Generalized Solution for Double-Porosity Flow Through a Graded Excavation Damaged Zone

IF 2.8 3区 地球科学 Q2 GEOSCIENCES, MULTIDISCIPLINARY
Kristopher L. Kuhlman
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Abstract

Prediction of flow to boreholes or excavations in fractured low-permeability rocks is important for resource extraction and disposal or sequestration activities. Analytical solutions for fluid pressure and flowrate, when available, are powerful, insightful, and efficient tools enabling parameter estimation and uncertainty quantification. A flexible porous media flow solution for arbitrary physical dimensions is derived and extended to double porosity for converging radial flow when permeability and porosity decrease radially as a power law away from a borehole or opening. This distribution can arise from damage accumulation due to stress relief associated with drilling or mining. The single-porosity graded conductivity solution was initially found for heat conduction, the arbitrary dimension flow solution comes from hydrology, and the solution with both arbitrary dimension and graded permeability distribution appeared in reservoir engineering. These existing solutions are combined and extended here to two implementations of the double-porosity conceptual model, for both a simpler thin-film mass transfer and more physically realistic diffusion between fracture and matrix. This work presents a new specified-flowrate solution with wellbore storage for the simpler double-porosity model, and a new, more physically realistic solution for any wellbore boundary condition. A new closed-form expression is derived for the matrix diffusion solution (applicable to both homogeneous and graded problems), improving on previous infinite series expressions.

Abstract Image

通过分级挖掘损坏区的双孔隙流的广义解法
对于资源开采、处置或封存活动而言,预测流体流向裂隙低渗透岩石中的钻孔或开挖口非常重要。流体压力和流速的分析解决方案(如果可用)是功能强大、见解深刻且高效的工具,可用于参数估计和不确定性量化。当渗透率和孔隙率在远离钻孔或开口的径向呈幂律递减时,推导出一种适用于任意物理尺寸的灵活多孔介质流动解决方案,并将其扩展到双孔隙率的收敛径向流动。这种分布可能是由于钻孔或采矿时的应力释放造成的损伤积累。单一孔隙率分级传导解法最初是为热传导而发现的,任意尺寸流动解法来自水文学,而同时具有任意尺寸和分级渗透率分布的解法则出现在储层工程中。本文将这些现有的解决方案结合起来,并扩展到双孔隙概念模型的两种实施方案中,既适用于更简单的薄膜传质,也适用于更符合物理实际的裂缝与基质之间的扩散。这项工作为较简单的双孔隙模型提出了一种新的带有井筒存储的指定流速解决方案,并为任何井筒边界条件提出了一种新的、更符合物理实际的解决方案。通过改进之前的无穷级数表达式,得出了矩阵扩散解的新闭式表达式(适用于同质和分级问题)。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Mathematical Geosciences
Mathematical Geosciences 地学-地球科学综合
CiteScore
5.30
自引率
15.40%
发文量
50
审稿时长
>12 weeks
期刊介绍: Mathematical Geosciences (formerly Mathematical Geology) publishes original, high-quality, interdisciplinary papers in geomathematics focusing on quantitative methods and studies of the Earth, its natural resources and the environment. This international publication is the official journal of the IAMG. Mathematical Geosciences is an essential reference for researchers and practitioners of geomathematics who develop and apply quantitative models to earth science and geo-engineering problems.
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