Pore Fluid Pressure Development in Compacting Fault Gouge in Theory, Experiments, and Nature

机译：在理论，实验和自然的压实故障凿孔中的孔隙流体压力开发

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Abstract >The strength of fault zones is strongly dependent on pore fluid pressures within them. Moreover, transient changes in pore fluid pressure can lead to a variety of slip behavior from creep to unstable slip manifested as earthquakes or slow slip events. The frictional properties of low‐permeability fault gouge in nature and experiment can be affected by pore fluid pressure development through compaction within the gouge layer, even when the boundaries are drained. Here the conditions under which significant pore fluid pressures develop are analyzed analytically, numerically, and experimentally. Friction experiments on low‐permeability fault gouge at different sliding velocities show progressive weakening as slip rate is increased, indicating that faster experiments are incapable of draining the pore fluid pressure produced by compaction. Experiments are used to constrain the evolution of the permeability and pore volume needed for numerical modeling of pore fluid pressure build up. The numerical results are in good agreement with the experiments, indicating that the principal physical processes have been considered. The model is used to analyze the effect of pore fluid pressure transients on the determination of the frictional properties, illustrating that intrinsic velocity‐strengthening behavior can appear velocity weakening if pore fluid pressure is not given sufficient time to equilibrate. The results illustrate that care must be taken when measuring experimentally the frictional characteristics of low‐permeability fault gouge. The contribution of compaction‐induced pore fluid pressurization leading to weakening of natural faults is considered. Cyclic pressurization of pore fluid within fault gouge during successive earthquakes on larger faults may reset porosity and hence the capacity for compaction weakening. </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”> <标题类型=“main”>抽象</ title> >断层区域的强度强烈依赖于它们内的孔隙流体压力。此外，孔隙流体压力的瞬态变化可能导致从蠕变到不稳定的滑动的各种滑动行为，表现为地震或缓冲事件。即使在排出边界时，通过压实孔隙流体压力，孔隙流体压力发育的摩擦性能和实验也可以影响孔隙流体压力的摩擦性能。在这里，在数值上分析显着的孔隙流体压力的条件在数值和实验上进行分析。在不同滑动速度下低渗透性故障凿孔的摩擦实验表明，随着滑移速率增加，表明更快的实验不能排出通过压实产生的孔隙流体压力。实验用于限制孔隙流体压力累积数值模拟所需的渗透性和孔体积的演变。数值结果与实验一致，表明已考虑主要物理过程。该模型用于分析孔隙流体压力瞬变对摩擦性能的测定的影响，说明如果孔隙流体压力没有足够的时间来平衡，则本型速度强化行为可以出现速度弱化。结果说明了在测量实验时，必须小心进行低渗透性故障凿孔的摩擦特性。考虑了压实诱导的孔隙流体加压的贡献，导致自然故障削弱。在较大故障上连续地震中发生故障凿孔内的孔隙流体的循环加压可以复位孔隙率，从而重压压实削弱的能力。</ p> </摘要> </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1期</span><b style="margin: 0 2px;">|</b><span>共16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=Faulkner D. R.&option=202" target="_blank" rel="nofollow">Faulkner D. R.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Sanchez‐Roa C.&option=202" target="_blank" rel="nofollow">Sanchez‐Roa C.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Boulton C.&option=202" target="_blank" rel="nofollow">Boulton C.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Hartog S. A. M.&option=202" target="_blank" rel="nofollow">Hartog S. A. M.;</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>Rock Deformation Laboratory Department of Earth Ocean and Ecological SciencesUniversity of LiverpoolLiverpool UK;</p> <p>Departamento de Geología y CEACTierra Unidad Asociada IACT (CSIC‐UGR)Universidad de JaénJaén Spain;</p> <p>Rock Deformation Laboratory Department of Earth Ocean and Ecological SciencesUniversity of LiverpoolLiverpool UK;</p> <p>Rock Deformation Laboratory Department of Earth Ocean and Ecological SciencesUniversity of LiverpoolLiverpool UK;</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=faults&option=203" rel="nofollow">faults;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=permeability&option=203" rel="nofollow">permeability;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=friction&option=203" rel="nofollow">friction;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=fluids&option=203" rel="nofollow">fluids;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=earthquake&option=203" rel="nofollow">earthquake;</a> </p> <div class="translation"> 机译：缺陷;渗透率;摩擦;液体;地震; </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/0704025591454.html">Pore Fluid Pressure Development in Compacting Fault Gouge in Theory, Experiments, and Nature</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Faulkner D. 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