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Pore-Scale Modeling of Multiphase Flow in Fractures and Matrix/Fracture Transfer

机译:裂缝中多相流的孔隙尺度建模与基质/裂缝转移

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We use pore-scale network modeling to simulate imbibition in fractures and the matrix/fracture interaction. We represent the fracture as a two-dimensional lattice of conceptual pores and throates. We allow flow in connected wetting layers that occupy roughness and crevices in the pore space. We model piston-like advance with a capillary pressure that accounts for the curvature of the meniscus due to the fracture aperture, as well as the curvature of the wetting front in the fracture plane. We show that the model gives results that are insensitive to the resolution or pore spacing of the network. To account for viscous forces, the wetting phase pressure is computed assuming a fixed conductance in wetting layers. This pressure, in combination with the local capilary pressure, is used to determine the displacement sequence. A matrix is incorporated by surrounding the twodimensional fracture plane by a three-dimensional network of pores and throats. We model multiphase flow in a real fracture using an aperture distribution obtained from CT scanning. The simulated saturation distributions agree with those measured using in situ imaging. We also study the matrix/fracture transfer in a large three-dimensional network.
机译:我们使用孔隙尺度网络模型来模拟裂缝中的吸水作用和基质/裂缝相互作用。我们将裂缝表示为概念孔和喉咙的二维晶格。我们允许在连接的润湿层中流动,这些润湿层占据了孔空间中的粗糙度和缝隙。我们用毛细压力模拟活塞状的推进,毛细压力解释了由于断裂孔引起的弯月面的曲率,以及在断裂面上的湿润前沿的曲率。我们表明该模型给出的结果对网络的分辨率或孔间距不敏感。为了考虑粘性力,假设在润湿层中的电导率固定,则计算润湿相压力。该压力与局部毛细血管压力一起用于确定位移顺序。通过用孔和喉的三维网络围绕二维断裂面并入基体。我们使用从CT扫描获得的孔径分布对真实裂缝中的多相流进行建模。模拟的饱和度分布与使用原位成像测量的饱和度分布一致。我们还研究了大型三维网络中的基质/裂缝转移。

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