首页> 外文会议>International Symposium of the Society of Core Analysts >JOINT X-RAY AND NEUTRON TOMOGRAPHY OF SHALE CORES FOR CHARACTERIZING STRUCTURAL MORPHOLOGY
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JOINT X-RAY AND NEUTRON TOMOGRAPHY OF SHALE CORES FOR CHARACTERIZING STRUCTURAL MORPHOLOGY

机译:页岩核心关节X射线和中子断层扫描,用于表征结构形态学

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To better model the storage and flow of gas and light hydrocarbons in shales,it is necessary to quantify the structural distributions of organic and inorganic components and fractures in shales over a large range of length scales. The combination of neutron and X-ray tomography provides these distributions on the core scale,in contrast to most current μm-scale SEM studies. We present a new conjoint X-ray and neutron computed tomography(CT)for 3D shalecore characterization. Neutrons are attenuated significantly by hydrogen compared with most other elements. Therefore,the hydrogen-rich areas,i.e. organic matter can be easily distinguished from fractures and inorganic,hydrogen-poor matter. On the other hand,Xrays are attenuated more when the atomic number Z of the element is larger and can be used to identify high-Z elements such as minerals. Therefore,combining X-ray and neutron tomography can provide much more comprehensive information of shale. The combination of neutron and X-ray tomography allows one to identify different minerals,fractures,and organic matter for improved and more realistic representation of the rock 3D structure.
机译:为了更好地模型Shales中的气体和轻质碳氢化合物的储存和流量,有必要在大范围的长度范围内量化有机和无机成分的结构和无机成分的结构分布和骨折。与大多数电流μM级SEM研究相比,中子和X射线断层扫描的组合提供了这些分布。我们为3D Shalecore表征提供了一个新的联合X射线和中子计算断层扫描(CT)。与大多数其他元素相比,中子通过氢气显着减弱。因此,富含氢区域,即。有机物可以容易地与骨折和无机,氢气差的物质区分开来。另一方面,当元件的原子Z更大并且可用于识别诸如矿物质的高Z元素时,XRAYS更加衰减。因此,组合X射线和中子断层扫描可以提供更全面的页岩信息。中子和X射线断层扫描的组合允许人们识别不同的矿物质,裂缝和有机物质,以改善岩石3D结构的改善和更现实的表示。

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