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On the relationship between effective permeability and stress for unconventional rocks: Analytical estimates from laboratory measurements

机译:关于非传统岩石有效渗透性与应力的关系:实验室测量的分析估计

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摘要

Permeability measurements show that unconventional rock is considerably stress sensitive because the matrix permeability is likely controlled by micro cracks and bedding structures in unconventional reservoirs. While there are a number of laboratory studies in the literature on the dependency of core-scale permeability on effective stress for unconventional rocks, how to determine the corresponding large-scale stress-dependency relationship (of more interest to practical applications) from the laboratory measurements has not been systematically investigated. This work proposes a method to estimate such a large-scale relationship from laboratory measurements.
机译:渗透性测量表明,由于基质渗透率可能受到非常规储层中的微裂纹和床上用品结构来控制的非常规岩石显着敏感。 虽然文献中有许多实验室研究关于核心磁化性对非传统岩石的有效应力的依赖性,但如何确定来自实验室测量的相应大规模应力依赖关系(对实际应用的更多兴趣) 尚未系统地调查。 这项工作提出了一种从实验室测量估计这种大规模关系的方法。

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