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首页> 外文期刊>Journal of geophysical research. Solid earth: JGR >Permeability Variations Associated With Fault Reactivation in a Claystone Formation Investigated by Field Experiments and Numerical Simulations
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Permeability Variations Associated With Fault Reactivation in a Claystone Formation Investigated by Field Experiments and Numerical Simulations

机译：通过现场实验和数值模拟研究了与粘土砂石形成中的故障再活化相关的渗透性变化

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Abstract >We studied the relation between rupture and changes in permeability within a fault zone intersecting the Opalinus Clay formation at 300?m depth in the Mont Terri Underground Research Laboratory (Switzerland). A series of water injection experiments were performed in a borehole straddle interval set within the damage zone of the main fault. A three‐component displacement sensor allowed an estimation of the displacement of a minor fault plane reactivated during a succession of step rate pressure tests. The experiment reveals that the fault hydromechanical (HM) behavior is different from one test to the other with varying pressure levels needed to trigger rupture and different slip behavior under similar pressure conditions. Numerical simulations were performed to better understand the reason for such different behavior and to investigate the relation between rupture nucleation, permeability change, pressure diffusion, and rupture propagation. Our main findings are as follows: (i) a rate frictional law and a rate‐and‐state permeability law can reproduce the first test, but it appears that the rate constitutive parameters must be pressure dependent to reproduce the complex HM behavior observed during the successive injection tests; (ii) almost similar ruptures can create or destroy the fluid diffusion pathways; (iii) a too high or too low diffusivity created by the main rupture prevents secondary rupture events from occurring whereas “intermediate” diffusivity favors the nucleation of a secondary rupture associated with the fluid diffusion. However, because rupture may in certain cases destroy permeability, this succession of ruptures may not necessarily create a continuous hydraulic pathway. </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> >我们研究了与蛋白石粘土形成相交的断层区域内破裂和渗透变化之间的关系在Mont Terri地下研究实验室（瑞士）深度300？M深度。在主故障的损伤区内设定的钻孔跨跨度间隔进行一系列注水实验。三组分位移传感器允许估计在连续的阶梯率压力测试期间重新激活的次要断层平面的位移。该实验表明，故障流体机械（HM）行为与另一个测试不同，该测试具有不同的压力水平来触发相似的压力条件下的破裂和不同滑动行为。进行数值模拟以更好地理解这种不同行为的原因，并研究破裂成核，渗透性变化，压力扩散和破裂繁殖之间的关系。我们的主要发现如下：（i）速率摩擦法和速率和状态渗透性法可以繁殖第一次测试，但似乎速率本构参数必须压力取决于再现观察到的复杂的HM行为连续注射测试; （ii）几乎类似的破裂可以产生或破坏流体扩散途径; （iii）由主要破裂产生的太高或太低的扩散率阻止了二次破裂事件发生，而“中间”扩散率有利于与流体扩散相关的二次破裂的成核。然而，由于在某些情况下破裂可能会破坏渗透性，因此这种破裂的连续可能不一定产生连续的液压通路。</ 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2期</span><b style="margin: 0 2px;">|</b><span>共17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=Jeanne Pierre&option=202" target="_blank" rel="nofollow">Jeanne Pierre;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Guglielmi Yves&option=202" target="_blank" rel="nofollow">Guglielmi Yves;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Rutqvist Jonny&option=202" target="_blank" rel="nofollow">Rutqvist Jonny;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Nussbaum Christophe&option=202" target="_blank" rel="nofollow">Nussbaum Christophe;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Birkholzer Jens&option=202" target="_blank" rel="nofollow">Birkholzer Jens;</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>Lawrence Berkeley National LaboratoryEnergy Geoscience DivisionBerkeley CA USA;</p> <p>Lawrence Berkeley National LaboratoryEnergy Geoscience DivisionBerkeley CA USA;</p> <p>Lawrence Berkeley National LaboratoryEnergy Geoscience DivisionBerkeley CA USA;</p> <p>Federal Office of Topography SwisstopoWabern Switzerland;</p> <p>Lawrence Berkeley National LaboratoryEnergy Geoscience DivisionBerkeley CA 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=fault reactivation&option=203" rel="nofollow">fault reactivation;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=changes in permeability&option=203" rel="nofollow">changes in permeability;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=rate and state&option=203" rel="nofollow">rate and state;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=role of fluid&option=203" rel="nofollow">role of fluid;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=in situ experiment&option=203" rel="nofollow">in situ experiment;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=numerical simulation&option=203" rel="nofollow">numerical simulation;</a> </p> <div class="translation"> 机译：故障重新激活;渗透性的变化;率和州;流体的作用;原位实验;数值模拟; </div> </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/0704025592041.html">Permeability Variations Associated With Fault Reactivation in a Claystone Formation Investigated by Field Experiments and Numerical Simulations</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Jeanne Pierre&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Jeanne Pierre,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Guglielmi Yves&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Guglielmi Yves,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Rutqvist Jonny&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Rutqvist Jonny,</a> <a href="/journal-foreign-34677/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of geophysical research. 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