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Improved Determination of Stress-Dependent Permeability for Anisotropic Formations

机译:各向异性地层应力相关渗透率的改进测定

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Qualitative determination of formation permeability is oftenrnobtained through laboratory flow tests on core plugs.rnHowever, the experimental determination of the permeabilityrnfor anisotropic plugs (particularly the horizontal permeability)rnis difficult and less than perfect; generally relying on a highlyrnsimplified Darcy flow analysis. Numerical analyses couldrngreatly improve the resolution, reduce the testing costs, andrnallow parametric investigations using sophisticated 3-Drnformulations. This paper reports such an analysis thatrninterprets the analytical Darcy flow-pressure measurements,rnusing numerical results to provide a “geometric factor”. Arnnumerical iterative procedure correlates the core plugrnmeasured flow and pressures at the inlet and outlet boundariesrnfor different boundary sources to derive the core plugrnanisotropic permeabilities. Since stress changes generallyrninfluence permeability, a conceptual model is developed—rnagain via an iterative numerical method—that accounts for therneffects of the solid deformations. From this, numericalrnschemes have been developed using “equivalent geometricrnfactors” with embedded mechanisms for modifying core plugrnpermeability based on the changes in the solid strains thatrnsimulate the coupled flow-deformation behavior of selectedrnreservoir rocks. This is the first detailed 3-D numericalrnanalysis iterative scheme that practically allows realisticrndetermination of permeabilities in anisotropic core plugs.
机译:通常通过对岩心塞的实验室流动测试来定性确定地层渗透率。然而,各向异性塞的渗透率(特别是水平渗透率)的实验确定是困难且不完美的。通常依赖高度简化的Darcy流分析。数值分析可以极大地提高分辨率,降低测试成本,并且可以使用复杂的3-Drnulations进行参数研究。本文报告了这样一种分析,该分析解释了达西流动压力的分析测量结果,并利用数值结果提供了“几何因子”。数值迭代程序将岩心测得的流量和压力在不同边界源的入口和出口边界处相关联,以得出岩心各向同性的渗透率。由于应力变化通常会影响渗透率,因此,我们通过迭代数值方法再次建立了概念模型,该模型考虑了固体变形的影响。据此,已经开发出了具有“等效几何因子”的数值方案,该方案具有嵌入机制,可根据模拟选定储层岩石耦合流动变形行为的固体应变变化来修改岩心的渗透率。这是第一个详细的3-D数值分析迭代方案,实际上可实际确定各向异性岩心塞的渗透率。

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