tuna Port. ARM values show variation with the top and bottom sample locations at different places. For instance, at Salaya, the top sample has a higher ARM value, while at Sikka Port, the bottom sample has a higher ARM value. SIRM value decreases with depth. Magnetic concentration parameters decrease every 13 cm, except at Sikka Port. Presence of ferrimagnetic minerals in Mudflats of GoK. The top samples are rich in ferrimagnetic minerals, while the bottom samples have low concentrations. Magnetic mineralogy Magnetic mineralogy (or composition) dependent parameters are Soft IRM, Hard IRM and S-ratio. The S-ratio is a dimensionless parameter that indicates presence of ferrimagnetic minerals and anti-ferromagnetic minerals. The S-ratio can be used to differentiate between ‘magnetite’ and ‘hematite’ (“soft” IRM and “hard” IRM; with respect to a saturating forward IRM and various back fields IRMs). S 300 in particular is used as indicator for the magnetite-hematite ratio. S-ratio value of 1 for pure magnetite and it decreases with increasing proportion of antiferromagnetic particles such as hematite. Magnetite completely saturates at 300mT field and hematite is (more) harder, yielding lower S-ratios. Magnetic minerals in sediments can be recognized as soft and hard fractions. The soft fraction shows low coercivity and can be used to find the concentration of magnetite (Thompson and Oldfield, 1986 ); whereas the hard fractions show high coercivity and is expected to approximate to the total concentration of canted antiferromagnetic minerals (hematite) (Oldfield and Richardson, 1990 ). Figure 3 depicts the variation in magnetic properties at each port. The range of S- ratio for Mudflats of GoK is 0.26 to 1.00 (Fig. 2c). Out of 80 samples only 2 samples show the S-ratio of < 0.50 i.e. 0.41 (sample no. 23, depth 78-91cm) and 0.26 (sample no. 24, depth 91-104cm) from Bedi Port, indicating the presence of antiferromagnetic minerals (hematite). The average S-ratio of 78 samples is 0.94, dominantly showing the presence of ferrimagnetic minerals (magnetite). Soft IRM varies from 20-10000 × 10 − 5 Am 2 kg − 1 (Fig. 2d). Hard IRM varies from 1.8-426.8 × 10 − 5 Am 2 kg − 1 (Fig. 2e). Sample no. 23 and 24 from Bedi Port shows a contrastingly different magnetic assemblage, with higher Hard IRM and low S-ratio values indicating dominant high coercivity and antiferromagnetic minerals (i.e. hematite). All other locations show high Soft IRM and high S-ratio values indicating dominant low coercivity and ferrimagnetic minerals assemblage (i.e. magnetite). Grain size of magnetic minerals The parameters of χ fd %, ARM/SIRM, and SIRM/χ are used for identifying magnetic grain size in a sample. Small grains have a different number of magnetic domains-zones with a uniform magnetization direction within a grain than large grains of the same magnetic minerals. Hence, magnetic properties that reflect the domain structure are grain size indicators. From the smallest grain size to the largest, four main domain structure types are distinguished: superparamagnetic [SP, smallest grains (0.001–0.01 mm)], stable single domain [SSD, slightly larger grains (~ 0.03 - ~ 0.50 mm)], pseudo single- domain [PSD, larger grains (~ 10 mm)] and multidomain [MD, largest grains ( > ~ 10 mm)]. The magnetic remanence of SSD grain assemblage is higher and more stable than that of MD grain. Single-domain grains contain one magnetic domain and are paleomagnetically most stable. For the present study, all average ARM/SIRM value is 12.30×10 − 3 which indicates the presence of relatively finer ferrimagnetic grain assemblages or significant SSD (magnetite) grains. Lowest values are observed at Bedi Port (2.07×10 − 3 ) and highest value at Kandla Port (28.81×10 − 3 ) indicating presence of coarser ferrimagnetic assemblages or indicate a large MD (magnetite) grains. χ fd % of 2.04% indicates negligible contributions from superparamagnetic grains. High ARM/SIRM values denote significantly presence of SSD (magnetite) grains and SIRM/χ ratio reflects the absence of MD grain. The spatial distribution of magnetic susceptibility (χ) and organic matter in the surface sediments (Fig. 4 ) reveals environmental gradients influenced by both natural and anthropogenic factors. Sampling stations such as Sikka Port and Bedi Port exhibit elevated magnetic susceptibility values (often > 40,000 SI units) accompanied by low organic matter content, indicative of substantial industrial influence, likely from harbor activities and effluent discharge introducing ferrimagnetic particles such as magnetite. The reduced organic content in these locations may be attributed to oxidative degradation or dilution by mineral-rich industrial inputs. In contrast, stations like Salaya and Kandla display moderate values for both χ and organic matter, suggesting a dynamic interplay between natural sedimentation processes and moderate anthropogenic inputs. Meanwhile, more pristine or naturally influenced environments are represented by sites such as Jodiya, Kasampir, and Modhva, which show low magnetic susceptibility alongside variable but generally higher organic matter concentrations, likely reflecting coastal or fluvial depositional dynamics with minimal industrial disturbance. These variations underscore the utility of environmental magnetic parameters as proxies for identifying pollution hotspots and understanding sedimentary processes within complex coastal systems. Conclusions The magnetic mineralogical composition of surface sediments retrieved from the Gulf of Kutch is predominantly dictated by ferrimagnetic constituents, principally magnetite, accompanied by subordinate quantities of hematite. The assemblage is typified by a coexistence of stable single domain (SSD) and multi-domain (MD) grain states, reflecting a bimodal grain-size distribution potentially influenced by both natural and anthropogenic processes. Among the suite of magnetic parameters assessed, the anhysteretic remanent magnetization susceptibility (χARM) and its ratio to bulk magnetic susceptibility (χARM/χ) emerge as particularly robust diagnostic indicators, capable of discerning variations in sediment provenance and pollution loading with high sensitivity. Multivariate correlation analyses between magnetic parameters and concentrations of major geochemical elements elucidate spatially heterogeneous patterns of magnetic enhancement, which, in turn, suggest differential anthropogenic influences across the region. Sites such as Navlakhi and Kandla exhibit conspicuously elevated values of χ, SIRM, and χARM/χ, implying a significant enrichment in fine-grained ferrimagnetic particles most plausibly attributable to industrial effluents, combustion by-products, and urban runoff derived from adjacent infrastructural and manufacturing hubs. These geochemical-magnetic anomalies designate these locales as potential pollution epicenters or ‘hotspots,’ wherein the anthropogenic magnetic signal overrides the detrital background. In contrast, the magnetic response from Modhva is emblematic of a more quiescent environmental setting, wherein the predominance of natural sedimentary dynamics modulated by coastal hydrodynamic regimes and/or fluvial deposition dampens the influence of external anthropogenic magnetic contributions. Additional locales such as Salaya and Jodiya, while not exhibiting uniformly elevated magnetic intensities, demonstrate high χARM/χ values, potentially reflective of the aeolian or atmospheric deposition of ultrafine magnetic particulates, likely sourced from regional industrial or urban emissions. Collectively, the magnetic dataset delineates a nuanced environmental gradient wherein magnetic susceptibility metrics function as sensitive, non-invasive proxies for sedimentary pollution assessment. This magnetic fingerprinting, therefore, constitutes a critical prelude to more exhaustive geochemical investigations and offers a strategic framework for environmental monitoring and remediation prioritization within the Gulf of Kutch. Declarations Declaration of Competing Interest The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper. Funding This research did not receive any specific grant from funding agencies in the public, commercial, or not-for-profit sectors. Author Contribution Sanjida A. Khan wrote the main manuscript text and reviewed the manuscript.Suvarna Naikuji prepared figures and reviewed the manuscript. Acknowledgements The authors are thankful to Dr. C. Rajshekhar, former Head, Department of Paleontology, ARI, Pune for his valuable suggestions during research work. References A. Kapicka, N. Jordanova, E. Petrovský and V. Podrázský, 2003. Magnetic Study of Weakly Contaminated Forest Soils. Water, Air, and Soil Pollution 148:31–44. Basavaiah N., 2011. Experimental Geomagnetism, Geomagnetism: Solid Earth and Upper Atmosphere Perspectives. Springer publisher, Netherland, 291-386. Bloemendal, J., King, J.W., Hall, F.R., Doh, S.J., 1992. Rock magnetism of Late Neogene and Pleistocene deepsea sediments: Relationship to sediment source, diagenetic processes, and sediment lithology. J. Geophys. Res. 97, 4361. Boltovskoy E., Wright R., 1976. Recent Foraminifera. The Hague. Dr. W. Junk B.V. Publishers, 515 p. Clemens Reimann, Patrice de Caritat., 2005. Distinguishing between natural and anthropogenic sources for elements in the environment: regional geochemical surveys versus enrichment factors. Science of The Total Environment, 337(1–3). Chaparro, M.A., Sinito, A.M., Ramasamy, V., Marinelli, C., Chaparro, M.A., Mullainathan, S., Murugesan, S., 2008. Magnetic measurements and pollutants of sediments from Cauvery and Palaru River, India. Environ. Geol. 56, 425. Chaparro, M.A., Chaparro, M.A., Rajkumar, P., Ramasamy, V., Sinito, A.M., 2011. Magnetic parameters, trace elements, and multivariate statistical studies of river sediments from southeastern India: a case study from the Vellar River. Environ. Earth Sci. 63 (2), 297–310. Chaparro, M.A., Krishnamoorthy, N., Chaparro, M.A., Lecomte, K.L., Mullainathan, S., Mehra, R., Sinito, A.M., 2015. Magnetic, chemical and radionuclide studies of river sediments and their variation with different physiographic regions of Bharathapuzha River, southwestern India. Stud. Geophys. Geod. 59 (3), 438–460. Chaparro, M.A., Sinito, A.M., Ramasamy, V., Marinelli, C., Chaparro, M.A., Mullainathan, S., Murugesan, S., 2008. Magnetic measurements and pollutants of sediments from Cauvery and Palaru River, India. Environ. Geol. 56, 425. Chauhan O. S., Vora K. H., 1990. Reflection Seismic Studies in the Macrotidal Gulf of Kachchh, India. Evidences of Physiographic Evolution. Continental Shelf Research , 10(4), 385-396. Chen, Q., Liu, Z., Kissel, C., 2017. Clay mineralogical and geochemical proxies of the East Asian summer monsoon evolution in the South China Sea during Late Quaternary. Sci. Rep. 7, 42083. Dearing, J., 1999. Environmental magnetic susceptibility using the bartington MS2 system, second ed. Chinese Publications, Kenilworth. Dearing J., 1999. Magnetic Susceptibility, In: Walden J., Oldfield F., and Smith J. P., (eds) Environmental Magnetism: a practical guide: Technical Guide No. 6, Quaternary Research Association, London, 250 p. E. Petrovský, A. Kapicˇka, N. Jordanova, M. Knab, V. Hoffmann, 2000. Low-field magnetic susceptibility: a proxy method of estimating increased pollution of different environmental systems. Environmental Geology 39 (3–4). GIS (Geographical Information system), 2002. Government of India, Department of Ocean Development, ICMAM, Project Directorate, Chennai, 1-53. Govil P., Naidu P. D., 2008. Late Quaternary changes in depositional processes along the western margin of the Indus Fan. Geo-Marine Lett ., 28, 1-6. Liviu Giosana, Stefan Constantinescub , Peter D. Cliftc , Ali R. Tabrezd , Muhammed Danishd and Asif Inamd.,2006. Recent morphodynamics of the Indus delta shore and shelf. Continental Shelf Research 26,1668–1684. https://doi:10.1016/j.csr.2006.05.009 Hatfield, R.G., Maher, B.A., 2009. Fingerprinting upland sediment sources: particle sizespecific magnetic linkages between soils, lake sediments and suspended sediments. Earth Surf. Proc. Land. 34 (10), 1359–1373. Hatfield, R.G., 2014. Particle size-specific magnetic measurements as a tool for enhancing our understanding of the bulk magnetic properties of sediments. Minerals 4 (4), 758–787. Hatfield, R.G., Wheeler, B.H., Reilly, B.T., Stoner, J.S., Housen, B.A., 2019. Particle size specific magnetic properties across the norwegian-greenland seas: insights into the influence of sediment source and texture on bulk magnetic records. Geochem. Geophys. Geosyst. 20 (2), 1004–1025. Hilgenfeldt, K. (2000). Diagenetic dissolution of biogenic magnetite in surface sediments of the Benguela upwelling system. International Journal of Earth Sciences , 88 (4), 630-640. https://doi.org/10.1007/s005310050293 Horng, C.S., Huh, C.A., 2011. Magnetic properties as tracers for source-to-sink dispersal of sediments: A case study in the Taiwan Strait. Earth Planet. Sci. Lett. 309, 141–152. Just, J., Dekkers, M. J., von Dobeneck, T., van Hoesel, A., & Bickert, T. (2012). Signatures and significance of aeolian, fluvial, bacterial and diagenetic magnetic mineral fractions in Late Quaternary marine sediments off Gambia, NW Africa. Geochemistry , Geophysics , Geosystems , 13 (9). https://doi.org /10.1029/2012gc004146 King, J., Banerjee, S.K., Marvin, J., Ozdemir, O., 1982. A comparison of different magnetic methods for determining the relative grain size of magnetite in natural materials: some results from lake sediments. Earth Planet. Sci. Lett. 59, 404–419. Kulkarni, Y.R., Sangode, S.J., Meshram, D.C., Patil, S.K., Dutt, Y., 2014. Mineral magnetic characterization of the Godavari River sediments: Implications to Deccan basalt weathering. J. Geol. Soc. India 83, 376–384. L.S Chan, S.L Ng, A.M Davis, W.W.S Yim, C.H Yeung., 2001. Magnetic Properties and Heavy-metal Contents of Contaminated Seabed Sediments of Penny's Bay, Hong Kong. Marine Pollution bulletin. 42(7), 569-583. Larrasoaña, J. C., Roberts, A. P., Stoner, J. S., Richter, C., & Wehausen, R. (2003b). A new proxy for bottom-water ventilation in the eastern Mediterranean based on diagenetically controlled magnetic properties of sapropel-bearing sediments. Palaeogeography , Palaeoclimatology , Palaeoecology , 190 , 221-242. https://doi.org/10.1016/s0031-0182(02)00607-7 Liu, X., Li, A., Dong, J., Lu, J., Huang, J., Wan, S., 2018. Provenance discrimination of sediments in the Zhejiang-Fujian mud belt, East China Sea: Implications for the development of the mud depocenter. J. Asian Earth Sci. 151, 1–15. Liu, Q., Roberts, A.P., Larrasoana, ˜ J.C., Banerjee, S.K., Guyodo, Y., Tauxe, L., Oldfield, F., 2012. Environmental magnetism: principles and applications. Rev. Geophys. 50 (4). Liviu Giosana, Stefan Constantinescub , Peter D. Cliftc , Ali R. Tabrezd , Muhammed Danishd , Asif Inamd.,2006. Recent morphodynamics of the Indus delta shore and shelf. Continental Shelf Research 26, 1668- 1684. Maher B. A., Watkins S. J., Brunskill G., Alexander J. J., Fielding C. R., 2009. Sediment provenance in a tropical fluvial and marine context by magnetic ‘fingerprinting’ of transportable sand fractions. Sedimentology , 56, 841-861. Murray J. W., 2006. Ecology and Applications of Benthic Foraminifera; Cambridge University Press, 426 p. Oldfield F., Richardson N., 1990. Lake sediment magnetism and atmospheric deposition; Philos. Trans. Roy. Soc. London B , 327,325-330. Prizomwala S. P., Bhatt N., Basavaiah N., 2014. Understanding the sediment routing system along the Gulf of Kachchh coast, western India: Significance of small ephemeral rivers. J. Earth Syst. Sci., 123(1),121-133. Roberts, A. P., Stoner, J. S., & Richter, C. (1999). Diagenetic magnetic enhancement of sapropels from the eastern Mediterranean Sea. Marine Geology , 153 (1-4), 103- 116. https://doi.org/10.1016/S0025-3227(98)00087-5 Roberts, A. P., Tauxe, L., & Heslop, D. (2013). Magnetic paleointensity stratigraphy and high-resolution Quaternary geochronology: Successes and future challenges. Quaternary Science Reviews , 61 , 1-16. https://doi.org/10.1016/ j.quascirev.2012.10.036 Robinson, S. G., Sahota, J. T., & Oldfield, F. (2000). Early diagenesis in North Atlantic abyssal plain sediments characterized by rock-magnetic and geochemical indices. Marine Geology , 163 (1-4), 77 107. https://doi.org/10.1016/s0025- 3227(99)00108-5 Rowan, C. J., Roberts, A. P., & Broadbent, T. (2009). Reductive diagenesis, magnetite dissolution, greigite growth and paleomagnetic smoothing in marine sediments: A new view. Earth and Planetary Science Letters , 277 (1-2), 223-235. https://doi.org/10.1016/j.epsl.2008.10.016 Sangode, S.J., Sinha, R., Phartiyal, B., Chauhan, O.S., Mazari, R.K., Bagati, T.N., Suresh, N., Mishra, S., Kumar, R., Bhattacharjee, P., 2007. Environmental magnetic studies on some Quaternary sediments of varied depositional settings in the Indian subcontinent. Quat. Int. 159, 102–118. Sandeep, K., Shankar, R., Krishnaswamy, J., 2011. Assessment of suspended particulate pollution in the Bhadra River catchment, Southern India: an environmental magnetic approach. Environ. Earth Sci. 62, 625–637. Syvitski, J.P., Peckham, S.D., Hilberman, R., Mulder, T., 2003. Predicting the terrestrial flux of sediment to the global ocean: a planetary perspective. Sed. Geol. 162 (1),5–24. Tarduno, J. A., & Wilkison, S. L. (1996). Non-steady state magnetic mineral reduction, chemical lock-in, and delayed remanence acquisition in pelagic sediments. Earth and Planetary Science Letters , 144 (3-4), 315-326. https://doi.org/ 10.1016/s0012-821x(96)00174-4 Thompson, R., Oldfield, R., 1986. Environmental Magnetism. Allen and Unwin, New York, pp. 227. Van Hoof, A. A. M., Van Os, B. J. H., Rademakers, J. G., Langereis, C. G., & de Lange, G. J. (1993). A paleomagnetic and geochemical record of the upper Cochiti reversal and two subsequent processional cycles from Southern Sicily (Italy). Earth and Planetary Science Letters , 117 (1-2), 235-250. https://doi.org/10.1016/0012-821X(93)90130-2 Additional Declarations No competing interests reported. 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Also discoverable on Platform About Our Team In Review Editorial Policies Advisory Board Help Center Resources Author Services Accessibility API Access RSS feed Manage Cookie Preferences © Research Square 2026 | ISSN 2693-5015 (online) Privacy Policy Terms of Service Do Not Sell My Personal Information {"props":{"pageProps":{"initialData":{"identity":"rs-6582332","acceptedTermsAndConditions":true,"allowDirectSubmit":true,"archivedVersions":[],"articleType":"Research Article","associatedPublications":[],"authors":[{"id":464796012,"identity":"8db513fa-d767-453c-b1f5-a98018a7f783","order_by":0,"name":"Sanjida A. Khan","email":"data:image/png;base64,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","orcid":"","institution":"Nowrosjee Wadia College","correspondingAuthor":true,"prefix":"","firstName":"Sanjida","middleName":"A.","lastName":"Khan","suffix":""},{"id":464796013,"identity":"392db524-cf8e-472d-8b59-03afbeeeecae","order_by":1,"name":"Suvarna Naikuji","email":"","orcid":"","institution":"Savitribai Phule Pune University","correspondingAuthor":false,"prefix":"","firstName":"Suvarna","middleName":"","lastName":"Naikuji","suffix":""}],"badges":[],"createdAt":"2025-05-03 06:38:14","currentVersionCode":1,"declarations":"","doi":"10.21203/rs.3.rs-6582332/v1","doiUrl":"https://doi.org/10.21203/rs.3.rs-6582332/v1","draftVersion":[],"editorialEvents":[],"editorialNote":"","failedWorkflow":false,"files":[{"id":83762599,"identity":"26904188-54e8-459d-8300-c42e1b1df199","added_by":"auto","created_at":"2025-06-02 10:05:04","extension":"png","order_by":1,"title":"Figure 1","display":"","copyAsset":false,"role":"figure","size":313469,"visible":true,"origin":"","legend":"\u003cp\u003eLocation map showing the Subsurface sampling sites, Gulf of Kachchh, Gujarat, India\u003c/p\u003e","description":"","filename":"1.png","url":"https://assets-eu.researchsquare.com/files/rs-6582332/v1/4e9702ef8545c522442f2d65.png"},{"id":83762440,"identity":"79f23c06-86c7-4adb-8900-1a651515340b","added_by":"auto","created_at":"2025-06-02 09:57:04","extension":"png","order_by":2,"title":"Figure 2","display":"","copyAsset":false,"role":"figure","size":39324,"visible":true,"origin":"","legend":"\u003cp\u003ea) χlf variations of Subsurface sediments, Mudflats, GoK b) ARM variation of Subsurface sediments c) S-ratio variation of Subsurface sediments d) Hard IRM acquisition of Subsurface sediments e) Soft IRM acquisition of Subsurface sediments f) χ fd % of Subsurface sediments g) Correlation between ARM and SIRM (10 \u003csup\u003e-3\u003c/sup\u003e) of Subsurface sediments h) Correlation between SIRM and χ (10 \u003csup\u003e2\u003c/sup\u003e) of Subsurface sediments, Mudflats, GoK.\u003c/p\u003e","description":"","filename":"2.png","url":"https://assets-eu.researchsquare.com/files/rs-6582332/v1/ddaa3f88b84cb83fb376153f.png"},{"id":83763240,"identity":"8f1b5b47-01ee-489a-8e81-e8652f37e9ab","added_by":"auto","created_at":"2025-06-02 10:13:04","extension":"png","order_by":3,"title":"Figure 3","display":"","copyAsset":false,"role":"figure","size":45262,"visible":true,"origin":"","legend":"\u003cp\u003eMagnetic properties of GoK\u003c/p\u003e","description":"","filename":"3.png","url":"https://assets-eu.researchsquare.com/files/rs-6582332/v1/b6bdf9af27749f58a1f3b437.png"},{"id":83762447,"identity":"17fc4420-3d7c-4af5-a7d7-fa20ccb3e956","added_by":"auto","created_at":"2025-06-02 09:57:04","extension":"png","order_by":4,"title":"Figure 4","display":"","copyAsset":false,"role":"figure","size":35632,"visible":true,"origin":"","legend":"\u003cp\u003eScatter plot illustrating the relationship between magnetic susceptibility (χ) and organic matter content.\u003c/p\u003e","description":"","filename":"4.png","url":"https://assets-eu.researchsquare.com/files/rs-6582332/v1/c67b4610a9ade5fc09f99fb6.png"},{"id":88803028,"identity":"a64cf42f-c8fa-4012-ae20-a81ca93a9e37","added_by":"auto","created_at":"2025-08-11 14:32:12","extension":"pdf","order_by":0,"title":"","display":"","copyAsset":false,"role":"manuscript-pdf","size":1770633,"visible":true,"origin":"","legend":"","description":"","filename":"manuscript.pdf","url":"https://assets-eu.researchsquare.com/files/rs-6582332/v1/11938312-6c6f-404f-a95f-7953afe165d3.pdf"}],"financialInterests":"No competing interests reported.","formattedTitle":"Environmental magnetic characterization of the sediments from shallow cores of Gulf of Kachchh, Gujarat, India","fulltext":[{"header":"Introduction","content":"\u003cp\u003eEnvironmental magnetism serves as an invaluable tool in the study of palaeoceanographic conditions, primarily because of its sharp sensitivity to both depositional processes and sedimentary diagenesis, particularly through the phenomenon of reductive dissolution, as documented by various studies (Larrasoa\u0026ntilde;a et al., \u003cspan citationid=\"CR27\" class=\"CitationRef\"\u003e2003b\u003c/span\u003e; Roberts et al., \u003cspan citationid=\"CR35\" class=\"CitationRef\"\u003e1999\u003c/span\u003e; Robinson et al., \u003cspan citationid=\"CR37\" class=\"CitationRef\"\u003e2000\u003c/span\u003e; Tarduno \u0026amp; Wilkinson, 1996; van Hoof et al., \u003cspan citationid=\"CR44\" class=\"CitationRef\"\u003e1993\u003c/span\u003e). The magnetic minerals present in marine sediments, which largely originate from detrital inputs, biomineralization, or subsequent post-depositional alterations of these sources, respond intricately to environmental fluctuations. This responsiveness not only underscores the utility of magnetic properties and grain size variations in these sediments as proxies for environmental changes but also facilitates the detailed characterization of geochemical environments and depositional regimes, thereby enriching our understanding of paleoceanographic dynamics (Hilgenfeldt, \u003cspan citationid=\"CR21\" class=\"CitationRef\"\u003e2000\u003c/span\u003e; Just et al., \u003cspan citationid=\"CR23\" class=\"CitationRef\"\u003e2012\u003c/span\u003e; Liu et al., \u003cspan citationid=\"CR29\" class=\"CitationRef\"\u003e2012\u003c/span\u003ea; Roberts et al., \u003cspan citationid=\"CR36\" class=\"CitationRef\"\u003e2013\u003c/span\u003e; Rowan et al., \u003cspan citationid=\"CR38\" class=\"CitationRef\"\u003e2009\u003c/span\u003e; Thompson \u0026amp; Oldfield, \u003cspan citationid=\"CR43\" class=\"CitationRef\"\u003e1986\u003c/span\u003e).\u003c/p\u003e \u003cp\u003eIron-bearing minerals, known for their sensitivity to environmental changes, offer valuable insights due to their pronounced and indicative signatures, which can be detected even at low concentrations. These minerals are reliably utilized to characterize sediment provenance (Thompson and Oldfield, \u003cspan citationid=\"CR43\" class=\"CitationRef\"\u003e1986\u003c/span\u003e; Dearing, \u003cspan citationid=\"CR12\" class=\"CitationRef\"\u003e1999\u003c/span\u003e; Hatfield and Maher, \u003cspan citationid=\"CR18\" class=\"CitationRef\"\u003e2009\u003c/span\u003e; Hatfield, \u003cspan citationid=\"CR19\" class=\"CitationRef\"\u003e2014\u003c/span\u003e). Mineral magnetic measurements have proven effective across various geo-scientific applications, ranging from the reconstruction of paleoclimate and recent climate changes to foraminifera assemblages and environmental risk assessments. This method not only aids to identify the foraminiferal assemblage in subsurface sediments but also facilitates the exploration of relationships between magnetic domain size and physical particle size of sediments. Such insights are crucial for understanding hydrodynamic conditions, sediment transport and depositional pathways, diagenetic and authigenic changes, as well as anthropogenic impacts (Bloemendal et al., \u003cspan citationid=\"CR3\" class=\"CitationRef\"\u003e1992\u003c/span\u003e; Sangode et al., \u003cspan citationid=\"CR39\" class=\"CitationRef\"\u003e2007\u003c/span\u003e; Hatfield and Maher, \u003cspan citationid=\"CR18\" class=\"CitationRef\"\u003e2009\u003c/span\u003e; Horng and Huh, \u003cspan citationid=\"CR22\" class=\"CitationRef\"\u003e2011\u003c/span\u003e; Chaparro et al., \u003cspan citationid=\"CR6\" class=\"CitationRef\"\u003e2008\u003c/span\u003e, \u003cspan citationid=\"CR7\" class=\"CitationRef\"\u003e2011\u003c/span\u003e, \u003cspan citationid=\"CR8\" class=\"CitationRef\"\u003e2015\u003c/span\u003e; Kulkarni et al., \u003cspan citationid=\"CR25\" class=\"CitationRef\"\u003e2014\u003c/span\u003e; Sandeep et al., \u003cspan citationid=\"CR40\" class=\"CitationRef\"\u003e2011\u003c/span\u003e; Chen et al., \u003cspan citationid=\"CR11\" class=\"CitationRef\"\u003e2017\u003c/span\u003e; Liu et al., \u003cspan citationid=\"CR28\" class=\"CitationRef\"\u003e2018\u003c/span\u003e; Hatfield et al., \u003cspan citationid=\"CR20\" class=\"CitationRef\"\u003e2019\u003c/span\u003e).\u003c/p\u003e \u003cp\u003eIn similar way, magnetic particles, recognized for their extensive surface area, serve as efficient absorbers of various toxic metals, thereby enabling magnetic parameters to be employed as proxies in chemical analyses, particularly in environmental studies (Hoffmann et al., 1999; Kapicka et al., \u003cspan citationid=\"CR1\" class=\"CitationRef\"\u003e2003\u003c/span\u003e; Petrovsky et al., 2000). The preferential absorption of heavy metals by iron oxides and hydroxides, as identified by Reimann and Caritat (2005), further emphasizes the utility of magnetic susceptibility (χ) measurements, which, despite their high natural variability, have been widely adopted as indicators of contamination. Moreover, in urban areas, χ measurements have proven particularly effective in assessing pollution from exhaust gases and industrial discharges, with the elevated χ values observed in marine sediments often attributable to fine-grained iron oxides originating from anthropogenic sources (Chan et al., \u003cspan citationid=\"CR26\" class=\"CitationRef\"\u003e2001\u003c/span\u003e).\u003c/p\u003e \u003cp\u003eThe present work investigates magnetic characteristics of the sediments to determine the mineralogy and grain size of magnetic minerals in subsurface sediments of Gulf of Kachchh coast\u003c/p\u003e\n\u003ch3\u003eStudy area\u003c/h3\u003e\n\u003cp\u003eThe GoK (Gulf of Kachchh will here written as GoK )is a semi-closed basin in the northern Arabian Sea lying between 22\u0026deg;15\u0026acute; to 23\u0026deg;N and 69\u0026deg; to 70\u0026deg;15\u0026acute;E along the west coast of India surrounded by Kachchh mainland in the north and Saurashtra horst in the south (Fig.\u0026nbsp;1). GoK divides Kachchh and the Kathiawar peninsula regions of Gujarat and is about 99 miles long. GoK exhibits a macro tidal environment with a tidal range of about 7 m at the head to 3 m at the mouth because of its peculiar shape. River Indus is placed at about 100 km north of GoK, which carries about 50\u0026nbsp;million tons of sediments yearly (Giosan \u003cem\u003eet al\u003c/em\u003e., 2006). GoK presently is a very active industrial hub with many small and large ports along the coasts such as Kandla, Adani, Mundra, Okha along with many pipelines, jetties, shipbuilding work, oil refineries, cement industries, etc.\u003c/p\u003e \u003cp\u003eThe high tidal flux at GoK covers vast low-lying areas of about 1500 km\u003csup\u003e2\u003c/sup\u003e in inner gulf encompassing a network of creeks, estuaries and mud flats (Govil and Naidu, \u003cspan citationid=\"CR16\" class=\"CitationRef\"\u003e2008\u003c/span\u003e). Three main creeks namely Kandla, Hansthal and Nakti make up the creek system and the little GoK are interconnected through many large and small creeks (Chauhan and Vora, \u003cspan citationid=\"CR10\" class=\"CitationRef\"\u003e1990\u003c/span\u003e). In GoK the intertidal expanse increases towards upstream. The increase is approximately from 0.5 to 2 km from Jakhau to Kandla and from around 1 km at Okha to over 10 km at Navlakhi (Chauhan and Vora, \u003cspan citationid=\"CR10\" class=\"CitationRef\"\u003e1990\u003c/span\u003e). The GoK overall occupies area under low tidal mudflats is 1590 km\u003csup\u003e2\u003c/sup\u003e and high tidal mudflats is 586 km\u003csup\u003e2\u003c/sup\u003e (GIS, 2002). The GoK covers approximately 1500 km2 of low-lying areas, including creeks, estuaries, and mud flats\u003c/p\u003e"},{"header":"Methodology","content":"\u003cdiv id=\"Sec3\" class=\"Section2\"\u003e \u003cp\u003eTotal 80 subsurface samples were collected from ten various mudflat localities, GoK namely (1) Salaya, (2) Sikka Port, (3) Bedi Port, (4) Jodiya, (5) Adani Port, (6) Navlakhi Port, (7) Kasampir, (8) Modhva, (9) Kandla Port and (10) Tuna Port. All the locations are from mudflats except Modhva which shows sandy beach. For subsurface sampling, 1m by 1m shallow core of square shaped ditch/trench was excavated with hand shovel. Samples were taken at regular intervals of 13 cm using measuring tape, thus in all total 8 samples were recovered from 1.04 m trench.\u003c/p\u003e \u003cp\u003eIn the course of laboratory investigations, approximately 9\u0026ndash;10 grams of meticulously air-dried sediment were precisely packed into standard non-magnetic styrene containers, subsequently rendered airtight to maintain the physicochemical integrity of the samples throughout the entirety of the magnetic susceptibility measurements. The magnetic susceptibility (χ) assessments were conducted on both bulk sediment matrices and granulometrically segregated sediment fractions utilizing a high-sensitivity MFK1-FA Kappabridge (3\u0026times;10⁻⁸ SI), operated at a low excitation frequency of 976 Hz and an applied alternating magnetic field intensity of 200 A/m.\u003c/p\u003e \u003cp\u003eAnhysteretic remanent magnetization (ARM) was imparted to the bulk sediment specimens employing a Molspin spinner magnetometer under the influence of a unidirectional steady magnetic field of 0.05 mT, superimposed with a decaying alternating field. The ARM intensities were subsequently normalized with respect to the magnitude of the applied steady field and expressed as the anhysteretic remanent magnetization susceptibility (χARM), thereby facilitating inter-sample comparison.\u003c/p\u003e \u003cp\u003eIsothermal remanent magnetization (IRM) acquisition was systematically executed on the bulk sediment samples via an ASC Impulse Magnetizer, wherein magnetization was induced in forward-directed magnetic fields of 40 mT and 1 T, followed by stepwise application of reverse (backfield) intensities at \u0026minus;\u0026thinsp;20, \u0026minus;30, \u0026minus;\u0026thinsp;40, \u0026minus;100, and \u0026minus;\u0026thinsp;300 mT. The resultant remanent magnetizations were quantified using the Molspin Spinner Magnetometer, ensuring high-resolution detection of coercivity distributions and magnetic mineralogy.\u003c/p\u003e \u003cp\u003eConcomitantly, foraminiferal analysis necessitated a rigorous sample preparation protocol primarily encompassing the disaggregation and sieving of sediments. Each sample was transferred into a pre-labeled 1-liter beaker and subjected to overnight oxidation in hydrogen peroxide. A volume of 15\u0026ndash;30 ml of a 15% hydrogen peroxide solution (diluted from a stock 30% concentration) was introduced to facilitate the degradation of organic constituents. Subsequently, the treated sediments underwent wet sieving through a series of ASTM-E11 standard mesh sieves\u0026mdash;specifically, mesh numbers 20, 80, 140, and 230\u0026mdash;enabling precise granulometric classification for downstream micropaleontological examination.\u003c/p\u003e \u003c/div\u003e"},{"header":"Results and discussion","content":"\u003cp\u003eThe environmental magnetic parameters for bulk sediments from the Gulf of Kachchh (GOK), summarized in Table\u0026nbsp;1, are further detailed in Table\u0026nbsp;2 and graphically illustrated in Fig.\u0026nbsp;2. At Salaya port, the moderate ARM/χ ratios combined with relatively high SIRM/χ values indicate that the grain size predominantly falls within the single-domain (SD) to pseudo-single-domain (PSD) range, with magnetite likely being the dominant mineral. S. Port exhibits variations in ARM/χ and SIRM/χ ratios, suggesting a mixture of grain sizes from fine to coarse, with a significant presence of low-coercivity minerals. In contrast, B. Port's high ARM/χ ratios point to fine grains, while moderate SIRM/χ values indicate a mix of SD and multi-domain (MD) grains. Jodiya's ARM/χ ratios and SIRM/χ values similarly suggest the presence of fine-grained magnetic minerals, likely in the SD to small PSD range, with magnetite as the dominant mineral. Navlakhi stands out with extremely high χ values coupled with moderate ARM/χ ratios, indicating a large concentration of magnetite with varying grain sizes. Kasampir shows evidence of fine grains, as indicated by high ARM/χ and SIRM/χ values, with significant concentrations of low-coercivity minerals. At Kandla, the ARM/χ values suggest a prevalence of finer grains, likely in the SD range, along with moderate coercivity minerals. Tuna Port's ARM/χ values also indicate finer grains with significant low-coercivity mineral content. Adani Port, on the other hand, shows low to moderate ARM/SIRM values, suggesting a mix of fine and coarse grains with a dominance of magnetite. Lastly, Modhva's low ARM/SIRM values suggest the presence of coarser grains, possibly within the multi-domain range.\u003c/p\u003e \u003cp\u003e\u003cstrong\u003eTable No.1\u003c/strong\u003e: Various magnetic mineral parameters used in the present study\u003c/p\u003e\n\u003ctable border=\"1\" cellspacing=\"0\" cellpadding=\"0\" width=\"591\"\u003e\n \u003ctbody\u003e\n \u003ctr\u003e\n \u003ctd valign=\"top\" style=\"width: 103px;\"\u003e\n \u003cp\u003e\u003cstrong\u003eParameter\u003c/strong\u003e\u003c/p\u003e\n \u003c/td\u003e\n \u003ctd valign=\"top\" style=\"width: 101px;\"\u003e\n \u003cp\u003e\u003cstrong\u003eUnits\u003c/strong\u003e\u003c/p\u003e\n \u003c/td\u003e\n \u003ctd valign=\"top\" style=\"width: 166px;\"\u003e\n \u003cp\u003e\u003cstrong\u003eDescription\u003c/strong\u003e\u003c/p\u003e\n \u003c/td\u003e\n \u003ctd valign=\"top\" style=\"width: 94px;\"\u003e\n \u003cp\u003e\u003cstrong\u003eFormula\u003c/strong\u003e\u003c/p\u003e\n \u003c/td\u003e\n \u003ctd valign=\"top\" style=\"width: 127px;\"\u003e\n \u003cp\u003e\u003cstrong\u003eReferences\u003c/strong\u003e\u003c/p\u003e\n \u003c/td\u003e\n \u003c/tr\u003e\n \u003ctr\u003e\n \u003ctd valign=\"top\" style=\"width: 103px;\"\u003e\n \u003cp\u003eLow frequency mass specific magnetic susceptibility (\u0026chi;lf)\u003c/p\u003e\n \u003c/td\u003e\n \u003ctd valign=\"top\" style=\"width: 101px;\"\u003e\n \u003cp\u003em\u0026sup3; kg⁻\u0026sup1;\u003c/p\u003e\n \u003c/td\u003e\n \u003ctd valign=\"top\" style=\"width: 166px;\"\u003e\n \u003cp\u003eRepresents the concentration of bulk magnetic minerals in a sample.\u003c/p\u003e\n \u003c/td\u003e\n \u003ctd valign=\"top\" style=\"width: 94px;\"\u003e\n \u003cp\u003e\u0026nbsp; \u0026nbsp; \u0026nbsp; \u0026nbsp; \u0026nbsp; -\u003c/p\u003e\n \u003c/td\u003e\n \u003ctd valign=\"top\" style=\"width: 127px;\"\u003e\n \u003cp\u003eThompson and Oldfield (1986); Dearing (1999)\u003c/p\u003e\n \u003c/td\u003e\n \u003c/tr\u003e\n \u003ctr\u003e\n \u003ctd valign=\"top\" style=\"width: 103px;\"\u003e\n \u003cp\u003ePercentage frequency dependent susceptibility (\u0026chi;fd%)\u003c/p\u003e\n \u003c/td\u003e\n \u003ctd valign=\"top\" style=\"width: 101px;\"\u003e\n \u003cp\u003e%\u003c/p\u003e\n \u003c/td\u003e\n \u003ctd valign=\"top\" style=\"width: 166px;\"\u003e\n \u003cp\u003eUsed to detect the presence of superparamagnetic (SP) ferrimagnetic particles.\u003c/p\u003e\n \u003c/td\u003e\n \u003ctd valign=\"top\" style=\"width: 94px;\"\u003e\n \u003cp\u003e\u0026chi;fd% = [(\u0026chi;lf \u0026minus; \u0026chi;hf) / \u0026chi;lf] \u0026times; 100\u003c/p\u003e\n \u003c/td\u003e\n \u003ctd valign=\"top\" style=\"width: 127px;\"\u003e\n \u003cp\u003eMaher (1986); Dearing (1999)\u003c/p\u003e\n \u003c/td\u003e\n \u003c/tr\u003e\n \u003ctr\u003e\n \u003ctd valign=\"top\" style=\"width: 103px;\"\u003e\n \u003cp\u003eFrequency dependent susceptibility (\u0026chi;fd)\u003c/p\u003e\n \u003c/td\u003e\n \u003ctd valign=\"top\" style=\"width: 101px;\"\u003e\n \u003cp\u003em\u0026sup3; kg⁻\u0026sup1;\u003c/p\u003e\n \u003c/td\u003e\n \u003ctd valign=\"top\" style=\"width: 166px;\"\u003e\n \u003cp\u003eIndicates the presence of ultrafine magnetic grains at the stable single domain (SD)/superparamagnetic (SP) boundary.\u003c/p\u003e\n \u003c/td\u003e\n \u003ctd valign=\"top\" style=\"width: 94px;\"\u003e\n \u003cp\u003e\u0026chi;fd = (\u0026chi;lf \u0026minus; \u0026chi;hf)\u003c/p\u003e\n \u003c/td\u003e\n \u003ctd valign=\"top\" style=\"width: 127px;\"\u003e\n \u003cp\u003eThompson and Oldfield (1986); Maher (1986); Dearing et al. (1996); Dearing (1999)\u003c/p\u003e\n \u003c/td\u003e\n \u003c/tr\u003e\n \u003ctr\u003e\n \u003ctd valign=\"top\" style=\"width: 103px;\"\u003e\n \u003cp\u003eSaturation isothermal remanent magnetization (SIRM)\u003c/p\u003e\n \u003c/td\u003e\n \u003ctd valign=\"top\" style=\"width: 101px;\"\u003e\n \u003cp\u003eAm\u0026sup2; kg⁻\u0026sup1;\u003c/p\u003e\n \u003c/td\u003e\n \u003ctd valign=\"top\" style=\"width: 166px;\"\u003e\n \u003cp\u003eHighest level of magnetic remanence induced in a sample by a high magnetic field (commonly at 1 T).\u003c/p\u003e\n \u003c/td\u003e\n \u003ctd valign=\"top\" style=\"width: 94px;\"\u003e\n \u003cp\u003e\u0026nbsp; \u0026nbsp; \u0026nbsp; \u0026nbsp; \u0026nbsp; \u0026nbsp;-\u003c/p\u003e\n \u003c/td\u003e\n \u003ctd valign=\"top\" style=\"width: 127px;\"\u003e\n \u003cp\u003eThompson et al. (1980); Thompson and Oldfield (1986)\u003c/p\u003e\n \u003c/td\u003e\n \u003c/tr\u003e\n \u003ctr\u003e\n \u003ctd valign=\"top\" style=\"width: 103px;\"\u003e\n \u003cp\u003eSusceptibility of anhysteretic remanent magnetization (\u0026chi;ARM)\u003c/p\u003e\n \u003c/td\u003e\n \u003ctd valign=\"top\" style=\"width: 101px;\"\u003e\n \u003cp\u003em\u0026sup3; kg⁻\u0026sup1;\u003c/p\u003e\n \u003c/td\u003e\n \u003ctd valign=\"top\" style=\"width: 166px;\"\u003e\n \u003cp\u003eSensitive to both concentration and grain size of ferrimagnetic minerals, particularly near the SP/SD boundary.\u003c/p\u003e\n \u003c/td\u003e\n \u003ctd valign=\"top\" style=\"width: 94px;\"\u003e\n \u003cp\u003e\u0026nbsp; \u0026nbsp; \u0026nbsp; \u0026nbsp; \u0026nbsp; -\u003c/p\u003e\n \u003c/td\u003e\n \u003ctd valign=\"top\" style=\"width: 127px;\"\u003e\n \u003cp\u003eKing et al. (1982); Thompson and Oldfield (1986)\u003c/p\u003e\n \u003c/td\u003e\n \u003c/tr\u003e\n \u003ctr\u003e\n \u003ctd valign=\"top\" style=\"width: 103px;\"\u003e\n \u003cp\u003eHard isothermal remanent magnetization (HIRM)\u003c/p\u003e\n \u003c/td\u003e\n \u003ctd valign=\"top\" style=\"width: 101px;\"\u003e\n \u003cp\u003eAm\u0026sup2; kg⁻\u0026sup1;\u003c/p\u003e\n \u003c/td\u003e\n \u003ctd valign=\"top\" style=\"width: 166px;\"\u003e\n \u003cp\u003eApproximates the concentration of antiferromagnetic minerals in a sample.\u003c/p\u003e\n \u003c/td\u003e\n \u003ctd valign=\"top\" style=\"width: 94px;\"\u003e\n \u003cp\u003eHIRM = 0.5 \u0026times; (SIRM + IRM-300mT)\u003c/p\u003e\n \u003c/td\u003e\n \u003ctd valign=\"top\" style=\"width: 127px;\"\u003e\n \u003cp\u003eThompson and Oldfield (1986); Liu et al. (2007)\u003c/p\u003e\n \u003c/td\u003e\n \u003c/tr\u003e\n \u003ctr\u003e\n \u003ctd valign=\"top\" style=\"width: 103px;\"\u003e\n \u003cp\u003eS-ratio\u003c/p\u003e\n \u003c/td\u003e\n \u003ctd valign=\"top\" style=\"width: 101px;\"\u003e\n \u003cp\u003eDimensionless\u003c/p\u003e\n \u003c/td\u003e\n \u003ctd valign=\"top\" style=\"width: 166px;\"\u003e\n \u003cp\u003eIndicates the relative abundance of low-coercivity and high-coercivity minerals in bulk samples. Values close to 1 indicate low-coercivity minerals, and values close to 0 or negative indicate high-coercivity minerals.\u003c/p\u003e\n \u003c/td\u003e\n \u003ctd valign=\"top\" style=\"width: 94px;\"\u003e\n \u003cp\u003eS-ratio = -IRM-300mT / SIRM\u003c/p\u003e\n \u003c/td\u003e\n \u003ctd valign=\"top\" style=\"width: 127px;\"\u003e\n \u003cp\u003eStober and Thompson (1979); Thompson and Oldfield (1986); Bloemendal et al. (1992)\u003c/p\u003e\n \u003c/td\u003e\n \u003c/tr\u003e\n \u003c/tbody\u003e\n\u003c/table\u003e\u003c/br\u003e\u003cp\u003e \u003cb\u003eTable No.2\u003c/b\u003e- Mineral magnetic parameters used for interpretation of magnetic mineral concentration, mineralogy and grain size.\u003c/p\u003e \u003cp\u003e \u003cdiv class=\"gridtable\"\u003e\u003ctable float=\"No\" id=\"Tabb\" border=\"1\"\u003e \u003ccolgroup cols=\"12\"\u003e \u003cdiv align=\"left\" class=\"colspec\" colname=\"c1\" colnum=\"1\"\u003e\u003c/div\u003e \u003cdiv align=\"char\" char=\".\" class=\"colspec\" colname=\"c2\" colnum=\"2\"\u003e\u003c/div\u003e \u003cdiv align=\"left\" class=\"colspec\" colname=\"c3\" colnum=\"3\"\u003e\u003c/div\u003e \u003cdiv align=\"char\" char=\".\" class=\"colspec\" colname=\"c4\" colnum=\"4\"\u003e\u003c/div\u003e \u003cdiv align=\"char\" char=\".\" class=\"colspec\" colname=\"c5\" colnum=\"5\"\u003e\u003c/div\u003e \u003cdiv align=\"char\" char=\".\" class=\"colspec\" colname=\"c6\" colnum=\"6\"\u003e\u003c/div\u003e \u003cdiv align=\"char\" char=\".\" class=\"colspec\" colname=\"c7\" colnum=\"7\"\u003e\u003c/div\u003e \u003cdiv align=\"char\" char=\".\" class=\"colspec\" colname=\"c8\" colnum=\"8\"\u003e\u003c/div\u003e \u003cdiv align=\"char\" char=\".\" class=\"colspec\" colname=\"c9\" colnum=\"9\"\u003e\u003c/div\u003e \u003cdiv align=\"char\" char=\".\" class=\"colspec\" colname=\"c10\" colnum=\"10\"\u003e\u003c/div\u003e \u003cdiv align=\"char\" char=\".\" class=\"colspec\" colname=\"c11\" colnum=\"11\"\u003e\u003c/div\u003e \u003cdiv align=\"char\" char=\".\" class=\"colspec\" colname=\"c12\" colnum=\"12\"\u003e\u003c/div\u003e \u003cthead\u003e \u003ctr\u003e \u003cth align=\"left\" colname=\"c1\" morerows=\"1\" rowspan=\"2\"\u003e \u003cp\u003eLocation Name\u003c/p\u003e \u003c/th\u003e \u003cth align=\"left\" colname=\"c2\" morerows=\"1\" rowspan=\"2\"\u003e \u003cp\u003eSample No.\u003c/p\u003e \u003c/th\u003e \u003cth align=\"left\" colname=\"c3\" morerows=\"1\" rowspan=\"2\"\u003e \u003cp\u003eDepth (cm)\u003c/p\u003e \u003c/th\u003e \u003cth align=\"left\" colspan=\"3\" nameend=\"c6\" namest=\"c4\"\u003e \u003cp\u003eMagnetic Concentration\u003c/p\u003e \u003c/th\u003e \u003cth align=\"left\" colspan=\"3\" nameend=\"c9\" namest=\"c7\"\u003e \u003cp\u003eMagnetic Composition\u003c/p\u003e \u003c/th\u003e \u003cth align=\"left\" colspan=\"3\" nameend=\"c12\" namest=\"c10\"\u003e \u003cp\u003eMagnetic Grain Size\u003c/p\u003e \u003c/th\u003e \u003c/tr\u003e \u003ctr\u003e \u003cth align=\"left\" colname=\"c4\"\u003e \u003cp\u003eχ\u003c/p\u003e \u003cp\u003e10\u003csup\u003e\u0026minus;\u0026thinsp;7\u003c/sup\u003e\u003c/p\u003e \u003cp\u003em\u003csup\u003e3\u003c/sup\u003e kg\u003csup\u003e\u0026minus;\u0026thinsp;1\u003c/sup\u003e\u003c/p\u003e \u003c/th\u003e \u003cth align=\"left\" colname=\"c5\"\u003e \u003cp\u003eSIRM\u003c/p\u003e \u003cp\u003e10\u003csup\u003e\u0026minus;\u0026thinsp;2\u003c/sup\u003e\u003c/p\u003e \u003cp\u003eAm\u003csup\u003e2\u003c/sup\u003ekg\u003csup\u003e\u0026minus;\u0026thinsp;1\u003c/sup\u003e\u003c/p\u003e \u003c/th\u003e \u003cth align=\"left\" colname=\"c6\"\u003e \u003cp\u003eARM\u003c/p\u003e \u003cp\u003e10\u003csup\u003e\u0026minus;\u0026thinsp;5\u003c/sup\u003e\u003c/p\u003e \u003cp\u003eAm\u003csup\u003e2\u003c/sup\u003ekg\u003csup\u003e\u0026minus;\u0026thinsp;1\u003c/sup\u003e\u003c/p\u003e \u003c/th\u003e \u003cth align=\"left\" colname=\"c7\"\u003e \u003cp\u003eSoft\u003c/p\u003e \u003cp\u003eIRM\u003c/p\u003e \u003cp\u003e10\u003csup\u003e\u0026minus;\u0026thinsp;5\u003c/sup\u003e\u003c/p\u003e \u003cp\u003eAm\u003csup\u003e2\u003c/sup\u003ekg\u003csup\u003e\u0026minus;\u0026thinsp;1\u003c/sup\u003e\u003c/p\u003e \u003c/th\u003e \u003cth align=\"left\" colname=\"c8\"\u003e \u003cp\u003eHard IRM\u003c/p\u003e \u003cp\u003e10\u003csup\u003e\u0026minus;\u0026thinsp;5\u003c/sup\u003e\u003c/p\u003e \u003cp\u003eAm\u003csup\u003e2\u003c/sup\u003ekg\u003csup\u003e\u0026minus;\u0026thinsp;1\u003c/sup\u003e\u003c/p\u003e \u003c/th\u003e \u003cth align=\"left\" colname=\"c9\"\u003e \u003cp\u003eS ratio\u003c/p\u003e \u003c/th\u003e \u003cth align=\"left\" colname=\"c10\"\u003e \u003cp\u003eχ\u003csub\u003efd\u003c/sub\u003e\u003c/p\u003e \u003cp\u003e%\u003c/p\u003e \u003c/th\u003e \u003cth align=\"left\" colname=\"c11\"\u003e \u003cp\u003eARM /\u003c/p\u003e \u003cp\u003eSIRM\u003c/p\u003e \u003cp\u003e(10\u003csup\u003e\u0026minus;\u0026thinsp;3\u003c/sup\u003e)\u003c/p\u003e \u003c/th\u003e \u003cth align=\"left\" colname=\"c12\"\u003e \u003cp\u003eSIRM/χ\u003c/p\u003e \u003cp\u003e10\u003csup\u003e2\u003c/sup\u003e\u003c/p\u003e \u003cp\u003eAm\u003csup\u003e\u0026minus;\u0026thinsp;1\u003c/sup\u003e\u003c/p\u003e \u003c/th\u003e \u003c/tr\u003e \u003c/thead\u003e \u003ctbody\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e \u003cp\u003eSalaya\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e1\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e0\u0026ndash;13\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e33.61\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e4.68\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e34.35\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e4163.37\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e1.78\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e1.00\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e2.16\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e7.33\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e139.37\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e2\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e13\u0026ndash;26\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e34.33\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e4.92\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e32.89\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e4161.69\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e5.91\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e1.00\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e1.94\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e6.69\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e143.29\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e3\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e26\u0026ndash;39\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e44.47\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e6.56\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e52.34\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e5212.19\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e29.31\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e1.00\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e2.14\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e7.97\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e147.59\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e4\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e39\u0026ndash;52\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e35.50\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e4.94\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e38.48\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e4058.37\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e65.33\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.99\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e2.31\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e7.78\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e139.26\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e5\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e52\u0026ndash;65\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e11.19\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e1.49\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e14.12\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e1175.01\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e83.21\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.94\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e2.86\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e9.50\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e132.72\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e6\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e65\u0026ndash;78\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e28.29\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e4.49\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e28.50\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e3726.24\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e105.49\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.98\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e2.32\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e6.35\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e158.57\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e7\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e78\u0026ndash;91\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e11.30\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e1.52\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e13.62\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e1223.84\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e68.86\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.95\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e2.62\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e8.98\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e134.15\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e8\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e91\u0026ndash;104\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e3.93\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e0.38\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e3.91\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e290.238\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e36.30\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.90\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e2.15\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e10.31\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e96.50\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e \u003cp\u003eSikka P.\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e9\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e0\u0026ndash;13\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e26.48\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e3.34\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e20.20\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e2985.01\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e9.81\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e1.00\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e2.31\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e6.04\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e126.23\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e10\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e13\u0026ndash;26\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e50.49\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e6.04\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e35.29\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e5664.36\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e164.91\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.97\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e1.85\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e5.85\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e119.54\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e11\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e26\u0026ndash;39\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e51.29\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e6.02\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e42.72\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e5928.7\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e201.83\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.97\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e2.19\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e7.10\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e117.39\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e12\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e39\u0026ndash;52\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e86.20\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e10.42\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e63.88\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e10000.5\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e114.27\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.99\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e1.98\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e6.13\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e120.89\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e13\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e52\u0026ndash;65\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e42.84\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e3.23\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e28.46\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e1255.7\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e12.84\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e1.00\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e1.69\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e8.82\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e75.30\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e14\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e65\u0026ndash;78\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e54.67\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e4.31\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e43.23\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e1223.15\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e72.67\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.98\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e1.91\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e10.03\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e78.84\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e15\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e78\u0026ndash;91\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e55.56\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e4.42\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e47.96\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e825.339\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e43.86\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.99\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e2.00\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e10.85\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e79.55\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e16\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e91\u0026ndash;104\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e48.44\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e3.98\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e43.89\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e834.183\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e93.30\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.98\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e1.76\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e11.02\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e82.26\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e \u003cp\u003eBedi P.\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e17\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e0\u0026ndash;13\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e66.63\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e13.33\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e52.12\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e8145.57\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e247.28\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.98\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e2.69\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e3.91\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e200.02\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e18\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e13\u0026ndash;26\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e57.20\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e13.06\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e43.66\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e7224.11\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e176.78\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.99\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e2.86\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e3.34\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e228.30\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e19\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e26\u0026ndash;39\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e33.69\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e6.31\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e33.45\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e3761.16\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e194.43\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.97\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e3.12\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e5.30\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e187.33\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e20\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e39\u0026ndash;52\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e32.39\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e5.61\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e31.74\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e3846.33\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e19.50\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e1.00\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e2.44\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e5.65\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e173.34\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e21\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e52\u0026ndash;65\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e30.06\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e5.18\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e31.55\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e3812.44\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e182.31\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.96\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e3.63\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e6.09\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e172.44\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e22\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e65\u0026ndash;78\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e4.41\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e0.64\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e5.58\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e314.618\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e157.70\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.75\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e6.42\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e8.73\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e144.98\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e23\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e78\u0026ndash;91\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e1.92\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e0.28\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e1.05\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e53.0491\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e228.81\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.17\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e6.19\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e3.80\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e144.37\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e24\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e91\u0026ndash;104\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e1.99\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e0.29\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e0.60\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e20.4985\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e156.30\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.46\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e5.30\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e2.07\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e146.45\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e \u003cp\u003eJodiya\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e25\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e0\u0026ndash;13\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e24.86\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e2.50\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e39.01\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e2284.7\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e79.62\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.97\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e3.77\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e15.58\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e100.72\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e26\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e13\u0026ndash;26\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e21.20\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e2.24\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e33.51\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e2048.33\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e68.02\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.97\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e3.41\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e14.93\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e105.87\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e27\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e26\u0026ndash;39\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e17.70\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e1.76\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e24.44\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e1568.45\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e70.07\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.96\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e3.28\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e13.88\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e99.48\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e28\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e39\u0026ndash;52\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e18.36\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e1.85\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e24.98\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e1645.85\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e65.29\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.96\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e3.36\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e13.52\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e100.67\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e29\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e52\u0026ndash;65\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e15.48\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e1.54\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e22.08\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e1387.27\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e65.23\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.96\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e3.14\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e14.32\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e99.61\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e30\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e65\u0026ndash;78\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e17.33\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e1.82\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e23.25\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e1630.67\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e82.36\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.95\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e1.88\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e12.81\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e105.17\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e31\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e78\u0026ndash;91\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e15.16\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e1.51\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e19.83\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e1396.15\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e78.04\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.95\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e2.51\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e13.14\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e99.55\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e32\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e91\u0026ndash;104\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e3.35\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e0.33\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e4.15\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e251.302\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e74.40\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.77\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e2.84\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e12.58\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e98.41\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e \u003cp\u003eNav. P.\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e33\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e0\u0026ndash;13\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e14.23\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e1.54\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e22.22\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e1407.96\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e130.57\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.91\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e2.22\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e14.48\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e107.88\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e34\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e13\u0026ndash;26\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e13.89\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e1.52\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e20.94\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e1353.97\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e131.75\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.91\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e2.24\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e13.74\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e109.71\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e35\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e26\u0026ndash;39\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e13.91\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e1.48\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e24.23\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e1333.76\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e116.97\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.92\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e2.29\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e16.41\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e106.18\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e36\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e39\u0026ndash;52\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e14.11\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e1.43\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e28.85\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e1311.04\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e114.20\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.92\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e2.32\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e20.20\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e101.25\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e37\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e52\u0026ndash;65\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e12.51\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e1.32\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e24.49\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e1192.72\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e117.23\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.91\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e2.25\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e18.57\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e105.38\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e38\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e65\u0026ndash;78\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e10.14\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e1.01\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e22.35\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e966.627\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e96.95\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.90\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e2.80\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e22.14\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e99.49\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e39\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e78\u0026ndash;91\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e9.48\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e0.91\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e20.95\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e894.167\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e88.73\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.90\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e2.22\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e22.92\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e96.46\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e40\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e91\u0026ndash;104\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e12.51\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e1.27\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e17.70\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e1210.46\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e108.09\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.91\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e2.09\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e13.94\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e101.48\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e \u003cp\u003eKasampir\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e41\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e0\u0026ndash;13\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e9.19\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e0.91\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e17.17\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e863.664\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e86.87\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.90\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e1.52\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e18.80\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e99.42\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e42\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e13\u0026ndash;26\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e9.57\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e0.91\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e16.75\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e841.158\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e76.10\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.92\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e2.35\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e18.47\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e94.73\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e43\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e26\u0026ndash;39\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e9.51\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e0.88\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e18.60\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e829.254\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e22.50\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.97\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e2.27\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e21.15\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e92.51\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e44\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e39\u0026ndash;52\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e11.08\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e1.11\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e24.77\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e1012.22\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e83.00\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.93\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e2.07\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e22.33\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e100.15\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e45\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e52\u0026ndash;65\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e12.53\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e1.24\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e28.26\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e1151.16\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e84.54\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.93\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e2.37\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e22.79\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e99.02\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e46\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e65\u0026ndash;78\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e12.72\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e1.27\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e20.54\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e1216.66\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e88.26\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.93\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e2.44\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e16.12\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e100.14\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e47\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e78\u0026ndash;91\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e12.32\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e1.27\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e17.17\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e1215.92\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e92.43\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.93\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e2.77\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e13.56\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e102.81\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e48\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e91\u0026ndash;104\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e7.78\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e0.75\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e8.62\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e702.92\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e48.49\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.94\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e1.32\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e11.46\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e96.71\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e \u003cp\u003eKandla\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e49\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e0\u0026ndash;13\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e8.91\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e0.95\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e16.24\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e865.023\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e72.43\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.92\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e0.86\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e17.05\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e106.99\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e50\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e13\u0026ndash;26\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e8.87\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e0.87\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e15.97\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e795.426\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e67.37\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.92\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e0.89\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e18.27\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e98.51\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e51\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e26\u0026ndash;39\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e8.55\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e0.86\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e18.77\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e770.089\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e66.48\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.92\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e0.20\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e21.95\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e100.02\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e52\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e39\u0026ndash;52\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e9.80\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e0.96\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e22.53\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e878.756\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e70.58\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.93\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e1.18\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e23.37\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e98.43\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e53\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e52\u0026ndash;65\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e5.27\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e0.48\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e13.89\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e446.22\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e46.30\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.90\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e0.23\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e28.81\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e91.57\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e54\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e65\u0026ndash;78\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e2.43\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e0.15\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e4.14\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e140.712\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e17.52\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.89\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e1.16\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e26.86\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e63.58\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e55\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e78\u0026ndash;91\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e1.39\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e0.04\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e0.81\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e32.0763\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e6.56\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.85\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e0.45\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e18.70\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e31.27\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e56\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e91\u0026ndash;104\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e1.26\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e0.04\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e0.74\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e25.4537\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e4.48\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.89\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e0.29\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e18.29\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e32.09\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e \u003cp\u003eTuna P.\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e57\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e0\u0026ndash;13\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e20.52\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e2.61\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e22.19\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e2503.31\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e283.67\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.89\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e2.43\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e8.49\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e127.31\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e58\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e13\u0026ndash;26\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e32.15\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e3.97\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e28.47\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e3597.75\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e322.05\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.92\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e2.71\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e7.17\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e123.55\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e59\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e26\u0026ndash;39\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e12.02\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e1.47\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e18.54\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e1425.66\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e121.86\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.92\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e2.02\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e12.65\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e121.93\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e60\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e39\u0026ndash;52\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e1.81\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e0.11\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e1.74\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e99.8983\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e12.50\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.89\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e0.77\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e15.63\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e61.58\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e61\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e52\u0026ndash;65\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e7.63\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e0.89\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e13.83\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e844.38\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e76.34\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.91\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e0.38\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e15.59\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e116.31\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e62\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e65\u0026ndash;78\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e5.98\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e0.63\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e9.35\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e611.199\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e50.55\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.92\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e0.54\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e14.80\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e105.72\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e63\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e78\u0026ndash;91\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e6.66\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e0.76\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e10.92\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e750.537\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e59.67\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.92\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e0.19\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e14.39\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e113.93\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e64\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e91\u0026ndash;104\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e12.00\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e1.59\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e14.16\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e1510.57\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e165.27\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.90\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e0.33\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e8.90\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e132.58\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e \u003cp\u003eAdani P.\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e65\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e0\u0026ndash;13\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e9.47\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e1.08\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e11.55\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e1066.89\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e59.92\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.94\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e1.48\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e10.67\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e114.34\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e66\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e13\u0026ndash;26\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e10.15\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e1.19\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e11.19\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e1136.61\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e60.04\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.95\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e2.21\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e9.39\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e117.37\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e67\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e26\u0026ndash;39\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e11.30\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e1.44\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e13.47\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e1372.47\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e76.64\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.95\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e2.66\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e9.36\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e127.41\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e68\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e39\u0026ndash;52\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e13.03\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e1.73\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e14.99\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e1672.29\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e74.13\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.96\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e2.40\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e8.67\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e132.65\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e69\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e52\u0026ndash;65\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e7.12\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e0.79\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e8.33\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e783.68\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e40.93\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.95\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e0.31\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e10.51\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e111.27\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e70\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e65\u0026ndash;78\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e1.97\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e0.12\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e1.72\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e122.629\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e9.90\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.92\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e0.73\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e13.99\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e62.68\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e71\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e78\u0026ndash;91\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e1.34\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e0.05\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e1.04\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e41.9403\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e5.22\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.89\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e2.16\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e21.44\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e36.10\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e72\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e91\u0026ndash;104\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e1.18\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e0.04\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e0.76\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e31.0844\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e3.09\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.93\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e1.84\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e17.58\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e36.78\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e \u003cp\u003eModhva\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e73\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e0\u0026ndash;13\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e12.76\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e2.11\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e10.97\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e2001.23\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e79.24\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.96\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e1.80\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e5.19\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e165.69\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e74\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e13\u0026ndash;26\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e9.75\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e1.57\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e9.69\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e1516.98\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e84.66\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.95\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e1.03\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e6.19\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e160.60\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e75\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e26\u0026ndash;39\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e7.35\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e1.25\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e7.42\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e1127.51\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e50.73\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.96\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e1.29\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e5.92\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e170.52\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e76\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e39\u0026ndash;52\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e14.65\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e2.46\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e11.59\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e2258.97\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e138.93\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.94\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e0.80\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e4.71\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e168.07\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e77\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e52\u0026ndash;65\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e10.71\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e1.70\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e9.46\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e1572.04\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e53.05\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.97\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e0.89\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e5.57\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e158.72\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e78\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e65\u0026ndash;78\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e13.56\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e2.19\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e11.34\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e2036.48\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e69.79\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.97\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e0.89\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e5.18\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e161.49\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e79\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e78\u0026ndash;91\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e11.20\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e1.88\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e10.36\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e1783.65\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e51.41\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.97\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e0.57\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e5.51\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e167.66\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003ctr\u003e \u003ctd align=\"left\" colname=\"c1\"\u003e\u0026nbsp;\u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c2\"\u003e \u003cp\u003e80\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"left\" colname=\"c3\"\u003e \u003cp\u003e91\u0026ndash;104\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c4\"\u003e \u003cp\u003e10.15\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c5\"\u003e \u003cp\u003e1.73\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c6\"\u003e \u003cp\u003e10.41\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c7\"\u003e \u003cp\u003e1620.83\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c8\"\u003e \u003cp\u003e54.19\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c9\"\u003e \u003cp\u003e0.97\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c10\"\u003e \u003cp\u003e1.05\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c11\"\u003e \u003cp\u003e6.01\u003c/p\u003e \u003c/td\u003e \u003ctd align=\"char\" char=\".\" colname=\"c12\"\u003e \u003cp\u003e170.63\u003c/p\u003e \u003c/td\u003e \u003c/tr\u003e \u003c/tbody\u003e \u003c/colgroup\u003e \u003c/table\u003e\u003c/div\u003e \u003c/p\u003e \u003cp\u003e \u003c/p\u003e \u003cp\u003e \u003c/p\u003e \u003cp\u003e \u003c/p\u003e \u003cp\u003eVariations in the content of ferrimagnetic minerals (Magnetite or titanium magnetite) generally can be indicated by changes in \u003cb\u003eχ\u003c/b\u003e, ARM and SIRM. Higher magnetic susceptibility significantly shows presence of ferrimagnetic minerals. However, \u003cb\u003eχ\u003c/b\u003e can be good indicator of magnetic mineral concentration of samples, whereas concentration of stable single domain ferrimagnetic minerals is shown by ARM and concentration of saturated ferrimagnetic minerals is given by SIRM (Maher et al., \u003cspan citationid=\"CR31\" class=\"CitationRef\"\u003e2009\u003c/span\u003e). The surface sediments of GoK are studied for distinguishing between different source areas of terrigenous sediments to the GoK (Prizomwala et al., \u003cspan citationid=\"CR34\" class=\"CitationRef\"\u003e2014\u003c/span\u003e). Here for the first time the mineral magnetic measurements are studied to observe the magnetic mineral behaviour in the subsurface sediments of GoK, Gujarat.\u003c/p\u003e \u003cp\u003eMagnetic susceptibility (Fig.\u0026nbsp;2a) measurements at various locations in the GoK indicate decreasing magnetic susceptibility with depth in the mudflats. ARM also shows similar trend like magnetic susceptibility, it also decreases with depth (Fig.\u0026nbsp;2b). ARM decreases with depth at various locations including Salaya, Sikka Port, Bedi Port, Jodiya, Adani Port, Navlakhi Port, Kasampir, Modhva, Kandla Port, and Tuna Port. ARM values show variation with the top and bottom sample locations at different places. For instance, at Salaya, the top sample has a higher ARM value, while at Sikka Port, the bottom sample has a higher ARM value.\u003c/p\u003e \u003cp\u003eSIRM value decreases with depth. Magnetic concentration parameters decrease every 13 cm, except at Sikka Port. Presence of ferrimagnetic minerals in Mudflats of GoK. The top samples are rich in ferrimagnetic minerals, while the bottom samples have low concentrations.\u003c/p\u003e\n\u003ch3\u003eMagnetic mineralogy\u003c/h3\u003e\n\u003cp\u003eMagnetic mineralogy (or composition) dependent parameters are Soft IRM, Hard IRM and S-ratio. The S-ratio is a dimensionless parameter that indicates presence of ferrimagnetic minerals and anti-ferromagnetic minerals. The S-ratio can be used to differentiate between \u0026lsquo;magnetite\u0026rsquo; and \u0026lsquo;hematite\u0026rsquo; (\u0026ldquo;soft\u0026rdquo; IRM and \u0026ldquo;hard\u0026rdquo; IRM; with respect to a saturating forward IRM and various back fields IRMs). S\u003csub\u003e300\u003c/sub\u003e in particular is used as indicator for the magnetite-hematite ratio. S-ratio value of 1 for pure magnetite and it decreases with increasing proportion of antiferromagnetic particles such as hematite. Magnetite completely saturates at 300mT field and hematite is (more) harder, yielding lower S-ratios.\u003c/p\u003e \u003cp\u003eMagnetic minerals in sediments can be recognized as soft and hard fractions. The soft fraction shows low coercivity and can be used to find the concentration of magnetite (Thompson and Oldfield, \u003cspan citationid=\"CR43\" class=\"CitationRef\"\u003e1986\u003c/span\u003e); whereas the hard fractions show high coercivity and is expected to approximate to the total concentration of canted antiferromagnetic minerals (hematite) (Oldfield and Richardson, \u003cspan citationid=\"CR33\" class=\"CitationRef\"\u003e1990\u003c/span\u003e). Figure\u0026nbsp;\u003cspan refid=\"Fig1\" class=\"InternalRef\"\u003e3\u003c/span\u003e depicts the variation in magnetic properties at each port.\u003c/p\u003e \u003cp\u003eThe range of S- ratio for Mudflats of GoK is 0.26 to 1.00 (Fig.\u0026nbsp;2c). Out of 80 samples only 2 samples show the S-ratio of \u0026lt;\u0026thinsp;0.50 i.e. 0.41 (sample no. 23, depth 78-91cm) and 0.26 (sample no. 24, depth 91-104cm) from Bedi Port, indicating the presence of antiferromagnetic minerals (hematite). The average S-ratio of 78 samples is 0.94, dominantly showing the presence of ferrimagnetic minerals (magnetite). Soft IRM varies from 20-10000 \u0026times; 10\u003csup\u003e\u0026minus;\u0026thinsp;5\u003c/sup\u003e Am\u003csup\u003e2\u003c/sup\u003ekg\u003csup\u003e\u0026minus;\u0026thinsp;1\u003c/sup\u003e(Fig.\u0026nbsp;2d). Hard IRM varies from 1.8-426.8 \u0026times; 10\u003csup\u003e\u0026minus;\u0026thinsp;5\u003c/sup\u003e Am\u003csup\u003e2\u003c/sup\u003ekg\u003csup\u003e\u0026minus;\u0026thinsp;1\u003c/sup\u003e (Fig.\u0026nbsp;2e).\u003c/p\u003e \u003cp\u003eSample no. 23 and 24 from Bedi Port shows a contrastingly different magnetic assemblage, with higher Hard IRM and low S-ratio values indicating dominant high coercivity and antiferromagnetic minerals (i.e. hematite). All other locations show high Soft IRM and high S-ratio values indicating dominant low coercivity and ferrimagnetic minerals assemblage (i.e. magnetite).\u003c/p\u003e\n\u003ch3\u003eGrain size of magnetic minerals\u003c/h3\u003e\n\u003cp\u003eThe parameters of χ\u003csub\u003efd\u003c/sub\u003e %, ARM/SIRM, and SIRM/χ are used for identifying magnetic grain size in a sample. Small grains have a different number of magnetic domains-zones with a uniform magnetization direction within a grain than large grains of the same magnetic minerals. Hence, magnetic properties that reflect the domain structure are grain size indicators. From the smallest grain size to the largest, four main domain structure types are distinguished: superparamagnetic [SP, smallest grains (0.001\u0026ndash;0.01 mm)], stable single domain [SSD, slightly larger grains (~\u0026thinsp;0.03 - ~ 0.50 mm)], pseudo single- domain [PSD, larger grains (~\u0026thinsp;10 mm)] and multidomain [MD, largest grains (\u0026thinsp;\u0026gt;\u0026thinsp;~\u0026thinsp;10 mm)]. The magnetic remanence of SSD grain assemblage is higher and more stable than that of MD grain. Single-domain grains contain one magnetic domain and are paleomagnetically most stable.\u003c/p\u003e \u003cp\u003e \u003c/p\u003e \u003cp\u003eFor the present study, all average ARM/SIRM value is 12.30\u0026times;10\u003csup\u003e\u0026minus;\u0026thinsp;3\u003c/sup\u003e which indicates the presence of relatively finer ferrimagnetic grain assemblages or significant SSD (magnetite) grains. Lowest values are observed at Bedi Port (2.07\u0026times;10\u003csup\u003e\u0026minus;\u0026thinsp;3\u003c/sup\u003e) and highest value at Kandla Port (28.81\u0026times;10\u003csup\u003e\u0026minus;\u0026thinsp;3\u003c/sup\u003e) indicating presence of coarser ferrimagnetic assemblages or indicate a large MD (magnetite) grains.\u003c/p\u003e \u003cp\u003e \u003c/p\u003e \u003cp\u003eχ\u003csub\u003efd\u003c/sub\u003e% of 2.04% indicates negligible contributions from superparamagnetic grains. High ARM/SIRM values denote significantly presence of SSD (magnetite) grains and SIRM/χ ratio reflects the absence of MD grain.\u003c/p\u003e \u003cp\u003e \u003c/p\u003e \u003cp\u003eThe spatial distribution of magnetic susceptibility (χ) and organic matter in the surface sediments (Fig.\u0026nbsp;\u003cspan refid=\"Fig2\" class=\"InternalRef\"\u003e4\u003c/span\u003e) reveals environmental gradients influenced by both natural and anthropogenic factors. Sampling stations such as Sikka Port and Bedi Port exhibit elevated magnetic susceptibility values (often\u0026thinsp;\u0026gt;\u0026thinsp;40,000 SI units) accompanied by low organic matter content, indicative of substantial industrial influence, likely from harbor activities and effluent discharge introducing ferrimagnetic particles such as magnetite. The reduced organic content in these locations may be attributed to oxidative degradation or dilution by mineral-rich industrial inputs. In contrast, stations like Salaya and Kandla display moderate values for both χ and organic matter, suggesting a dynamic interplay between natural sedimentation processes and moderate anthropogenic inputs. Meanwhile, more pristine or naturally influenced environments are represented by sites such as Jodiya, Kasampir, and Modhva, which show low magnetic susceptibility alongside variable but generally higher organic matter concentrations, likely reflecting coastal or fluvial depositional dynamics with minimal industrial disturbance. These variations underscore the utility of environmental magnetic parameters as proxies for identifying pollution hotspots and understanding sedimentary processes within complex coastal systems.\u003c/p\u003e"},{"header":"Conclusions","content":"\u003cp\u003eThe magnetic mineralogical composition of surface sediments retrieved from the Gulf of Kutch is predominantly dictated by ferrimagnetic constituents, principally magnetite, accompanied by subordinate quantities of hematite. The assemblage is typified by a coexistence of stable single domain (SSD) and multi-domain (MD) grain states, reflecting a bimodal grain-size distribution potentially influenced by both natural and anthropogenic processes. Among the suite of magnetic parameters assessed, the anhysteretic remanent magnetization susceptibility (χARM) and its ratio to bulk magnetic susceptibility (χARM/χ) emerge as particularly robust diagnostic indicators, capable of discerning variations in sediment provenance and pollution loading with high sensitivity.\u003c/p\u003e \u003cp\u003eMultivariate correlation analyses between magnetic parameters and concentrations of major geochemical elements elucidate spatially heterogeneous patterns of magnetic enhancement, which, in turn, suggest differential anthropogenic influences across the region. Sites such as Navlakhi and Kandla exhibit conspicuously elevated values of χ, SIRM, and χARM/χ, implying a significant enrichment in fine-grained ferrimagnetic particles most plausibly attributable to industrial effluents, combustion by-products, and urban runoff derived from adjacent infrastructural and manufacturing hubs. These geochemical-magnetic anomalies designate these locales as potential pollution epicenters or \u0026lsquo;hotspots,\u0026rsquo; wherein the anthropogenic magnetic signal overrides the detrital background.\u003c/p\u003e \u003cp\u003eIn contrast, the magnetic response from Modhva is emblematic of a more quiescent environmental setting, wherein the predominance of natural sedimentary dynamics modulated by coastal hydrodynamic regimes and/or fluvial deposition dampens the influence of external anthropogenic magnetic contributions. Additional locales such as Salaya and Jodiya, while not exhibiting uniformly elevated magnetic intensities, demonstrate high χARM/χ values, potentially reflective of the aeolian or atmospheric deposition of ultrafine magnetic particulates, likely sourced from regional industrial or urban emissions.\u003c/p\u003e \u003cp\u003eCollectively, the magnetic dataset delineates a nuanced environmental gradient wherein magnetic susceptibility metrics function as sensitive, non-invasive proxies for sedimentary pollution assessment. This magnetic fingerprinting, therefore, constitutes a critical prelude to more exhaustive geochemical investigations and offers a strategic framework for environmental monitoring and remediation prioritization within the Gulf of Kutch.\u003c/p\u003e"},{"header":"Declarations","content":"\u003ch2\u003eDeclaration of Competing Interest\u003c/h2\u003e\n\u003cp\u003eThe authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper.\u003c/p\u003e\n\u003ch2\u003eFunding\u003c/h2\u003e\n\u003cp\u003eThis research did not receive any specific grant from funding agencies in the public, commercial, or not-for-profit sectors.\u003c/p\u003e\n\u003ch2\u003eAuthor Contribution\u003c/h2\u003e\n\u003cp\u003eSanjida A. Khan wrote the main manuscript text and reviewed the manuscript.Suvarna Naikuji prepared figures and reviewed the manuscript.\u003c/p\u003e\n\u003ch2\u003eAcknowledgements\u003c/h2\u003e\n\u003cp\u003eThe authors are thankful to Dr. C. Rajshekhar, former Head, Department of Paleontology, ARI, Pune for his valuable suggestions during research work.\u003c/p\u003e"},{"header":"References","content":"\u003col\u003e\n\u003cli\u003eA. Kapicka, N. Jordanova, E. Petrovsk\u0026yacute; and V. Podr\u0026aacute;zsk\u0026yacute;, 2003. Magnetic Study of Weakly Contaminated Forest Soils. \u003cem\u003eWater, Air, and Soil Pollution \u003c/em\u003e148:31\u0026ndash;44.\u003c/li\u003e\n\u003cli\u003eBasavaiah N., 2011. Experimental Geomagnetism, Geomagnetism: Solid Earth and Upper Atmosphere Perspectives. Springer publisher, Netherland, 291-386.\u003c/li\u003e\n\u003cli\u003eBloemendal, J., King, J.W., Hall, F.R., Doh, S.J., 1992. Rock magnetism of Late Neogene and Pleistocene deepsea sediments: Relationship to sediment source, diagenetic processes, and sediment lithology. J. Geophys. Res. 97, 4361.\u003c/li\u003e\n\u003cli\u003eBoltovskoy E., Wright R., 1976. Recent Foraminifera. \u003cem\u003eThe Hague. \u003c/em\u003eDr. W. Junk B.V. Publishers, 515 p.\u003c/li\u003e\n\u003cli\u003eClemens Reimann, Patrice de Caritat., 2005. Distinguishing between natural and anthropogenic sources for elements in the environment: regional geochemical surveys versus enrichment factors. Science of The Total Environment, 337(1\u0026ndash;3).\u003c/li\u003e\n\u003cli\u003eChaparro, M.A., Sinito, A.M., Ramasamy, V., Marinelli, C., Chaparro, M.A., Mullainathan, S., Murugesan, S., 2008. Magnetic measurements and pollutants of sediments from Cauvery and Palaru River, India. Environ. Geol. 56, 425.\u003c/li\u003e\n\u003cli\u003eChaparro, M.A., Chaparro, M.A., Rajkumar, P., Ramasamy, V., Sinito, A.M., 2011. Magnetic parameters, trace elements, and multivariate statistical studies of river sediments from southeastern India: a case study from the Vellar River. Environ. Earth Sci. 63 (2), 297\u0026ndash;310.\u003c/li\u003e\n\u003cli\u003eChaparro, M.A., Krishnamoorthy, N., Chaparro, M.A., Lecomte, K.L., Mullainathan, S., Mehra, R., Sinito, A.M., 2015. Magnetic, chemical and radionuclide studies of river sediments and their variation with different physiographic regions of Bharathapuzha River, southwestern India. Stud. Geophys. Geod. 59 (3), 438\u0026ndash;460.\u003c/li\u003e\n\u003cli\u003eChaparro, M.A., Sinito, A.M., Ramasamy, V., Marinelli, C., Chaparro, M.A., Mullainathan, S., Murugesan, S., 2008. Magnetic measurements and pollutants of sediments from Cauvery and Palaru River, India. Environ. Geol. 56, 425.\u003c/li\u003e\n\u003cli\u003eChauhan O. S., Vora K. H., 1990. Reflection Seismic Studies in the Macrotidal Gulf of Kachchh, India. Evidences of Physiographic Evolution. \u003cem\u003eContinental Shelf Research\u003c/em\u003e, 10(4), 385-396. \u003c/li\u003e\n\u003cli\u003eChen, Q., Liu, Z., Kissel, C., 2017. Clay mineralogical and geochemical proxies of the East Asian summer monsoon evolution in the South China Sea during Late Quaternary. Sci. Rep. 7, 42083.\u003c/li\u003e\n\u003cli\u003eDearing, J., 1999. Environmental magnetic susceptibility using the bartington MS2 system, second ed. Chinese Publications, Kenilworth.\u003c/li\u003e\n\u003cli\u003eDearing J., 1999. Magnetic Susceptibility, In: Walden J., Oldfield F., and Smith J. P., (eds) Environmental Magnetism: a practical guide: Technical Guide No. 6, Quaternary Research Association, London, 250 p.\u003c/li\u003e\n\u003cli\u003eE. Petrovsk\u0026yacute;, A. Kapicˇka, N. Jordanova, M. Knab, V. Hoffmann, 2000. Low-field magnetic susceptibility: a proxy method of estimating increased pollution of different environmental systems. Environmental Geology 39 (3\u0026ndash;4).\u003c/li\u003e\n\u003cli\u003eGIS (Geographical Information system), 2002. Government of India, Department of Ocean Development, ICMAM, Project Directorate, Chennai, 1-53.\u003c/li\u003e\n\u003cli\u003eGovil P., Naidu P. D., 2008. Late Quaternary changes in depositional processes along the western margin of the Indus Fan. \u003cem\u003eGeo-Marine Lett\u003c/em\u003e., 28, 1-6.\u003c/li\u003e\n\u003cli\u003eLiviu Giosana, Stefan Constantinescub , Peter D. Cliftc , Ali R. Tabrezd , Muhammed Danishd and Asif Inamd.,2006. Recent morphodynamics of the Indus delta shore and shelf. Continental Shelf Research 26,1668\u0026ndash;1684. https://doi:10.1016/j.csr.2006.05.009\u003c/li\u003e\n\u003cli\u003eHatfield, R.G., Maher, B.A., 2009. Fingerprinting upland sediment sources: particle sizespecific magnetic linkages between soils, lake sediments and suspended sediments. Earth Surf. Proc. Land. 34 (10), 1359\u0026ndash;1373.\u003c/li\u003e\n\u003cli\u003eHatfield, R.G., 2014. Particle size-specific magnetic measurements as a tool for enhancing our understanding of the bulk magnetic properties of sediments. Minerals 4 (4), 758\u0026ndash;787.\u003c/li\u003e\n\u003cli\u003eHatfield, R.G., Wheeler, B.H., Reilly, B.T., Stoner, J.S., Housen, B.A., 2019. Particle size specific magnetic properties across the norwegian-greenland seas: insights into the influence of sediment source and texture on bulk magnetic records. Geochem. Geophys. Geosyst. 20 (2), 1004\u0026ndash;1025.\u003c/li\u003e\n\u003cli\u003eHilgenfeldt, K. (2000). Diagenetic dissolution of biogenic magnetite in surface sediments of the Benguela upwelling system. \u003cem\u003eInternational Journal of Earth Sciences\u003c/em\u003e, \u003cem\u003e88\u003c/em\u003e(4), 630-640. https://doi.org/10.1007/s005310050293\u003c/li\u003e\n\u003cli\u003eHorng, C.S., Huh, C.A., 2011. Magnetic properties as tracers for source-to-sink dispersal of sediments: A case study in the Taiwan Strait. Earth Planet. Sci. Lett. 309, 141\u0026ndash;152.\u003c/li\u003e\n\u003cli\u003eJust, J., Dekkers, M. J., von Dobeneck, T., van Hoesel, A., \u0026amp; Bickert, T. (2012). Signatures and significance of aeolian, fluvial, bacterial and diagenetic magnetic mineral fractions in Late Quaternary marine sediments off Gambia, NW Africa. \u003cem\u003eGeochemistry\u003c/em\u003e, \u003cem\u003eGeophysics\u003c/em\u003e, \u003cem\u003eGeosystems\u003c/em\u003e, \u003cem\u003e13\u003c/em\u003e(9). https://doi.org /10.1029/2012gc004146\u003c/li\u003e\n\u003cli\u003eKing, J., Banerjee, S.K., Marvin, J., Ozdemir, O., 1982. A comparison of different magnetic methods for determining the relative grain size of magnetite in natural materials: some results from lake sediments. Earth Planet. Sci. Lett. 59, 404\u0026ndash;419.\u003c/li\u003e\n\u003cli\u003eKulkarni, Y.R., Sangode, S.J., Meshram, D.C., Patil, S.K., Dutt, Y., 2014. Mineral magnetic characterization of the Godavari River sediments: Implications to Deccan basalt weathering. J. Geol. Soc. India 83, 376\u0026ndash;384.\u003c/li\u003e\n\u003cli\u003eL.S Chan, S.L Ng, A.M Davis, W.W.S Yim, C.H Yeung., 2001. Magnetic Properties and Heavy-metal Contents of Contaminated Seabed Sediments of Penny\u0026apos;s Bay, Hong Kong. Marine Pollution bulletin. 42(7), 569-583.\u003c/li\u003e\n\u003cli\u003eLarrasoa\u0026ntilde;a, J. C., Roberts, A. P., Stoner, J. S., Richter, C., \u0026amp; Wehausen, R. (2003b). A new proxy for bottom-water ventilation in the eastern Mediterranean based on diagenetically controlled magnetic properties of sapropel-bearing sediments. \u003cem\u003ePalaeogeography\u003c/em\u003e, \u003cem\u003ePalaeoclimatology\u003c/em\u003e, \u003cem\u003ePalaeoecology\u003c/em\u003e, \u003cem\u003e190\u003c/em\u003e, 221-242. https://doi.org/10.1016/s0031-0182(02)00607-7\u003c/li\u003e\n\u003cli\u003eLiu, X., Li, A., Dong, J., Lu, J., Huang, J., Wan, S., 2018. Provenance discrimination of sediments in the Zhejiang-Fujian mud belt, East China Sea: Implications for the development of the mud depocenter. J. Asian Earth Sci. 151, 1\u0026ndash;15.\u003c/li\u003e\n\u003cli\u003eLiu, Q., Roberts, A.P., Larrasoana, \u0026tilde; J.C., Banerjee, S.K., Guyodo, Y., Tauxe, L., Oldfield, F., 2012. Environmental magnetism: principles and applications. Rev. Geophys. 50 (4).\u003c/li\u003e\n\u003cli\u003eLiviu Giosana, Stefan Constantinescub , Peter D. Cliftc , Ali R. Tabrezd , Muhammed Danishd , Asif Inamd.,2006. Recent morphodynamics of the Indus delta shore and shelf. Continental Shelf Research 26, 1668- 1684.\u003c/li\u003e\n\u003cli\u003eMaher B. A., Watkins S. J., Brunskill G., Alexander J. J., Fielding C. R., 2009. Sediment provenance in a tropical fluvial and marine context by magnetic \u0026lsquo;fingerprinting\u0026rsquo; of transportable sand fractions. \u003cem\u003eSedimentology\u003c/em\u003e, 56, 841-861.\u003c/li\u003e\n\u003cli\u003eMurray J. W., 2006. Ecology and Applications of Benthic Foraminifera; Cambridge University Press, 426 p.\u003c/li\u003e\n\u003cli\u003eOldfield F., Richardson N., 1990. Lake sediment magnetism and atmospheric deposition; Philos. \u003cem\u003eTrans. Roy. Soc. London\u003c/em\u003e \u003cem\u003eB\u003c/em\u003e, 327,325-330.\u003c/li\u003e\n\u003cli\u003ePrizomwala S. P., Bhatt N., Basavaiah N., 2014. Understanding the sediment routing system along the Gulf of Kachchh coast, western India: Significance of small ephemeral rivers. \u003cem\u003eJ. Earth Syst. Sci.,\u003c/em\u003e 123(1),121-133.\u003c/li\u003e\n\u003cli\u003eRoberts, A. P., Stoner, J. S., \u0026amp; Richter, C. (1999). Diagenetic magnetic enhancement of sapropels from the eastern Mediterranean Sea. \u003cem\u003eMarine Geology\u003c/em\u003e, \u003cem\u003e153\u003c/em\u003e(1-4), 103- 116. https://doi.org/10.1016/S0025-3227(98)00087-5\u003c/li\u003e\n\u003cli\u003eRoberts, A. P., Tauxe, L., \u0026amp; Heslop, D. (2013). Magnetic paleointensity stratigraphy and high-resolution Quaternary geochronology: Successes and future challenges.\u003cem\u003eQuaternary Science Reviews\u003c/em\u003e, \u003cem\u003e61\u003c/em\u003e, 1-16. https://doi.org/10.1016/ j.quascirev.2012.10.036\u003c/li\u003e\n\u003cli\u003eRobinson, S. G., Sahota, J. T., \u0026amp; Oldfield, F. (2000). Early diagenesis in North Atlantic abyssal plain sediments characterized by rock-magnetic and geochemical indices. \u003cem\u003eMarine Geology\u003c/em\u003e, \u003cem\u003e163\u003c/em\u003e(1-4), 77 107. https://doi.org/10.1016/s0025- 3227(99)00108-5\u003c/li\u003e\n\u003cli\u003eRowan, C. J., Roberts, A. P., \u0026amp; Broadbent, T. (2009). Reductive diagenesis, magnetite dissolution, greigite growth and paleomagnetic smoothing in marine sediments: A new view. \u003cem\u003eEarth and Planetary Science Letters\u003c/em\u003e, \u003cem\u003e277\u003c/em\u003e(1-2), 223-235. https://doi.org/10.1016/j.epsl.2008.10.016\u003c/li\u003e\n\u003cli\u003eSangode, S.J., Sinha, R., Phartiyal, B., Chauhan, O.S., Mazari, R.K., Bagati, T.N., Suresh, N., Mishra, S., Kumar, R., Bhattacharjee, P., 2007. Environmental magnetic studies on some Quaternary sediments of varied depositional settings in the Indian subcontinent. Quat. Int. 159, 102\u0026ndash;118.\u003c/li\u003e\n\u003cli\u003eSandeep, K., Shankar, R., Krishnaswamy, J., 2011. Assessment of suspended particulate pollution in the Bhadra River catchment, Southern India: an environmental magnetic approach. Environ. Earth Sci. 62, 625\u0026ndash;637.\u003c/li\u003e\n\u003cli\u003eSyvitski, J.P., Peckham, S.D., Hilberman, R., Mulder, T., 2003. Predicting the terrestrial flux of sediment to the global ocean: a planetary perspective. Sed. Geol. 162 (1),5\u0026ndash;24.\u003c/li\u003e\n\u003cli\u003eTarduno, J. A., \u0026amp; Wilkison, S. L. (1996). Non-steady state magnetic mineral reduction, chemical lock-in, and delayed remanence acquisition in pelagic sediments. \u003cem\u003eEarth\u003c/em\u003e \u003cem\u003eand Planetary Science Letters\u003c/em\u003e, \u003cem\u003e144\u003c/em\u003e(3-4), 315-326. https://doi.org/ 10.1016/s0012-821x(96)00174-4\u003c/li\u003e\n\u003cli\u003eThompson, R., Oldfield, R., 1986. Environmental Magnetism. Allen and Unwin, New York, pp. 227.\u003c/li\u003e\n\u003cli\u003eVan Hoof, A. A. M., Van Os, B. J. H., Rademakers, J. G., Langereis, C. G., \u0026amp; de Lange, G. J. (1993). A paleomagnetic and geochemical record of the upper Cochiti reversal and two subsequent processional cycles from Southern Sicily (Italy). \u003cem\u003eEarth and Planetary Science Letters\u003c/em\u003e, \u003cem\u003e117\u003c/em\u003e(1-2), 235-250. https://doi.org/10.1016/0012-821X(93)90130-2\u003c/li\u003e\n\u003c/ol\u003e"}],"fulltextSource":"","fullText":"","funders":[],"hasAdminPriorityOnWorkflow":false,"hasManuscriptDocX":true,"hasOptedInToPreprint":true,"hasPassedJournalQc":"","hasAnyPriority":false,"hideJournal":true,"highlight":"","institution":"","isAcceptedByJournal":false,"isAuthorSuppliedPdf":false,"isDeskRejected":"","isHiddenFromSearch":false,"isInQc":false,"isInWorkflow":false,"isPdf":false,"isPdfUpToDate":true,"isWithdrawnOrRetracted":false,"journal":{"display":true,"email":"[email protected]","identity":"researchsquare","isNatureJournal":false,"hasQc":true,"allowDirectSubmit":true,"externalIdentity":"","sideBox":"","snPcode":"","submissionUrl":"/submission","title":"Research Square","twitterHandle":"researchsquare","acdcEnabled":true,"dfaEnabled":false,"editorialSystem":"","reportingPortfolio":"","inReviewEnabled":false,"inReviewRevisionsEnabled":true},"keywords":"Gulf of Kachchh, anthropogenic, rock magnetics","lastPublishedDoi":"10.21203/rs.3.rs-6582332/v1","lastPublishedDoiUrl":"https://doi.org/10.21203/rs.3.rs-6582332/v1","license":{"name":"CC BY 4.0","url":"https://creativecommons.org/licenses/by/4.0/"},"manuscriptAbstract":"\u003cp\u003eThis study examines the environmental magnetic properties of 80 subsurface sediment samples from the mudflats along the Gulf of Kachchh coast, Gujarat, India. A 1.04-meter shallow core was obtained from ten distinct locations, considering the impact of anthropogenic activities on coastal sediments. Magnetic parameters were employed as proxies for assessing environmental pollution, particularly in identifying anthropogenic particles. The subsurface sediments in the Gulf of Kachchh (GOK) are primarily dominated by ferromagnetic minerals, likely magnetite. The χfd percentage indicates the presence of superparamagnetic/single-domain (SSD) magnetic minerals, while elevated ARM/SIRM values suggest a significant presence of SSD (magnetite) grains. Additionally, the SIRM/χ ratio indicates an absence of multidomain (MD) grains. This study demonstrates the utility of magnetic proxies in detecting regions with higher pollution levels, potentially associated with heavy metal contamination.\u003c/p\u003e","manuscriptTitle":"Environmental magnetic characterization of the sediments from shallow cores of Gulf of Kachchh, Gujarat, India","msid":"","msnumber":"","nonDraftVersions":[{"code":1,"date":"2025-06-02 09:57:00","doi":"10.21203/rs.3.rs-6582332/v1","editorialEvents":[{"type":"communityComments","content":0}],"status":"published","journal":{"display":true,"email":"[email protected]","identity":"researchsquare","isNatureJournal":false,"hasQc":true,"allowDirectSubmit":true,"externalIdentity":"","sideBox":"","snPcode":"","submissionUrl":"/submission","title":"Research Square","twitterHandle":"researchsquare","acdcEnabled":true,"dfaEnabled":false,"editorialSystem":"","reportingPortfolio":"","inReviewEnabled":false,"inReviewRevisionsEnabled":true}}],"origin":"","ownerIdentity":"ff6f23fd-9dd0-4fc3-b0db-b7c504503a70","owner":[],"postedDate":"June 2nd, 2025","published":true,"recentEditorialEvents":[],"rejectedJournal":[],"revision":"","amendment":"","status":"posted","subjectAreas":[],"tags":[],"updatedAt":"2025-08-11T14:23:57+00:00","versionOfRecord":[],"versionCreatedAt":"2025-06-02 09:57:00","video":"","vorDoi":"","vorDoiUrl":"","workflowStages":[]},"version":"v1","identity":"rs-6582332","journalConfig":"researchsquare"},"__N_SSP":true},"page":"/article/[identity]/[[...version]]","query":{"redirect":"/article/rs-6582332","identity":"rs-6582332","version":["v1"]},"buildId":"8U1c8b4HqxoKbykW_rLl7","isFallback":false,"isExperimentalCompile":false,"dynamicIds":[84888],"gssp":true,"scriptLoader":[]}