Effective Pressure Law for the Intrinsic Formation Factor in Low Permeability Sandstones

机译：低渗透性砂岩内部形成系数的有效压力法

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Abstract > The effective pressure law for the intrinsic formation factor of low permeability sandstones from the Ordos Basin (northwest of China) was studied experimentally by measuring the electrical resistivity of brine saturated rock samples while cycling the pore and confining pressures, <fi>p</fi> <sub> <fi>p</fi> </sub> and <fi>p</fi> <sub> <fi>c</fi> </sub> . We used a 100,000?ppm NaCl solution so that the results could be directly interpreted in terms of the intrinsic formation factor <fi>F</fi> . The Response Surface method was used to construct a quadratic function of <fi>p</fi> <sub> <fi>p</fi> </sub> and <fi>p</fi> <sub> <fi>c</fi> </sub> fitting the experimental data, from which the coefficient <fi>α</fi> of the effective pressure law, <fi>p</fi> <sub> <fi>eff</fi> </sub> ?=? <fi>p</fi> <sub> <fi>c</fi> </sub> – α <fi>p</fi> <sub> <fi>p</fi> </sub> , was determined. We found that the coefficient <fi>α</fi> generally had low values, mainly from 0.2 to 0.4, thus contradicting the theoretical prediction that α should be equal to 1 for scale‐invariant properties, such as <fi>F</fi> , in linear elastic materials having a homogeneous solid matrix. Since the two underlying assumptions, linear elasticity and homogeneity of the solid matrix, are likely violated in reservoir rocks, we tried to assess their effects on α using simple analytical models, based on idealized geometries of the pore and solid phases. Analysis of these models suggests that non‐linear elasticity asso </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> >来自鄂尔多斯盆地的低渗透砂岩的内在形成系数的有效压力法（西北在中国）通过测量盐水饱和岩石样品的电阻率，同时循环孔隙和限制压力，<Fi> P </ Fi> <Fi> P </ Fi> </ sub>和<Fi > P </ FI> <sub> <fi> c </ fi> </ sub>。我们使用了100,000个ppm NaCl解决方案，以便在内在形成因子</ Fi>中直接解释结果。响应表面方法用于构建<fi> p </ fi> <sub> <fi> p </ fi> <sub>和<fi> p </ fi> <sub> <fi>的二次函数C </ fi>拟合实验数据，从中的有效压力法的系数<fi>α</ fi> <fi> p </ fi> <sub> <fi> eff </ fi > </ sub>？=？ <fi> p </ fi> <sub> <fi> c </ fi> </ sub> - α<fi> p </ fi> <sub> <fi> p </ fi> </ sub>决定。我们发现系数<fi>α</ fi>通常具有低值，主要是0.2至0.4，因此与α应等于1的理论预测，用于鳞片不变性，例如<fi> f </ Fi>，在具有均相固体基质的线性弹性材料中。由于两种潜在的假设，固体矩阵的线性弹性和均匀性，因此可能在储层岩石中侵犯，我们试图使用简单的分析模型来评估它们对α的影响，基于孔和固相的理想几何形状。对这些模型的分析表明非线性弹性分析 </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15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=Chen M.&option=202" target="_blank" rel="nofollow">Chen M.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Li M.&option=202" target="_blank" rel="nofollow">Li M.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Bernabé Y.&option=202" target="_blank" rel="nofollow">Bernabé Y.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zhao J. Z.&option=202" target="_blank" rel="nofollow">Zhao J. Z.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zhang L. H.&option=202" target="_blank" rel="nofollow">Zhang L. H.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zhang Z. Y.&option=202" target="_blank" rel="nofollow">Zhang Z. Y.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Tang Y. B.&option=202" target="_blank" rel="nofollow">Tang Y. B.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Xiao W. L.&option=202" target="_blank" rel="nofollow">Xiao W. L.;</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>State Key Laboratory of Oil and Gas Reservoir Geology and ExploitationSouthwest Petroleum UniversityChengdu China;</p> <p>State Key Laboratory of Oil and Gas Reservoir Geology and ExploitationSouthwest Petroleum UniversityChengdu China;</p> <p>Earth Atmospheric and Planetary Sciences DepartmentMassachusetts Institute of TechnologyCambridge MA USA;</p> <p>State Key Laboratory of Oil and Gas Reservoir Geology and ExploitationSouthwest Petroleum UniversityChengdu China;</p> <p>State Key Laboratory of Oil and Gas Reservoir Geology and ExploitationSouthwest Petroleum UniversityChengdu China;</p> <p>School of Geoscience and TechnologySouthwest Petroleum UniversityChengdu China;</p> <p>State Key Laboratory of Oil and Gas Reservoir Geology and ExploitationSouthwest Petroleum UniversityChengdu China;</p> <p>State Key Laboratory of Oil and Gas Reservoir Geology and ExploitationSouthwest Petroleum UniversityChengdu China;</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=Low permeability sandstones&option=203" rel="nofollow">Low permeability sandstones;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Formation factor&option=203" rel="nofollow">Formation factor;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Nonlinear effective pressure&option=203" rel="nofollow">Nonlinear effective pressure;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Microstructure&option=203" rel="nofollow">Microstructure;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Simple analytical models&option=203" rel="nofollow">Simple analytical models;</a> </p> <div class="translation"> 机译：低渗透砂岩;形成系数;非线性有效压力;微观结构;简单的分析模型; </div> </li> <li> <span class="lefttit">入库时间</span> <span>2022-08-20 09:24:19</span> </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/0704020651546.html">Effective Pressure Law for the Intrinsic Formation Factor in Low Permeability Sandstones</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Chen M.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Chen M.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Li M.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Li M.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Bernabe Y.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Bernabe Y.,</a> <a href="/journal-foreign-34656/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of Geophysical Research. 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Xiao,</a> <span>2009</span> </span> </div> <p class="zwjiyix translation" style="max-width: initial;height: auto;word-break: break-all;white-space: initial;text-overflow: initial;overflow: initial;"> <span>机译：E-BEI砂岩渗透性的有效压力法</span> </p> </li> <li> <div> <b>8. </b><a class="enjiyixqcontent" href="/ntis-science-report_de_thesis/02071882269.html">Nonassociated gas resources in low-permeability sandstone reservoirs, lower tertiary Wasatch Formation, and upper Cretaceous Mesaverde Group, Uinta Basin, Utah</a> <b>[R] </b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Fouch, T. D. &option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Fouch, T. D. ,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Schmoker, J. W. &option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Schmoker, J. W. ,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Boone, L. 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