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Gas Hydrates in Permafrost: Distinctive Effect of Gas Hydrates and Ice on the Geomechanical Properties of Simulated Hydrate‐Bearing Permafrost Sediments

机译：多年冻土中的天然气水合物：天然气水合物和冰对模拟水合物多年冻土沉积物的地质力学性能的独特作用

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Abstract >The geomechanical stability of the permafrost formations containing gas hydrates in the Arctic is extremely vulnerable to global warming and the drilling of wells for oil and gas exploration purposes. In this work the effect of gas hydrate and ice on the geomechanical properties of sediments was compared by triaxial compression tests for typical sediment conditions: unfrozen hydrate‐free sediments at 0.3?°C, hydrate‐free sediments frozen at ?10?°C, unfrozen sediments containing about 22?vol% methane hydrate at 0.3?°C, and hydrate‐bearing sediments frozen at ?10?°C. The effect of hydrate saturation on the geomechanical properties of simulated permafrost sediments was also investigated at predefined temperatures and confining pressures. Results show that ice and gas hydrates distinctively influence the shearing characteristics and deformation behavior. The presence of around 22?vol% methane hydrate in the unfrozen sediments led to a shear strength as strong as those of the frozen hydrate‐free specimens with 85?vol% of ice in the pores. The frozen hydrate‐free sediments experienced brittle‐like failure, while the hydrate‐bearing sediments showed large dilatation without rapid failure. Hydrate formation in the sediments resulted in a measurable reduction in the internal friction, while freezing did not. In contrast to ice, gas hydrate plays a dominant role in reinforcement of the simulated permafrost sediments. Finally, a new physical model was developed, based on formation of hydrate networks or frame structures to interpret the observed strengthening in the shear strength and the ductile deformation. </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”>摘要</标题> >北极水水合物的永久冻土形成的地质力学稳定性极易受到全球变暖的影响以及井井油和天然气勘探目的。在这项工作中，通过三轴压缩试验进行典型沉积物条件的三轴压缩试验对气体水合物和冰对沉积物的地质力学性能的影响：0.3Ω·℃，无水柄沉积物在α℃下冷冻沉积物，在0.3℃下含有约22℃的甲烷水合物，含有约22℃的下来沉积物，并在α℃下冷冻沉积物。在预定温度和限制压力下，还研究了水合物饱和对模拟多年冻土沉积物的地质力学性能的影响。结果表明，冰和天然气巩固了剪切特性和变形行为。在未冷却的沉积物中存在约22？Vol％的甲烷水合物导致剪切强度，与冷冻水合物的样品一样强，毛孔中的85克拉％的冰。冷冻水合物的沉积物经历了脆性的失效，而含水剂沉积物表现出大的扩张而无需快速失效。沉积物中的水合物形成导致内部摩擦的可测量降低，而冻结则没有。与冰相比，天然气水合物在增强模拟的永久冻土沉积物中起着显着作用。最后，基于水合物网络或框架结构的形成，开发了一种新的物理模型，以解释剪切强度和延展性变形中观察到的增强。</ 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>2019年第3期</span><b style="margin: 0 2px;">|</b><span>共13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=Yang J.&option=202" target="_blank" rel="nofollow">Yang J.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Hassanpouryouzband A.&option=202" target="_blank" rel="nofollow">Hassanpouryouzband A.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Tohidi B.&option=202" target="_blank" rel="nofollow">Tohidi B.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Chuvilin E.&option=202" target="_blank" rel="nofollow">Chuvilin E.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Bukhanov B.&option=202" target="_blank" rel="nofollow">Bukhanov B.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Istomin V.&option=202" target="_blank" rel="nofollow">Istomin V.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Cheremisin A.&option=202" target="_blank" rel="nofollow">Cheremisin A.;</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>Institute of Petroleum Engineering School of Energy Geoscience Infrastructure and SocietyHeriot‐Watt UniversityEdinburgh UK;</p> <p>Institute of Petroleum Engineering School of Energy Geoscience Infrastructure and SocietyHeriot‐Watt UniversityEdinburgh UK;</p> <p>Institute of Petroleum Engineering School of Energy Geoscience Infrastructure and SocietyHeriot‐Watt UniversityEdinburgh UK;</p> <p>Center for Hydrocarbon RecoverySkolkovo Institute of Science and TechnologyMoscow Russia;</p> <p>Center for Hydrocarbon RecoverySkolkovo Institute of Science and TechnologyMoscow Russia;</p> <p>Center for Hydrocarbon RecoverySkolkovo Institute of Science and TechnologyMoscow Russia;</p> <p>Center for Hydrocarbon RecoverySkolkovo Institute of Science and TechnologyMoscow Russia;</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=gas hydrate&option=203" rel="nofollow">gas hydrate;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=ice&option=203" rel="nofollow">ice;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=triaxial shearing&option=203" rel="nofollow">triaxial shearing;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=sediments&option=203" rel="nofollow">sediments;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=geomechanical properties&option=203" rel="nofollow">geomechanical properties;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=microhydrate networks&option=203" rel="nofollow">microhydrate networks;</a> </p> <div class="translation"> 机译：天然气水合物;冰;三轴剪切;沉积物;地质力学性质;微水合物网络; </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/0704025592836.html">Gas Hydrates in Permafrost: Distinctive Effect of Gas Hydrates and Ice on the Geomechanical Properties of Simulated Hydrate‐Bearing Permafrost Sediments</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yang J.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Yang J.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Hassanpouryouzband A.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Hassanpouryouzband A.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Tohidi B.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Tohidi B.,</a> <a href="/journal-foreign-34677/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of geophysical research. 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