Impact of Mineral Interface Network Topology on the Micromechanical Properties of Central Quartz Grains in Shale: Rigid Constraint and Compliant Decoupling

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The paper studies how mineral interface network topology governs micromechanical properties of central quartz grains in Lower Cambrian Qiongzhusi Formation shale (Sichuan Basin) by combining high-resolution SEM-EDS with targeted nanoindentation to map local environments and quantify them using a proposed weighted interface constraint strength coefficient (C_eff). It reports that central quartz grains show substantial micromechanical variability (coefficient of variation >14%) that depends on whether interfaces form high-C_eff rigid interlocking networks (producing a “rigid constraint stiffening effect”) or low-C_eff weak wrapping networks (producing “compliant decoupling weakening” with interface debonding and reduced apparent properties). The authors further attribute constraint differentiation to competing diagenetic processes—chemical pressure solution versus mechanical compaction. This paper does not explicitly discuss endometriosis or adenomyosis; it was included in the corpus via a keyword match in the upstream search index.

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Abstract The accurate prediction of shale's macroscopic mechanical behavior has long been limited by insufficient understanding of its micro-scale heterogeneity. Traditional rock physics models often overlook micro-scale heterogeneity by assuming constant mineral properties, failing to explain the significant mechanical variability observed in experiments. To overcome the limitations of component-based analysis, we integrated high-resolution SEM-EDS with targeted nanoindentation to investigate how interface network topology controls the micromechanical response of central quartz grains in the Lower Cambrian Qiongzhusi Formation shale (Sichuan Basin, China). A "weighted interface constraint strength coefficient" ( C eff ) was proposed to quantify the local micromechanical environment. Results indicate that central quartz grains exhibit significant micromechanical property variability (CV > 14%), which is governed by the mineral interface network topology. Specifically, high -C eff rigid interlocking networks enhance the mechanical performance of central quartz grains through a "rigid constraint stiffening effect." Conversely, low- C eff weak wrapping networks trigger a "compliant decoupling weakening effect" inducing interface debonding and attenuating apparent mechanical properties of central quartz grains. Further analysis reveals that the variation in interface network constraints is essentially a micromechanical differentiation resulting from the competitive evolution between chemical pressure solution and mechanical compaction. The diagenetic evolution model of mineral interface network micromechanical differentiation established in this study lays a theoretical foundation for shifting shale brittleness evaluation from a "composition-oriented" to a "topology-oriented" paradigm, offering significant implications for identifying fracturing "sweet spots" in deep shale gas reservoirs.
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Impact of Mineral Interface Network Topology on the Micromechanical Properties of Central Quartz Grains in Shale: Rigid Constraint and Compliant Decoupling | 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 Impact of Mineral Interface Network Topology on the Micromechanical Properties of Central Quartz Grains in Shale: Rigid Constraint and Compliant Decoupling YUNFEI GUO, Hucheng Deng, Jianhua He, Ruixue Li This is a preprint; it has not been peer reviewed by a journal. https://doi.org/ 10.21203/rs.3.rs-8778143/v1 This work is licensed under a CC BY 4.0 License Status: Under Review Version 1 posted 6 You are reading this latest preprint version Abstract The accurate prediction of shale's macroscopic mechanical behavior has long been limited by insufficient understanding of its micro-scale heterogeneity. Traditional rock physics models often overlook micro-scale heterogeneity by assuming constant mineral properties, failing to explain the significant mechanical variability observed in experiments. To overcome the limitations of component-based analysis, we integrated high-resolution SEM-EDS with targeted nanoindentation to investigate how interface network topology controls the micromechanical response of central quartz grains in the Lower Cambrian Qiongzhusi Formation shale (Sichuan Basin, China). A "weighted interface constraint strength coefficient" ( C eff ) was proposed to quantify the local micromechanical environment. Results indicate that central quartz grains exhibit significant micromechanical property variability (CV > 14%), which is governed by the mineral interface network topology. Specifically, high -C eff rigid interlocking networks enhance the mechanical performance of central quartz grains through a "rigid constraint stiffening effect." Conversely, low- C eff weak wrapping networks trigger a "compliant decoupling weakening effect" inducing interface debonding and attenuating apparent mechanical properties of central quartz grains. Further analysis reveals that the variation in interface network constraints is essentially a micromechanical differentiation resulting from the competitive evolution between chemical pressure solution and mechanical compaction. The diagenetic evolution model of mineral interface network micromechanical differentiation established in this study lays a theoretical foundation for shifting shale brittleness evaluation from a "composition-oriented" to a "topology-oriented" paradigm, offering significant implications for identifying fracturing "sweet spots" in deep shale gas reservoirs. Shale micromechanics Nanoindentation test Interface network topology Micromechanical heterogeneity Diagenetic evolution Full Text Additional Declarations No competing interests reported. Cite Share Download PDF Status: Under Review Version 1 posted Reviews received at journal 27 Apr, 2026 Reviewers agreed at journal 27 Apr, 2026 Reviewers invited by journal 27 Apr, 2026 Editor assigned by journal 05 Feb, 2026 Submission checks completed at journal 05 Feb, 2026 First submitted to journal 03 Feb, 2026 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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