Does fault strengthening in laboratory rock friction experiments really depend primarily upon time and not slip?

Bhattacharya Pathikrit; Rubin Allan M.; Beeler Nicholas M.

摘要

Abstract > The popular constitutive formulations of rate‐and‐state friction offer two end‐member views on whether friction evolves only with slip (Slip law) or with time even without slip (Aging law). While rate stepping experiments show support for the Slip law, laboratory‐observed frictional behavior near zero slip rates has traditionally been inferred as supporting Aging law style time‐dependent healing, in particular, from the slide‐hold‐slide experiments of Beeler et al. (1994). Using a combination of new analytical results and explicit numerical (Bayesian) inversion, we show instead that the slide‐hold‐slide data of Beeler et al. (1994) favor slip‐dependent state evolution during holds. We show that, while the stiffness‐independent rate of growth of peak stress (following reslides) with hold duration is a property shared by both the Aging and (under a more restricted set of parameter combinations) Slip laws, the observed stiffness dependence of the rate of stress relaxation during long holds is incompatible with the Aging law with constant rate‐state parameters. The Slip law consistently fits the evolution of the stress minima at the end of the holds well, whether fitting jointly with peak stresses or otherwise. But neither the Aging nor Slip laws fit all the data well when a ? b is constrained to values derived from prior velocity steps. We also attempted to fit the evolution of stress peaks and minima with the Kato‐Tullis hybrid law and the shear stress‐dependent Nagata law, both of which, even with the freedom of an extra parameter, generally reproduced the best Slip law fits to the data. </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：ID =“JGRB52205-ABS-ABS-0001”> <标题类型=“MAIN”> Abstract </ Title> >率 - 状态摩擦的流行组成配方提供两个结束 - 成员观点，即摩擦是否仅在滑动（滑动法）或即使没有滑动（老化法）时也仅演变。虽然汇率踩踏实验表明对防滑律的支持，但是，传统上推断出零滑滑速率附近的实验室摩擦行为，特别是支持贝尔等人的滑动载玻片实验的老化法则依赖性愈合。（1994）。使用新的分析结果和显式数值（贝叶斯）反转的组合，我们显示了Beeler等人的滑动载滑数据。（1994）持有期间的依赖依赖状态演变。我们展示了，虽然具有保持持续时间的峰值应力的刚度和峰值的刚度的生长速率是由老化和（在更受限制的参数组合）的情况下共享的属性，但是观察到的刚度依赖性在长期保持过程中应力松弛率与具有恒定率 - 状态参数的老化法不相容。滑移法始终符合保持良好的压力最小值的演变，无论是否与峰值应力联合或其他方式。但是，当 a </ i>时，老化和滑动法都不适合所有数据？ B </ i>被限制为源自先前速度步骤的值。我们还试图利用Kato-Tullis混合法和剪切应力依赖性Nagata法，均应符合压力峰值和最小值的演变，这两种剪切应力依赖性的纳播法则，即使是额外参数的自由，通常再现最佳的滑动法适合数据。 </ 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>2017年第8期</span><b style="margin: 0 2px;">|</b><span>共42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=Bhattacharya Pathikrit&option=202" target="_blank" rel="nofollow">Bhattacharya Pathikrit;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Rubin Allan M.&option=202" target="_blank" rel="nofollow">Rubin Allan M.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Beeler Nicholas M.&option=202" target="_blank" rel="nofollow">Beeler Nicholas 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>Department of GeosciencesPrinceton UniversityPrinceton New Jersey USA;</p> <p>Department of GeosciencesPrinceton UniversityPrinceton New Jersey USA;</p> <p>Brown UniversityProvidence Rhode Island 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=frictional healing&option=203" rel="nofollow">frictional healing;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=rate‐state friction&option=203" rel="nofollow">rate‐state friction;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=earthquake cycle&option=203" rel="nofollow">earthquake cycle;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=state evolution laws&option=203" rel="nofollow">state evolution laws;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=laboratory friction&option=203" rel="nofollow">laboratory friction;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Bayesian inversion&option=203" rel="nofollow">Bayesian inversion;</a> </p> <div class="translation"> 机译：摩擦愈合;率 - 状态摩擦;地震循环;国家进化法则;实验室摩擦;贝叶斯反演; </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/0704020652012.html">Does fault strengthening in laboratory rock friction experiments really depend primarily upon time and not slip?</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Bhattacharya Pathikrit&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Bhattacharya Pathikrit,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Rubin Allan M.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Rubin Allan M.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Beeler Nicholas M.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Beeler Nicholas M. </a> <a href="/journal-foreign-34656/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of Geophysical Research. 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