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Depletion-Induced Permeability Changes in Naturally-Fractured Gas-Sorbing Formations: A Double-Porosity Fluid Flow and Poromechanical Model

机译:天然压裂含气地层的贫化诱导渗透率变化:双孔渗流和岩体力学模型

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Reservoir stress changes associated with pore-pressure depletion are well-known to have significant impact on permeability in reservoirs with abundant natural fractures In most fractured reservoirs depletion induces increases of effective stresses and therefore a decrease in permeability. However, some reservoirs that accommodate significant amounts of gas adsorbed in organic micropores in the rock matrix can manifest opposite trends with increases in permeability during depletion. This permeability enhancement occurs due to stress relaxation and opening of fractures induced by rock matrix shrinkage during gas desorption. Additionally, pore pressure drawdown results in increased stress anisotropy potentially leading to reactivation of critically-oriented fractures and shear failure Fracture and rock matrix depletion have different time scales which depend on fracture permeability, rock matrix permeability, surface area of fractures in contact with the rock matrix, and fracture connectivity among others. The objective of this paper is to present a FEM solution of a double-porosity coupled poromechanical model that discriminates fracture pressure and rock matrix pressure and accounts for desorption-induced stresses. The results of the study show that implications from desorption such as gas production and stress relaxation can be significantly delayed with respect to fracture depletion, and therefore, wellhead pressure. We highlight the importance of multiple-porosity approach in calculating the timing of sorption stresses, which is crucial when modeling production in stress-sensitive unconventional reservoirs.
机译:众所周知,与孔隙压力枯竭相关的储层应力变化对天然裂缝丰富的储层的渗透率有重要影响。在大多数裂缝性储层中,枯竭引起有效应力增加,从而降低了渗透率。但是,一些在岩石基质中容纳大量吸附在有机微孔中的气体的储层可能会显示出相反的趋势,即在枯竭过程中渗透率会增加。渗透率的提高是由于气体解吸过程中岩石基体收缩引起的应力松弛和裂缝开裂而发生的。此外,孔隙压力下降会导致应力各向异性增加,从而可能导致重新定向的裂缝和剪切破坏。裂缝和岩石基质耗竭具有不同的时间尺度,这取决于裂缝的渗透率,岩石基质的渗透率,与岩石接触的裂缝的表面积基质,以及裂缝之间的连通性。本文的目的是提出一种双孔隙耦合岩体力学模型的有限元解决方案,该模型能够识别裂缝压力和岩石基质压力,并解释解吸引起的应力。研究结果表明,相对于裂缝耗竭,井口压力,诸如气体产生和应力松弛之类的解吸作用可能会大大延迟。我们强调了多孔方法在计算吸附应力时机中的重要性,这在对应力敏感的非常规油藏进行建模时至关重要。

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