Development of predominant-period and average S-wave velocity maps for Hue City, Central Vietnam

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Abstract We have developed maps of the predominant period of the ground and average S-wave velocity to depths of 10, 20 and 30 m (VS10, 20 and 30) as the fundamental data for seismic hazard assessment for Hue City, Central Vietnam. We conducted microtremor single-station measurements at 461 sites and microtremor array measurements at 157 sites in and around the city (i.e., within an area of about 15 km x 15 km). The peak period of horizontal-to-vertical spectral ratios (HVSR) obtained from three-component microtremor waveforms at a single station were regarded as a S-wave predominant period of the ground. Rayleigh-wave phase velocity at wavelengths of 13, 25 and 40 m obtained from vertical-component array measurements were regarded as VS10, 20 and 30, respectively. It revealed that the predominant periods range from 0.03 to 1.98 s (i.e., 0.5 to 33 Hz) in Hue City, which show a tendency to be longer in the northern part of the city than in the southern part. The analysis results of the average S-wave velocity indicate that soft sediments are very thick in the northern part of the city, where VS10, 20 and 30 ranges from 149 to 189 m/s. These analysis results are consistent with an existing geological map and quantify the geoenvironmental conditions in Hue City, indicating the effectiveness of the microtremor measurements for a seismic assessment.
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Development of predominant-period and average S-wave velocity maps for Hue City, Central Vietnam | Research Square window.SnipcartSettings = { analytics: { enabled: false } }; (function() { var accessVector = localStorage.getItem('access_vector') || ''; window.dataLayer = window.dataLayer || []; if (accessVector) { window.dataLayer.push({ user: { profile: { profileInfo: { snid: accessVector } } } }); } })(); (function(w,d,s,l,i){w[l]=w[l]||[];w[l].push({'gtm.start':new Date().getTime(),event:'gtm.js'});var f=d.getElementsByTagName(s)[0],j=d.createElement(s),dl=l!='dataLayer'?'&l='+l:'';j.async=true;j.src='https://www.googletagmanager.com/gtm.js?id='+i+dl;f.parentNode.insertBefore(j,f);})(window,document,'script','dataLayer','GTM-K279D39R'); Browse Preprints In Review Journals COVID-19 Preprints AJE Video Bytes Research Tools Research Promotion AJE Professional Editing AJE Rubriq About Preprint Platform In Review Editorial Policies Our Team Advisory Board Help Center Sign In Submit a Preprint Cite Share Download PDF Research Article Development of predominant-period and average S-wave velocity maps for Hue City, Central Vietnam Duong Anh Nguyen, Ikuo Cho, Makoto Okubo, Tuan Minh Vu, Hai Thanh Nguyen, and 7 more This is a preprint; it has not been peer reviewed by a journal. https://doi.org/ 10.21203/rs.3.rs-5252201/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 We have developed maps of the predominant period of the ground and average S-wave velocity to depths of 10, 20 and 30 m (VS10, 20 and 30) as the fundamental data for seismic hazard assessment for Hue City, Central Vietnam. We conducted microtremor single-station measurements at 461 sites and microtremor array measurements at 157 sites in and around the city (i.e., within an area of about 15 km x 15 km). The peak period of horizontal-to-vertical spectral ratios (HVSR) obtained from three-component microtremor waveforms at a single station were regarded as a S-wave predominant period of the ground. Rayleigh-wave phase velocity at wavelengths of 13, 25 and 40 m obtained from vertical-component array measurements were regarded as VS10, 20 and 30, respectively. It revealed that the predominant periods range from 0.03 to 1.98 s (i.e., 0.5 to 33 Hz) in Hue City, which show a tendency to be longer in the northern part of the city than in the southern part. The analysis results of the average S-wave velocity indicate that soft sediments are very thick in the northern part of the city, where VS10, 20 and 30 ranges from 149 to 189 m/s. These analysis results are consistent with an existing geological map and quantify the geoenvironmental conditions in Hue City, indicating the effectiveness of the microtremor measurements for a seismic assessment. Shear-wave velocity microtremor array HVSR Hue City Central Vietnam. Full Text Supplementary Files graphicalabstractc2.png Cite Share Download PDF Status: Posted Version 1 posted You are reading this latest preprint version Research Square lets you share your work early, gain feedback from the community, and start making changes to your manuscript prior to peer review in a journal. As a division of Research Square Company, we’re committed to making research communication faster, fairer, and more useful. We do this by developing innovative software and high quality services for the global research community. Our growing team is made up of researchers and industry professionals working together to solve the most critical problems facing scientific publishing. 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