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A phase-by-phase upstream scheme that converges to the vanishing capillarity solution for countercurrent two-phase flow in two-rock media

机译:逐步收敛到逐渐消失的毛细作用解的逆流两相介质中的两相流方案

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摘要

We discuss the convergence of the upstream phase-by-phase scheme (or upstream mobility scheme) towards the vanishing capillarity solution for immiscible incompressible two-phase flows in porous media made of several rock types. Troubles in the convergence were recently pointed out by Mishra and Jaffre (Comput. Geosci. 14, 105-124, 2010) and Tveit and Aavatsmark (Comput. Geosci. 16, 809-825, 2012). In this paper, we clarify the notion of vanishing capillarity solution, stressing the fact that the physically relevant notion of solution differs from the one inferred from the results of Kaasschieter (Comput. Geosci. 3, 23-48, 1999). In particular, we point out that the vanishing capillarity solution depends on the formally neglected capillary pressure curves, as it was recently proven in by Andreianov and Cances (Comput. Geosci. 17, 551-572, 2013). Then, we propose a numerical procedure based on the hybridization of the interfaces that converges towards the vanishing capillarity solution. Numerical illustrations are provided.
机译:我们讨论了由几种岩石构成的多孔介质中不可混溶的不可压缩两相流向消失的毛细作用解的上游分步方案(或上游迁移方案)的收敛性。 Mishra和Jaffre(Comput。Geosci。,14,105-124,2010)和Tveit和Aavatsmark(Comput。Geosci。,16,809-825,2012)最近指出了收敛的麻烦。在本文中,我们阐明了消失的毛细作用解的概念,强调了这样一个事实,即与物理相关的解的概念与从Kaasschieter的结果推论得出的概念不同(Comput。Geosci。3,23-48,1999)。特别要指出的是,消失的毛细作用解决方案取决于形式上被忽略的毛细管压力曲线,最近由Andreianov和Cances证明了这一点(Comput。Geosci。17,551-572,2013)。然后,我们提出了一个基于界面混合的数值过程,该过程收敛于消失的毛细作用解。提供了数字插图。

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