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Multi-scale experimental and numerical simulation workflow of absolute permeability in heterogeneous carbonates

机译:多均匀碳酸盐绝对渗透性的多尺度实验性和数值模拟工作流程

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摘要

Digital Rock Physics (DRP) is a field that makes use of recent advances in imaging technology and computational methods to determine several rock properties by running numerical simulations on 3D rock images. In this work, DRP tools were used in a novel multi-scale approach that combined micro and macro computations to determine permeability for comparison with lab experiments of 2 different samples at 2 different sizes; 0.5 inch diameter and the standard 1.5 inch diameter. The Lattice Boltzmann Method (LBM) was used to perform micro-scale computations on subvolumes of images at high-resolution images. This was done to determine the permeability, and extract porosity-permeability trends. Then, a macro-scale computational grid was set to have porosity and permeability values from the micro-scale simulations in order to compute the upscaled effective permeability which could then be compared to experimental results. The workflow was first applied to a standard Silurian Dolomite to validate it and then applied to a carbonate sample from an Abu Dhabi reservoir that exhibited a higher level of heterogeneity.
机译:数字岩石物理(DRP)是一种领域,它通过在3D岩图像上运行数值模拟来确定近期成像技术和计算方法的领域。在这项工作中,DRP工具以新颖的多尺度方法使用,使微型和宏观计算组合以确定与2种不同尺寸的2种不同样品的实验室实验相比的渗透率; 0.5英寸直径和标准的1.5英寸直径。用格子Boltzmann方法(LBM)用于在高分辨率图像处对图像的子域进行微级计算。这是为了确定渗透性和提取孔隙率渗透性趋势。然后,将宏观计算网格设定为具有来自微级模拟的孔隙率和渗透率值,以计算可以与实验结果进行比较的上升的有效渗透率。首先将工作流程应用于标准的硅脲白云石以验证它,然后从阿布扎比储层应用于碳酸盐样品,其表现出更高水平的异质性。

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