Low‐Field Nuclear Magnetic Resonance Characterization of Carbonate and Sandstone Reservoirs From Rock Spring Uplift of Wyoming

Wang Heng; Alvarado Vladimir; McLaughlin J. Fred; Bagdonas Davin A.; Kaszuba John P.; Campbell Erin; Grana Dario

摘要

Abstract > Laboratory measurements including gas (N <sub>2</sub> ) porosity and permeability, time‐domain nuclear magnetic resonance, thin section, and scanning electron microscopy analysis were conducted to obtain petrographical and petrophysical descriptions of the Weber Sandstone and Madison Limestone at the Rock Spring Uplift, a potential carbon dioxide storage site in Southwestern Wyoming. The relationships between pore structures, such as pore geometry, pore‐size distribution, pore network, and porosity/permeability are investigated. First, using thin sections combined with scanning electron microscopy for pore structures description, all samples are described in detail from the geological, petrographysical, and diagenetic viewpoint. Results show that within the Madison Limestone, pore types include intercrystalline, vuggy, moldic, or mixed (combination of all other pore types). Both moldic and vuggy pore types are associated with samples of high porosity and permeability. Nuclear magnetic resonance relaxation time distributions show either bimodal or multimodal distributions. Large relaxation time components are associated with samples with large pores, whereas small components are dominated by small pores. The T <sub>2</sub> geometric mean correlates well with gas permeability. Additionally, short‐time diffusion coefficients (D) were measured by pulsed field gradient method using a series of gradient strengths. We found that diffusion coefficient distributions correlate with the corresponding T <sub>2</sub> distributions for macropores. By comparing the dominant peak position of T <sub>2</sub> distributions and their corresponding diffusion coefficient distributions, we predicted the surface relaxivity of different rock types. We found that surface relaxivities of Webe </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”XML：ID =“JGRB52981-ABS-ABS-ABS-ABS-0001”> <标题类型=“MAIN”>抽象</标题> <P>实验室测量，包括气体（n <sub > 2 </ sub>）孔隙率和渗透性，时域核磁共振，薄截面和扫描电子显微镜分析，以获得岩春隆起的冬季砂岩和麦迪逊石灰石的岩体和岩石物理描述，潜在的碳西南部怀俄明州的二氧化二氧化碳储存场所。研究了孔隙结构之间的关系，例如孔隙几何形状，孔径分布，孔网络和孔隙率/渗透率。首先，使用与扫描电子显微镜结合的薄切片进行孔结构描述，从地质，岩化学和成岩性观点详细描述了所有样品。结果表明，在麦迪逊石灰石内，孔隙类型包括肾脏，vuggy，模塑或混合（所有其他孔类型的组合）。模塑和Vuggy孔隙类型都与高孔隙率和渗透性的样品相关。核磁共振弛豫时间分布显示双峰或多模级分布。大量放松时间分量与具有大孔的样品相关，而小部件由小孔支配。 T <sub> 2 </ sub>几何平均与透气性很好地相关。另外，使用一系列梯度强度通过脉冲场梯度法测量短时漫射系数（D）。我们发现扩散系数分布与Macropores的相应T <Sub> 2 </ sub>分布相关。通过比较T <sub> 2 </ sub>分布及其相应的扩散系数分布的显性峰位置，我们预测了不同岩石类型的表面松弛率。我们发现Webe的表面松弛性 </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9期</span><b style="margin: 0 2px;">|</b><span>共17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=Wang Heng&option=202" target="_blank" rel="nofollow">Wang Heng;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Alvarado Vladimir&option=202" target="_blank" rel="nofollow">Alvarado Vladimir;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=McLaughlin J. Fred&option=202" target="_blank" rel="nofollow">McLaughlin J. Fred;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Bagdonas Davin A.&option=202" target="_blank" rel="nofollow">Bagdonas Davin A.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Kaszuba John P.&option=202" target="_blank" rel="nofollow">Kaszuba John P.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Campbell Erin&option=202" target="_blank" rel="nofollow">Campbell Erin;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Grana Dario&option=202" target="_blank" rel="nofollow">Grana Dario;</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 Petroleum EngineeringUniversity of WyomingLaramie WY USA;</p> <p>Department of Petroleum EngineeringUniversity of WyomingLaramie WY USA;</p> <p>Center for Economic Geology ResearchUniversity of WyomingLaramie WY USA;</p> <p>Center for Economic Geology ResearchUniversity of WyomingLaramie WY USA;</p> <p>Department of Geology &</p> <p>GeophysicsUniversity of WyomingLaramie WY USA;</p> <p>Wyoming State Geological SurveyLaramie WY USA;</p> <p>Department of Geology &</p> <p>GeophysicsUniversity of WyomingLaramie WY USA;</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=NMR&option=203" rel="nofollow">NMR;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=rock characterization&option=203" rel="nofollow">rock characterization;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=restricted diffusion&option=203" rel="nofollow">restricted diffusion;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=diffusion coefficient distribution&option=203" rel="nofollow">diffusion coefficient distribution;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=T2 distribution&option=203" rel="nofollow">T2 distribution;</a> </p> <div class="translation"> 机译：NMR;岩石表征;限制扩散;扩散系数分布;T2分布; </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/0704025591842.html">Low‐Field Nuclear Magnetic Resonance Characterization of Carbonate and Sandstone Reservoirs From Rock Spring Uplift of Wyoming</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wang Heng&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Wang Heng,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Alvarado Vladimir&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Alvarado Vladimir,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=McLaughlin J. 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