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High‐Resolution Mapping of Yield Curve Shape and Evolution for Porous Rock: The Effect of Inelastic Compaction on Porous Bassanite

机译：屈服曲线形状的高分辨率映射和多孔岩的演化：无弹性压实对多孔酪乳石的影响

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Abstract > Porous rock deformation has important implications for fluid flow in a range of crustal settings as compaction can increase fluid pressure and alter permeability. The onset of inelastic strain for porous materials is typically defined by a yield curve plotted in differential stress ( <fi>Q</fi> ) versus effective mean stress ( <fi>P</fi> ) space. Empirical studies have shown that these curves are broadly elliptical in shape. Here conventional triaxial experiments are first performed to document (a) the yield curve of porous bassanite (porosity?≈?27–28%), a material formed from the dehydration of gypsum, and (b) the postyield behavior, assuming that <fi>P</fi> and <fi>Q</fi> track along the yield surface as inelastic deformation accumulates. The data reveal that after initial yield, the yield surface cannot be perfectly elliptical and must evolve significantly as inelastic strain is accumulated. To investigate this further, a novel stress‐probing methodology is developed to map precisely the yield curve shape and subsequent evolution for a single sample. These measurements confirm that the high‐pressure side of the curve is partly composed of a near‐vertical limb. Yield curve evolution is shown to be dependent on the nature of the loading path. Bassanite compacted under differential stress develops a heterogeneous microstructure and has a yield curve with a peak that is almost double that of an equal porosity sample that has been compacted hydrostatically. The dramatic effect of different loading histories on the strength of porous bassanite highlights the importance of understanding the associated microstructural controls on the nature of inelastic deformation in porous rock. </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> >多孔岩石变形对于在一系列地壳环境中具有重要意义，因为压实可以增加流体压力和改变渗透性。多孔材料的非弹性应变的发作通常由诸如差分应力（<Fi> Q / Fi>）绘制的产曲线与有效平均应力（<Fi> P </ Fi>）空间。实证研究表明，这些曲线呈广泛椭圆形。这里首先进行常规的三轴实验以进行文件（a）多孔甲癸酯的产曲线（孔隙率≈α27-28％），这是由石膏的脱水形成的材料，并假设<fi > P </ FI>和<FI> Q </ FI>沿屈服表面轨道，因为内部变形累积。数据显示，在初始产率之后，屈服表面不能完全椭圆形，并且必须显着地发展，因为绝体应变累积。为了进一步研究这一点，开发了一种新的应力探测方法，精确地映射产曲线形状和随后的单个样品的演变。这些测量结果证实曲线的高压侧部分地由近垂直肢体组成。产量曲线演变被认为取决于装载路径的性质。在差分应力下压实的南非乳石显影性微观结构，具有峰值的屈服曲线，峰值几乎是静静压的等于孔隙率样品的两倍。不同载荷历史对多孔碳酸盐岩强度的显着作用凸显了了解多孔岩石中无弹性变形性质的相关微观结构控制的重要性。 </ 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2期</span><b style="margin: 0 2px;">|</b><span>共18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=Bedford John D.&option=202" target="_blank" rel="nofollow">Bedford John D.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Faulkner Daniel R.&option=202" target="_blank" rel="nofollow">Faulkner Daniel R.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Leclère Henri&option=202" target="_blank" rel="nofollow">Leclère Henri;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wheeler John&option=202" target="_blank" rel="nofollow">Wheeler John;</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 Earth Ocean and Ecological SciencesUniversity of LiverpoolLiverpool UK;</p> <p>Department of Earth Ocean and Ecological SciencesUniversity of LiverpoolLiverpool UK;</p> <p>Department of Earth Ocean and Ecological SciencesUniversity of LiverpoolLiverpool UK;</p> <p>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=yield curve&option=203" rel="nofollow">yield curve;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=compaction&option=203" rel="nofollow">compaction;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=dilation&option=203" rel="nofollow">dilation;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=localization&option=203" rel="nofollow">localization;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=bassanite&option=203" rel="nofollow">bassanite;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=porous rock&option=203" rel="nofollow">porous rock;</a> </p> <div class="translation"> 机译：产量曲线;压实;扩张;本地化;巴斯岩;多孔岩石; </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/0704025592794.html">High‐Resolution Mapping of Yield Curve Shape and Evolution for Porous Rock: The Effect of Inelastic Compaction on Porous Bassanite</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Bedford John D.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Bedford John D.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Faulkner Daniel R.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Faulkner Daniel R.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Leclère Henri&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Leclère Henri,</a> <a href="/journal-foreign-34677/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of geophysical research. 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<span> <a href="/conference-cn-16988/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 中国力学学会2009学术大会 </a> <span> <span> . 2009</span> </span> </div> </li> <li> <div> <b>7. </b><a class="enjiyixqcontent" href="/academic-degree-domestic_mphd_thesis/020312669616.html">多孔Ti-7.5Nb-4Mo-2.5Sn形状记忆合金的制备及孔结构对其超弹性能的影响</a> <b>[A] </b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=张芸&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 张芸</a> <span> . 2014</span> </span> </div> </li> </ul> <ul style="display: none;"> <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/patent-detail/06130459741649.html">Thermoforming synthetic parts with complex curved surfaces partic. transparent polycarbonate for automobile use - by placing blank between flexible gas tight membrane and former of required shape made from rigid porous body coated with gas permeable surface and drawing vacuum through the porous body causing membrane</a> 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