An upwind generalized finite difference method (GFDM) for meshless analysis of heat and mass transfer in porous media

IF 2.8 3区 工程技术 Q1 MATHEMATICS, INTERDISCIPLINARY APPLICATIONS Computational Particle Mechanics Pub Date : 2022-09-06 DOI:10.1007/s40571-022-00501-w
Xiang Rao
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引用次数: 9

Abstract

In this paper, an upwind GFDM is developed for coupled heat and mass transfer problems in porous media. GFDM is a meshless method that can obtain the difference schemes of spatial derivatives by using Taylor expansion in local node influence domains and the weighted least squares method. The first-order single-point upstream scheme in the FDM/FVM-based reservoir simulator is introduced to GFDM to form the upwind GFDM, based on which a sequential coupled discrete scheme of the pressure diffusion equation and the heat convection-conduction equation is solved to obtain pressure and temperature profiles. This paper demonstrates that this method can be used to obtain the meshless solution of the convection–diffusion equation with a stable upwind effect. For porous flow problems, the upwind GFDM is more practical and stable than the method of manually adjusting the influence domain based on the prior information of the flow field to achieve the upwind effect. Two types of calculation errors are analyzed, and three numerical examples are implemented to illustrate the good calculation accuracy and convergence of the upwind GFDM for heat and mass transfer problems in porous media and indicate the increase in the radius of the node influence domain will increase the calculation error of temperature profiles. Overall, the upwind GFDM discretizes the computational domain using only a point cloud that is generated with much less topological constraints than the generated mesh, but achieves good computational performance as the mesh-based approaches, and therefore has great potential to be developed as a general-purpose numerical simulator for various porous flow problems in domains with complex geometry.

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多孔介质中无网格传热传质分析的迎风广义有限差分法(GFDM)
本文针对多孔介质中传热传质耦合问题,开发了一种迎风GFDM。GFDM是一种利用局部节点影响域泰勒展开和加权最小二乘法获得空间导数差分格式的无网格方法。将FDM/ fvm油藏模拟器中的一阶单点上游格式引入到GFDM中,形成迎风GFDM,在此基础上求解压力扩散方程和热对流传导方程的顺序耦合离散格式,得到压力和温度分布。结果表明,该方法可用于求解具有稳定逆风效应的对流扩散方程的无网格解。对于多孔流动问题,迎风GFDM比基于流场先验信息手动调整影响域以达到迎风效果的方法更实用、更稳定。分析了两种类型的计算误差,并通过三个数值算例说明了迎风GFDM对多孔介质传热传质问题具有良好的计算精度和收敛性,并指出节点影响域半径的增大会增大温度分布的计算误差。总体而言,迎风GFDM仅使用点云来离散计算域,该点云比生成的网格具有更少的拓扑约束,但与基于网格的方法相比具有良好的计算性能,因此具有很大的发展潜力,可以作为复杂几何结构域中各种多孔流动问题的通用数值模拟器。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Computational Particle Mechanics
Computational Particle Mechanics Mathematics-Computational Mathematics
CiteScore
5.70
自引率
9.10%
发文量
75
期刊介绍: GENERAL OBJECTIVES: Computational Particle Mechanics (CPM) is a quarterly journal with the goal of publishing full-length original articles addressing the modeling and simulation of systems involving particles and particle methods. The goal is to enhance communication among researchers in the applied sciences who use "particles'''' in one form or another in their research. SPECIFIC OBJECTIVES: Particle-based materials and numerical methods have become wide-spread in the natural and applied sciences, engineering, biology. The term "particle methods/mechanics'''' has now come to imply several different things to researchers in the 21st century, including: (a) Particles as a physical unit in granular media, particulate flows, plasmas, swarms, etc., (b) Particles representing material phases in continua at the meso-, micro-and nano-scale and (c) Particles as a discretization unit in continua and discontinua in numerical methods such as Discrete Element Methods (DEM), Particle Finite Element Methods (PFEM), Molecular Dynamics (MD), and Smoothed Particle Hydrodynamics (SPH), to name a few.
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