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Dynamic coupling of pore-scale and reservoir-scale models for multiphase flow

机译:多相流孔尺度和储层尺度模型的动态耦合

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摘要

The concept of coupling pore-scale and continuum-scale models for subsurface flow has long been viewed as beneficial, but implementation has been slow. In this paper, we present an algorithm for direct coupling of a dynamic pore-network model for multiphase flow with a traditional continuum-scale simulator. The ability to run the two models concurrently (exchanging parameters and boundary conditions in real numerical time) is made possible by a new dynamic pore-network model that allows simultaneous injection of immiscible fluids under either transient-state or steady-state conditions. Allowing the pore-scale model to evolve to steady state during each time step provides a unique method for reconciling the dramatically different time and length scales across the coupled models. The model is implemented by embedding networks in selected gridblocks in the reservoir model. The network model predicts continuum-scale parameters such as relative permeability or average capillary pressure from first principles, which are used in the continuum model. In turn, the continuum reservoir simulator provides boundary conditions from the current time step back to the network model to complete the coupling process. The model is tested for variable-rate immiscible displacements under conditions in which relative permeability depends on flow rate, thus demonstrating a situation that cannot be modeled using a traditional approach. The paper discusses numerical challenges with this approach, including the fact that there is not a way to explicitly force pore-scale phase saturation to equal the continuum saturation in the host gridblock without an artificial constraint. Hurdles to implementing this type of modeling in practice are also discussed.
机译:长期以来,人们一直认为将孔隙尺度和连续尺度模型耦合用于地下流动的概念是有益的,但实施起来却很缓慢。在本文中,我们提出了一种用于多相流动态孔隙网络模型与传统连续谱规模模拟器直接耦合的算法。新的动态孔隙网络模型使同时运行两个模型(实时交换参数和边界条件)的能力成为可能,该模型允许在瞬态或稳态条件下同时注入不混溶的流体。允许孔隙尺度模型在每个时间步长演变为稳态,提供了一种独特的方法,可以在耦合模型之间协调截然不同的时间尺度和长度尺度。该模型是通过将网络嵌入储层模型中选定的网格块中来实现的。网络模型根据连续原理模型中使用的第一性原理预测连续体比例参数,例如相对渗透率或平均毛细压力。反过来,连续储层模拟器提供了从当前时间步回到网络模型的边界条件,以完成耦合过程。在相对渗透率取决于流速的条件下测试了该模型的可变速率不混溶位移,因此证明了使用传统方法无法建模的情况。本文讨论了使用此方法的数值挑战,包括以下事实:在没有人为约束的情况下,没有一种方法可以显式地强制孔隙尺度相饱和度等于宿主网格块中的连续体饱和度。还讨论了在实践中实施此类建模的障碍。

著录项

  • 来源
    《Water resources research》 |2013年第9期|5973-5988|共16页
  • 作者

    Qiang Sheng; Karsten Thompson;

  • 作者单位

    Department of Chemical Engineering, Louisiana State University, Baton Rouge, Louisiana, USA;

    Department of Petroleum Engineering, Louisiana State University, 2107 Patrick F. Taylor Hall, Baton Rouge, LA 70803, USA;

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  • 正文语种 eng
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