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Stabilized finite element methods for vertically averaged multiphase flow for carbon sequestration

机译:稳定的有限元方法,用于碳封存的垂直平均多相流动

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摘要

A computationally efficient numerical model that describes carbon sequestration in deep saline aquifers is presented. The model is based on the multiphase flow and vertically averaged mass balance equations, requiring the solution of two partial differential equations - a pressure equation and a saturation equation. The saturation equation is a nonlinear advective equation for which the application of Galerkin finite element method (FEM) can lead to non-physical oscillations in the solution. In this article, we extend three stabilized FEM formulations, which were developed for uncoupled systems, to the governing nonlinear coupled PDEs. The methods developed are based on the streamline upwind, the streamline upwind/Petrov-Galerkin and the least squares FEM. Two sequential solution schemes are developed: a single step and a predictor-corrector. The range of Courant numbers yielding smooth and oscillation-free solutions is investigated for each method. The useful range of Courant numbers found depends upon both the sequential scheme (single step vs predictor-corrector) and also the time integration method used (forward Euler, backward Euler or Crank-Nicolson). For complex problems such as when two plumes meet, only the SU stabilization with an amplified stabilization parameter gives satisfactory results when large time steps are used. Copyright (C) 2016 John Wiley & Sons, Ltd.
机译:提出了描述深盐含水层中碳封存的计算上有效的数值模型。该模型基于多相流和垂直平均质量平衡方程,需要解决两个部分微分方程 - 压力方程和饱和方程。饱和方程是一种非线性平程方程,其应用Galerkin有限元方法(FEM)可以导致解决方案中的非物理振荡。在本文中,我们扩展了三种稳定的FEM配方,该FEM配方是为解耦系统开发的,用于控制非线性耦合PDE。开发的方法基于Streamline Upwind,Streamline Upwind / Petrov-Galerkin和最小二乘法式化。开发了两个顺序解决方案:单步和预测器校正器。针对每种方法研究了产生平滑和无振荡溶液的扶手数范围。找到的有用范围的扶手数量取决于顺序方案(单步VS预测器校正器)以及所使用的时间集成方法(转发欧拉,后向欧拉或曲柄尼洛尔森)。对于诸如两羽碱基时,仅使用扩增的稳定参数的SU稳定产生诸如苏稳定时,在使用大时间步骤时,苏稳定性会产生令人满意的结果。版权所有(c)2016 John Wiley&Sons,Ltd。

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