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ANALYSIS OF ROCK MICROSTRUCTURE USING HIGHRESOLUTION X-RAY TOMOGRAPHY

机译:高分辨率X射线断层扫描的岩石微观结构分析

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In previous work we have described and validated robust techniques for partitioning the pore space of a porous material into simple regions, thereby allowing it to be represented by a network of simple building blocks. The primary purpose of this analysis is the generation of a pore-throat network for modelling immiscible multi-phase fluid displacements. However, combining our partitioning algorithms with recently developed methods for studying complex and disordered networks, and geometric studies of the building blocks themselves, results in powerful tools for characterising rock microstructure. We extend this approach by applying the analysis to both the pore space and its complement, the grain space. Partitioning the grain space has particular meaning for clastic rocks where it is equivalent to identifying individual grains. Studying the two interpenetrating networks that result gives us a more complete description of the material, and in particular, gives us the chance to study causal relationships linking microstructure to macroscopic properties. We apply this methodology to a selection of clastic and carbonate rock images from the library of samples imaged at the ANU X-Ray micro-CT facility. For the clastic samples, we are able to assess whether differences in porosity and connectivity are the result of variations in grain size, grain shape or packing efficiency. For all samples, we look at the robustness and usefulness of several characterisation measures.
机译:在先前的工作中,我们描述和验证了用于将多孔材料的孔隙空间划分为简单区域的鲁棒技术,从而允许它由简单构建块的网络表示。该分析的主要目的是产生用于建模不混溶的多相流体位移的孔隙型网络。然而,将划分算法与最近开发的方法相结合,用于研究复杂和无序网络的方法,以及建筑物本身的几何研究,导致用于表征岩石微观结构的强大工具。我们通过将分析应用于孔隙空间及其补充,谷物空间来扩展这种方法。分隔颗粒空间对于碎屑岩体具有特殊意义,在那里它相当于识别单个颗粒。研究结果的两个互进网络使我们能够更完整地描述材料,特别是,给我们有机会研究将微观结构连接到宏观性质的因果关系。我们将该方法应用于从ANU X射线微型CT设施上成像的样本库中的一种选择的碎屑和碳酸盐岩图像。对于碎屑样本,我们能够评估孔隙率和连接是否是晶粒尺寸,晶粒形状或包装效率变化的结果。对于所有样本,我们介绍了几种特征措施的稳健性和有用性。

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