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Dual Pore Network Model of Electrical Resistivity for Carbonate Rocks

机译:碳酸盐岩电阻率的双孔网模型

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We develop a model which explains the non-Archie behavior of carbonate rocks with multi-scale structure. Non-Archie behavior in such rocks is qualitatively related to the degree of connectedness(percolation)of different water fractions,namely water residing in networks comprising pores of very disparate scales(micro-porosity and macro-porosity). To this end,we investigate here a previously reported dual pore network model(D-PNM)which allows for heterogeneous matrix(micro-porosity)properties and variably-connected macro-porosity. By varying the relative amounts,geometric properties and degree of connectedness of microporosity and macro-porosity,we are able to stylistically reproduce all documented deviations of the resistivity index from Archie behavior.
机译:我们开发了一种模型,解释了具有多尺度结构的碳酸盐岩的非原始行为。 这种岩石中的非Archie行为与不同水分分数的关联度(渗透)的定性相关,即驻留在包含非常不同的尺度(微孔隙率和宏观孔隙率)的网络中的水。 为此,我们在此进行先前报告的双孔网络模型(D-PNM),其允许异质基质(微孔隙度)性能和可变连接的宏观孔隙度。 通过改变微孔孔隙度和宏观孔隙的相对量,几何特性和程度,我们能够模拟地再现来自Archie行为的所有记录的电阻率指数的偏差。

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