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Effective Hydraulic Conductivity of Three-Dimensional Heterogeneous Formations of Lognormal Permeability Distribution: The Impact of Connectivity

机译:对数正态渗透率分布的三维非均质地层的有效水导率:连通性的影响

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摘要

Uniform mean flow takes place in a 3-D heterogeneous formation of normal hydraulic logconductivity Y=ln K. The aim of the study is to derive the dependence of the horizontal K-efh and vertical K-efv effective conductivities on the structural parameters of hydraulic conductivity and investigate the impact of departure from multi-Gaussianity on K-ef, by numerical simulations of flow in formations that share the same pdf and covariance of Y but differ in the connectivity of classes of Y. The main result is that for the extreme models of connected and disconnected high Y zones the ratio between the effective conductivities in isotropic media is much smaller than in 2-D. The dependence of Kefh and K-efv upon the logconductivity variance and the anisotropy ratio is compared with existing approximations (first-order, Landau-Matheron conjecture, self-consistent approximation). Besides the theoretical interest, the results offer a basis for empirical relationships to be used in applications.
机译:平均水流发生在正常水力对数电导率Y = ln K的3-D非均质地层中。研究的目的是推导出水平K-efh和垂直K-efv有效电导率对水力结构参数的依赖性通过对具有相同pdf和Y协方差但在Y类的连通性方面不同的地层中的流动进行数值模拟,研究电导率并研究背离多高斯性对K-ef的影响。主要结果是对于极值在连通和不连通的高Y区域模型中,各向同性介质中有效电导率之间的比率远小于二维。将Kefh和K-efv对数电导率方差和各向异性比率的依赖关系与现有近似值(一阶,Landau-Matheron猜想,自洽近似)进行比较。除了理论上的兴趣外,结果还为在应用中使用经验关系提供了基础。

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