A Broadband Laboratory Study of the Seismic Properties of Cracked and Fluid‐Saturated Synthetic Glass Media

机译：裂缝和流体饱和合成玻璃介质抗震性能的宽带实验室研究

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Abstract > For better understanding of frequency dependence (dispersion) of seismic wave velocities caused by stress‐induced fluid flow, broadband laboratory measurements were performed on a suite of synthetic glass media containing both equant pores and thermal cracks. Complementary forced oscillation, resonant bar, and ultrasonic techniques provided access to millihertz‐hertz frequencies, ~1?kHz frequency, and ~1?MHz frequency, respectively. The wave speeds or effective elastic moduli and associated dissipation were measured on samples under dry, argon‐ or nitrogen‐saturated, and water‐saturated conditions in sequence. The elastic moduli, in situ permeability, and crack porosity inferred from in situ X‐ray computed tomography all attest to strong pressure‐induced crack closure for differential (confining‐minus‐pore) pressures <30?MPa, consistent with zero‐pressure crack aspect ratios <4?×?10 ?4 . The low permeabilities of these materials allow access to undrained conditions, even at subhertz frequencies. The ultrasonically measured elastic moduli reveal consistently higher shear and bulk moduli upon fluid saturation—diagnostic of the saturated‐isolated regime. For a glass rod specimen, containing cracks but no pores, saturated‐isolated conditions apparently persist to subhertz frequencies—requiring in situ aspect ratios (minimum/maximum dimension) <10 ?5 . In marked contrast, the shear modulus measured at subhertz frequencies on a cracked glass bead specimen of 5% porosity, is insensitive to fluid saturation, consistent with the Biot‐Gassmann model for the saturated‐isobaric regime. The measured dispersion of the shear modulus approaches 10% over the millihertz‐megahertz frequency range for the cracked and fluid‐saturated media—implying that laboratory ultrasonic data should be used with care in the </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> >，用于更好地理解由应力诱导的流体引起的地震波速度的频率依赖性（分散）流动，宽带实验室测量是在含有刻表孔和热裂缝的合成玻璃介质套件上进行的。互补强制振荡，谐振棒和超声波技术可分别提供对MilliHertz-Hertz频率，〜1？kHz频率和〜1？MHz频率的访问。在干燥，氩气或氮气饱和和水饱和条件下的样品上测量波速或有效的弹性模量和相关耗散。从原位X射线计算断层扫描推断出的弹性模量，都证明了对差分（限制 - 减去孔）压力<30≤MPa的强大压力诱导的裂纹闭合，与零压裂裂缝一致纵横比<4？×10 ？4 </ sup>。这些材料的低渗透性允许在Subhertz频率下允许访问不驱动的条件。超声测量的弹性模量在流体饱和诊断时呈始终如一的剪切和散装模量达到饱和状态。对于玻璃棒样本，含有裂缝但没有孔，饱和的条件明显持续存在于原位纵横比（最小/最大尺寸）<10 5 </ sup>的次静电频率。在标记对比中，在裂化玻璃珠样品上测量的5％孔隙率的脉冲玻璃珠样品的剪切模量对流体饱和度不敏感，与饱和同级制度的Biot-Gassmann模型一致。剪切模量的测量分散方法在裂缝和流体饱和介质的千赫氏 - Megahertz频率范围内接近10％ - 暗示实验室超声数据应在护理中使用 </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5期</span><b style="margin: 0 2px;">|</b><span>共38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=Li Yang&option=202" target="_blank" rel="nofollow">Li Yang;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=David Emmanuel C.&option=202" target="_blank" rel="nofollow">David Emmanuel C.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Nakagawa Seiji&option=202" target="_blank" rel="nofollow">Nakagawa Seiji;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Kneafsey Timothy J.&option=202" target="_blank" rel="nofollow">Kneafsey Timothy J.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Schmitt Douglas R.&option=202" target="_blank" rel="nofollow">Schmitt Douglas R.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Jackson Ian&option=202" target="_blank" rel="nofollow">Jackson Ian;</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>Research School of Earth SciencesAustralian National UniversityCanberra ACT Australia;</p> <p>Research School of Earth SciencesAustralian National UniversityCanberra ACT Australia;</p> <p>Energy Geosciences Division EESALawrence Berkeley National LaboratoryBerkeley CA USA;</p> <p>Energy Geosciences Division EESALawrence Berkeley National LaboratoryBerkeley CA USA;</p> <p>Department of PhysicsUniversity of AlbertaEdmonton Alberta Canada;</p> <p>Research School of Earth SciencesAustralian National UniversityCanberra ACT Australia;</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=seismic properties&option=203" rel="nofollow">seismic properties;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=broadband measurement&option=203" rel="nofollow">broadband measurement;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=synthetic glass media&option=203" rel="nofollow">synthetic glass media;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=dispersion and attenuation&option=203" rel="nofollow">dispersion and attenuation;</a> </p> <div class="translation"> 机译：地震特性;宽带测量;合成玻璃介质;分散和衰减; </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/0704025591008.html">A Broadband Laboratory Study of the Seismic Properties of Cracked and Fluid‐Saturated Synthetic Glass Media</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Li Yang&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Li Yang,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=David Emmanuel C.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">David Emmanuel C.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Nakagawa Seiji&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Nakagawa Seiji,</a> <a href="/journal-foreign-34677/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of geophysical research. 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