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Testing and evaluation of 2D/3D digital image analysis methods and inclusion theory for microporosity and S-wave prediction in carbonates

机译:碳酸盐碳酸盐液体微孔和S波预测的2D / 3D数字图像分析方法和夹杂物理论的测试与评价

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Three digital image analysis (DIA) methods are proposed to evaluate the geometric properties of the pore system in 2D/3D and identify the macro- and mesopores: 1) optical microscopy of thin sections computed by Fiji-ImageJ software, 2) mu CT data volume decomposition using 2D slices and Fiji-ImageJ, and 3) application of GEODICT, 2015) software and PoreShape GeoLab routines to compute the 3D pores. Microporosity is characterized using assumptions based on the difference between helium gas and the image porosity and the classification system by Anselmetti et al. and rock physics modeling of the differential effective medium theory is applied to estimate the micropore aspect ratio via Vp, supplying a calibrated method to predict Vs for similar rocks. According to the results, the 2D processing methods (#1 and #2) are more realistic and theoretically consistent for estimating 2D DIA parameters. The approximation of the detected 3D pores to 2D in method #3 results in poor representativeness of the pore texture, limiting the potential usefulness of the mu CT data, although the same resolution is inherent to the mu CT data volume and is applied in methods #2 and #3. The use of mu CT data from 2D slices (method #2) was evaluated as the best method for computing the 2D DIA parameters, and the optical thin sections used in method #1 were limited by differences in the resolution and the low representativeness of the micrograph quantity in correlating the texture complexities. This work generates a valuable outcrop dataset and original discussions of DIA at different image scales for input modeling to match ultrasonic and elastic properties with the lithological characteristics of Oman samples.
机译:提出了三种数字图像分析(DIA)方法以评估2D / 3D的孔系统的几何特性,并识别由Fiji-ImageJ软件计算的薄截面的宏观和中孔:1)光学显微镜,2)MU CT数据使用2D片和Fiji-Imagej的卷分解,以及3)GeoDict,2015)软件和Poreshape Geolab例程的应用来计算3D孔隙。微孔的特征在于使用基于氦气和图像孔隙率的差异和Anselmetti等人的分类系统的假设。差分有效介质理论的岩石物理建模应用于通过VP估计微孔宽高比,供应校准的方法来预测类似岩石的VS。根据结果​​,2D处理方法(#1和#2)更现实,并且理论上是为了估计2D直径参数。在方法#3中检测到的3D孔隙到2D的近似导致孔纹理的差,但是限制了MU CT数据的潜在有用性,尽管MU CT数据量是固有的,并且以方法应用于MU CT数据量。 2和#3。从2D切片(方法#2)的使用MU CT数据被评估为计算2D DIA参数的最佳方法,方法#1中使用的光学薄部分受到分辨率差异的限制和较低的代表性显微照片在关联质地复杂性时数量。这项工作产生了有价值的露头数据集和对不同图像尺度的原始讨论,用于输入建模,以将超声波和弹性性质与阿曼样品的岩性特征匹配。

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