Modeling Forced Imbibition Processes and the Associated Seismic Attenuation in Heterogeneous Porous Rocks

Solazzi Santiago G.; Guarracino Luis; Rubino J. Germán; Müller Tobias M.; Holliger Klaus

摘要

Abstract >Quantifying seismic attenuation during laboratory imbibition experiments can provide useful information toward the use of seismic waves for monitoring injection and extraction of fluids in the Earth's crust. However, a deeper understanding of the physical causes producing the observed attenuation is needed for this purpose. In this work, we analyze seismic attenuation due to mesoscopic wave‐induced fluid flow (WIFF) produced by realistic fluid distributions representative of imbibition experiments. To do so, we first perform two‐phase flow simulations in a heterogeneous rock sample to emulate a forced imbibition experiment. We then select a subsample of the considered rock containing the resulting time‐dependent saturation fields and apply a numerical upscaling procedure to compute the associated seismic attenuation. By exploring both saturation distributions and seismic attenuation, we observe that two manifestations of WIFF arise during imbibition experiments: the first one is produced by the compressibility contrast associated with the saturation front, whereas the second one is due to the presence of patches containing very high amounts of water that are located behind the saturation front. We demonstrate that while the former process is expected to play a significant role in the case of high injection rates, which are associated with viscous‐dominated imbibition processes, the latter becomes predominant during capillary‐dominated processes, that is, for relatively low injection rates. We conclude that this kind of joint numerical analysis constitutes a useful tool for improving our understanding of the physical mechanisms producing seismic attenuation during laboratory imbibition experiments. </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 =“JGRB52357-ABS-ABS-ABS-ABS-0001”> <标题类型=“MAIN”>摘要</标题> <P>在实验室内吸收实验期间量化地震衰减可以为使用提供有用的信息用于监测地壳中液体喷射和提取流体的地震波。然而，为此目的需要更深入地了解产生观察到的衰减的物理原因。在这项工作中，我们通过代表利用实验实验的现实流体分布产生的介性波引起的流体流动（WIFF）来分析地震衰减。为此，我们首先在异质岩样中执行两相流模拟，以模拟强制性的吸收实验。然后，我们选择包含产生的时间依赖饱和度字段的所考虑的岩石的子样本，并应用数值Upscaling过程来计算相关的地震衰减。通过探索饱和度分布和地震衰减，我们观察到在吸收实验期间出现的两种表现出来：第一个由与饱和正面相关的压缩性对比产生，而第二个是由于存在含有非常高的贴片位于饱和正面后面的水量。我们证明预期前一个过程在高注射率的情况下在粘性主导的吸入过程相关的情况下发挥重要作用，而后者在毛细管主导的过程中成为主要的，即，对于相对低的注射率。我们得出结论，这种联合数值分析构成了一种有用的工具，用于改善我们对实验室吸收实验期间产生地震衰减的物理机制的理解。</ 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>2017年第11期</span><b style="margin: 0 2px;">|</b> <span>共19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=Solazzi Santiago G.&option=202" target="_blank" rel="nofollow">Solazzi Santiago G.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Guarracino Luis&option=202" target="_blank" rel="nofollow">Guarracino Luis;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Rubino J. Germán&option=202" target="_blank" rel="nofollow">Rubino J. Germán;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Müller Tobias M.&option=202" target="_blank" rel="nofollow">Müller Tobias M.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Holliger Klaus&option=202" target="_blank" rel="nofollow">Holliger Klaus;</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>CONICET Facultad de Ciencias Astronómicas y GeofísicasUniversidad Nacional de La PlataLa Plata Argentina;</p> <p>CONICET Facultad de Ciencias Astronómicas y GeofísicasUniversidad Nacional de La PlataLa Plata Argentina;</p> <p>CONICETCentro Atómico Bariloche‐CNEASan Carlos de Bariloche Argentina;</p> <p>Commonwealth Scientific and Industrial Research Organization EnergyPerth Western Australia Australia;</p> <p>Applied and Environmental Geophysics Group Institute of Earth SciencesUniversity of LausanneLausanne Switzerland;</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 attenuation&option=203" rel="nofollow">seismic attenuation;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=computational seismology&option=203" rel="nofollow">computational seismology;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=theoretical seismology&option=203" rel="nofollow">theoretical seismology;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=acoustic properties&option=203" rel="nofollow">acoustic properties;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=imbibition&option=203" rel="nofollow">imbibition;</a> </p> <div class="translation"> 机译：地震衰减;计算地震学;理论地震学;声学特性;吸收; </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/0704020651749.html">Modeling Forced Imbibition Processes and the Associated Seismic Attenuation in Heterogeneous Porous Rocks</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Solazzi Santiago G.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Solazzi Santiago G.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Guarracino Luis&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Guarracino Luis,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Rubino J. 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