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RESERVOIR COMPACTION, STRAIN LOCALIZATION AND HYDROMECHANICAL COUPLING

机译:储层压实,应变局部化和水力耦合

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摘要

In the constitutive modeling and numerical simulation of mechanical compaction in reservoir mechanics, it is often assumed that the deformation is delocalized so that the possibility of strain localization is ignored. However, recent field and laboratory observations in porous sandstones have documented the pervasive occurrence of compaction localization, and in particular compaction bands have been observed to develop as tabular zones subperpendicular to the maximum compression direction. As a failure mode compaction bands have proved to be very effective in reducing the permeability by orders of magnitude over relativelysmall amount of strain. In this paper we summarize recent advances in our understanding of several questions related to compaction and hydromechanical coupling, specifically (1) constitutive modeling of mechanical compaction and bifurcation analysis of strain localization; (2) influence of compaction and strain localization on permeability; and (3) CT-imaging of compaction band and the micromechanics of compaction localization.
机译:在储层力学中机械压实的本构模型和数值模拟中,通常假设变形是局部的,从而忽略了应变局部化的可能性。但是,最近在多孔砂岩中进行的现场和实验室观察已记录了压实局部现象的普遍发生,尤其是观察到压实带以垂直于最大压缩方向的平板状区域发展。作为一种失效模式,压实带已被证明在相对较小的应变量下非常有效地将磁导率降低了几个数量级。在本文中,我们总结了我们对与压实和流体力学耦合有关的几个问题的理解的最新进展,特别是(1)机械压实的本构模型和应变局部化的分叉分析; (2)压实和应变局部化对渗透率的影响; (3)压实带的CT成像及压实定位的微观力学。

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