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Effective conductivity in steady well-type flows through porous formations

机译:稳定井型中的有效电导率流经多孔地层

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A steady flow generated by a well of given strength takes place in a two-dimensional heterogeneous porous formation where the conductivity K is modeled as a random space function (RSF). As a consequence, the flow-variables become RSF s, and we wish to compute the effective conductivity (EC) by means of the self-consistent approximation. Toward this aim, the porous formation is sought as a collection of circular, non overlapping, inclusions with different (and statistically independent) conductivities. We compute the EC by adapting a procedure which was originally developed for mean uniform flows. Overall, the EC is found to be position-dependent, and therefore it can not be regarded as a medium's property (unless one is dealing with large distances from the well). Then, it is shown how results of the present study can be used for practical applications.
机译:由给定强度的井产生的稳定流发生在二维非均质多孔地层中,其中电导率K被建模为随机空间函数(RSF)。因此,流量变量变为RSF s,我们希望通过自洽近似来计算有效电导率(EC)。为了达到这个目的,寻求多孔形成物是具有不同(和统计上独立)电导率的圆形,非重叠,夹杂物的集合。我们通过采用最初为平均流量均匀开发的程序来计算EC。总体而言,发现EC与位置有关,因此不能将其视为介质的属性(除非有人要处理距井很远的距离)。然后,说明了如何将本研究的结果用于实际应用。

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