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stress sensitivity of fractured reservoirs

机译:裂缝性储层的应力敏感性

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A fractured reservoir has a rock mechanical character which can be described by considering it to be built up from intact rock bounded by mechanical discontinuities. These discontinuities have been formed by natural processes and comprise fractures which normally make a steep angle to bedding, and the frequently ignored bedding-plane parallel discontinuities caused by, for example, weak clay-rich layers in clastics, or stylolites in carbonates. Both the intact rock and the discontinuities exhibit sensitivity to stress. In the case of the intact rock, this expresses itself as a pore geometry sensitivity which influences permeabilities and capillary pressures, with the changes being influenced by the stress-state. In the case of the discontinuities, three types of permeability changes are proposed, depending ~on the stress and strain which develops across the discontinuity. Importantly, all the constitutive laws for permeability stress-sensitivity can now be incorporated in simulations. While allowing for these effects complicates the simulation of fractured reservoirs, the enhanced realism brought to the simulation should improve the efficacy of the reservoir management.
机译:裂缝性储层具有岩石力学特征,可以通过考虑其由受机械不连续性限制的完整岩石构造来描述。这些不连续性是通过自然过程形成的,包括通常与地层成陡峭角度的裂缝,以及由例如碎屑中富含粘土的薄弱层或碳酸盐中的辉石引起的层理面平行不连续性。完整的岩石和不连续面都表现出对应力的敏感性。对于完整的岩石,这表现为孔隙几何敏感性,它会影响渗透率和毛细压力,而变化会受应力状态的影响。在不连续的情况下,提出了三种类型的渗透率变化,这取决于整个不连续处产生的应力和应变。重要的是,所有渗透率应力敏感性的本构定律现在都可以纳入模拟中。尽管考虑到这些影响使裂缝性储层的模拟复杂化,但模拟带来的增强的真实感应该可以提高储层管理的效率。

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