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3-D Modelling and Experimental Comparison of Reactive Flow in Carbonates under Radial Flow Conditions

机译:径向流动条件下碳酸盐岩中反应流的3-D建模和实验比较

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摘要

We use a two-scale continuum model to simulate reactive flow and wormhole formation in carbonate rocks under 3-D radial flow conditions. More specifically, we present a new structure-property relationship based on the fractal geometry theory, to describe the evolution of local permeability, pore radius, and specific area with porosity variation. In the numerical calculation, to improve the convergence rate, the heterogeneous medium in question is extended by adding a thin layer of homogeneous porous medium to its inlet. We compare the simulation results with the available experimental observations and find that they are qualitatively consistent with each other. Additionally, sensitivity analysis of the dissolution process with respect to acid injection rate and rock heterogeneity, including heterogeneity magnitude and correlation length, is presented.
机译:我们使用两尺度连续模型来模拟3D径向流条件下碳酸盐岩中的反应流和虫洞形成。更具体地说,我们基于分形几何理论提出了一种新的结构-特性关系,以描述局部渗透率,孔半径和孔隙率变化的比表面积的演化。在数值计算中,为了提高收敛速度,通过在均质多孔介质的入口处添加薄层均质多孔介质来扩展所讨论的非均质介质。我们将模拟结果与可用的实验观察结果进行比较,发现它们在质量上相互一致。此外,提出了关于酸注入速率和岩石非均质性(包括非均质性大小和相关长度)的溶解过程敏感性分析。

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