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A Poroelastic Model of Serpentinization: Exploring the Interplay Between Rheology, Surface Energy, Reaction, and Fluid Flow

机译：蛇形化的多孔弹性模型：探索流变，表面能，反应与流体流动的相互作用

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Abstract > The interactions between reactive fluids and solids are critical in Earth dynamics. Implications of such processes are wide ranging: from earthquake physics to geologic carbon sequestration and the cycling of fluids and volatiles through subduction zones. Peridotite alteration is a common feature in many of these processes, which—despite its obvious importance—is relatively poorly understood from a geodynamical perspective. In particular, although frequently observed in nature, it is still unknown how rocks can undergo 100% hydration/carbonation. One potential explanation of this observation is the mechanism of <fi>reaction‐driven cracking</fi> : that volume changes associated with these reactions are large enough to fracture the surrounding rock, leading to a positive feedback where new reactive surfaces are exposed and fluid pathways are created. The purpose of this study is to investigate the relative roles of reaction, elastic stresses, and surface tension in alteration reactions. In this regard, we derive a system of equations describing reactive fluid flow in elastically deformable porous media, which we apply to a model of serpentinization in a subseafloor environment. The stoichiometry of the serpentinization reaction predicts net volume reduction of the multiphase system, which, according to our numerical simulations, can lead to failure in tension. We also explore a parameterization of surface energy in the model, which allows fluid to infiltrate regions of dry peridotite, significantly changing the stresses and potentially leading to growing crack fronts. </abstract> </span> <span class="z_kbtn z_kbtnclass hoverxs" style="display: none;">展开▼</span> </div> <div class="translation abstracttxt"> <span class="zhankaihshouqi fivelineshidden" id="abstract"> <span>机译：</span><Abstract Type =“main”XML：Lang =“en”XML：ID =“JGRB53093-Abs-Abs-0001”> <标题类型=“main”>抽象</标题> >反应性流体和固体之间的相互作用地球动力学批评。这种过程的含义广泛测距：从地震物理到地质碳封存和通过俯冲区域循环流体和挥发物的循环。橄榄石改变是许多这些过程中的一个共同特征，尽管它显而易见 - 从地磁角度来看，相对较差地理解。特别是，虽然经常在自然界中观察到，但仍然是岩石如何经历100％水合/碳酸化的方式。这种观察结果的一个潜在说明是<FI>反应驱动的裂化的机理</ fi>：与这些反应相关的体积变化足够大以破坏周围岩石，导致新的反应表面暴露的正反馈产生流体途径。本研究的目的是探讨反应，弹性应力和表面张力在改变反应中的相对作用。在这方面，我们得出了一种描述可弹性变形多孔介质中的反应性流体流动的方程式，我们适用于海底环境中的蛇形化模型。蛇形化反应的化学计量预测了多相体系的净体积减少，根据我们的数值模拟，可以导致张力失效。我们还探讨了模型中表面能的参数化，这允许流体渗透干燥的恒星区域，显着改变应力并可能导致生长的裂缝前沿。 </ p> </ abstract> </span> <span class="z_kbtn z_kbtnclass hoverxs" style="display: none;">展开▼</span> </div> </div> <div class="record"> <h2 class="all_title" id="enpatent33" >著录项</h2> <ul> <li> <span class="lefttit">来源</span> <div style="width: 86%;vertical-align: text-top;display: inline-block;"> <a href='/journal-foreign-34677/'>《Journal of geophysical research. Solid earth: JGR》</a> <b style="margin: 0 2px;">|</b><span>2018年第10期</span><b style="margin: 0 2px;">|</b><span>共23页</span> </div> </li> <li> <div class="author"> <span class="lefttit">作者</span> <p id="fAuthorthree" class="threelineshidden zhankaihshouqi"> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Evans Owen&option=202" target="_blank" rel="nofollow">Evans Owen;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Spiegelman Marc&option=202" target="_blank" rel="nofollow">Spiegelman Marc;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Kelemen Peter B.&option=202" target="_blank" rel="nofollow">Kelemen Peter B.;</a> </p> <span class="z_kbtnclass z_kbtnclassall hoverxs" id="zkzz" style="display: none;">展开▼</span> </div> </li> <li> <div style="display: flex;"> <span class="lefttit">作者单位</span> <div style="position: relative;margin-left: 3px;max-width: 639px;"> <div class="threelineshidden zhankaihshouqi" id="fOrgthree"> <p>Department of Applied Physics and Applied MathematicsColumbia UniversityNew York NY USA;</p> <p>Department of Applied Physics and Applied MathematicsColumbia UniversityNew York NY USA;</p> <p>Lamont‐Doherty Earth ObservatoryColumbia UniversityPalisades NY USA;</p> </div> <span class="z_kbtnclass z_kbtnclassall hoverxs" id="zhdw" style="display: none;">展开▼</span> </div> </div> </li> <li > <span class="lefttit">收录信息</span> <span style="width: 86%;vertical-align: text-top;display: inline-block;"></span> </li> <li> <span class="lefttit">原文格式</span> <span>PDF</span> </li> <li> <span class="lefttit">正文语种</span> <span>eng</span> </li> <li> <span class="lefttit">中图分类</span> <span><a href="https://www.zhangqiaokeyan.com/clc/163.html" title="地球物理学">地球物理学;</a></span> </li> <li class="antistop"> <span class="lefttit">关键词</span> <p style="width: 86%;vertical-align: text-top;"> </p> </li> </ul> </div> </div> <div class="literature cardcommon"> <div class="similarity "> <h3 class="all_title" id="enpatent66">相似文献</h3> <div class="similaritytab clearfix"> <ul> <li class="active" >外文文献</li> <li >中文文献</li> <li >专利</li> </ul> </div> <div class="similarity_details"> <ul > <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704025592843.html">A Poroelastic Model of Serpentinization: Exploring the Interplay Between Rheology, Surface Energy, Reaction, and Fluid Flow</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Evans Owen&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Evans Owen,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Spiegelman Marc&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Spiegelman Marc,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Kelemen Peter B.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Kelemen Peter B. </a> <a href="/journal-foreign-34677/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of geophysical research. 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