Seismicity Enhances Macrodispersion in Finite Porous and Fractured Domains: A Pore‐Scale Perspective

机译：地震性增强了有限多孔和裂缝结构域中的宏观分解：孔径展示

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Abstract > Understanding the effects of oscillating flow field induced by seismicity on the transport process is vital for predicting the fate and transport of solute in many dynamic environments. However, there is prominent discrepancy in arguing with the response of dispersion to the oscillating flow field (i.e., the longitudinal dispersion coefficient would decrease, increase, or maintain unchanged). To unravel the underpinning physics about this controversial response, we simulated two‐hundred twenty pore‐scale numerical experiments for the seismicity‐induced oscillating flow field and associated solute transport in the idealized finite porous (i.e., fluidic plate) and fractured (i.e., parallel plates) domains. The numerically obtained breakthrough curves were fitted to the macroscopic advection‐dispersion equation to retrieve the mean velocity and apparent macrodispersion coefficient ( D <sub> L </sub> ). We found that D <sub> L </sub> increases to its maxima when the oscillating flow field resonates with the finite systems, that is, the period ( T ) of the oscillating flow field or the seismic wave approaches the pore volume ( τ ) of a finite domain. The resonant effects diminish and D <sub> L </sub> barely changes when T is much larger or smaller than τ . Moreover, the degree of enhancement in D <sub> L </sub> increases exponentially with the amplitude of the seismic force. Fundamental understanding of the response of macrodispersion to the oscillating flow field adds value in p </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”> <标题类型=“main”>抽象</ title> >了解振荡流场在运输过程中引起的振荡流场对预测至关重要许多动态环境中溶质的命运和运输。然而，随着振荡流场的响应来争论（即，纵向分散系数将减小，增加或保持不变），突出差异。为了解开内宁物理关于这种有争议的反应，我们模拟了两百二十孔隙率的数值实验，用于地震性诱导的振荡流场和理想化的有限多孔（即流体板）中的相关溶质输送和裂缝（即平行板块）域。数值获得的突破性曲线拟合到宏观的平坦分散方程中，以检测平均速度和表观宏观分子系数（ D </ i> <亚> l </ i> </ sub>）。我们发现 d </ i> <sub> l </ i> </ sub>当振荡流场与有限系统一起共振</ i>时，它增加到其最大值，振荡流场或地震波的时段（ t </ i>）接近有限域的孔体积（τ</ i>）。共振</ i>效果递减，并且 d </ i> <sub> l </ sl </ sum>当 t </ i>更大或小于τ</ i>。此外， D </ i> <sub> l </ se> </ sub的增强程度随着地震力的幅度指数增加。对宏分解对振荡流场响应的根本理解增加了p的价值 </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>2019年第3期</span><b style="margin: 0 2px;">|</b><span>共14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=Zheng Lizhi&option=202" target="_blank" rel="nofollow">Zheng Lizhi;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wang Lichun&option=202" target="_blank" rel="nofollow">Wang Lichun;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Deng Wen&option=202" target="_blank" rel="nofollow">Deng Wen;</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 Geological SciencesThe University of Texas at AustinAustin TX USA;</p> <p>Institute of Surface‐Earth System ScienceTianjin UniversityTianjin China;</p> <p>Department of Civil Architectural and Environmental EngineeringMissouri University of Science and TechnologyRolla MO 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;"> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=seismicity&option=203" rel="nofollow">seismicity;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=oscillating flow field&option=203" rel="nofollow">oscillating flow field;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=macrodispersion&option=203" rel="nofollow">macrodispersion;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=pore scale&option=203" rel="nofollow">pore scale;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=porous and fractured media&option=203" rel="nofollow">porous and fractured media;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=finite domain&option=203" rel="nofollow">finite domain;</a> </p> <div class="translation"> 机译：地震性;振荡流场;宏观分裂;孔隙率;多孔和裂缝介质;有限域; </div> </li> <li> <span class="lefttit">入库时间</span> <span>2022-08-20 09:24:19</span> </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/0704025591461.html">Seismicity Enhances Macrodispersion in Finite Porous and Fractured Domains: A Pore‐Scale Perspective</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zheng Lizhi&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Zheng Lizhi,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wang Lichun&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Wang Lichun,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Deng Wen&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Deng Wen </a> <a href="/journal-foreign-34677/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of geophysical research. 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