A Graph-theoretic Pipe Network Method for water flow simulation in a porous medium: GPNM

被引:27
作者
Xu, Z. H. [1 ,2 ]
Ma, G. W. [2 ]
Li, S. C. [1 ]
机构
[1] Shandong Univ, Geotech & Struct Engn Res Ctr, Jinan 250061, Shandong, Peoples R China
[2] Univ Western Australia, Sch Civil & Resource Engn, Perth, WA 6009, Australia
基金
中国国家自然科学基金;
关键词
Porous medium; Water flow; Pressure; Flow rate; Velocity; Graph-theoretic Pipe Network Method; FINITE-VOLUME METHOD; LATTICE BOLTZMANN-EQUATION; FLUID-FLOW; ELEMENT; INFLOW;
D O I
10.1016/j.ijheatfluidflow.2013.11.003
中图分类号
O414.1 [热力学];
学科分类号
摘要
A new numerical simulation method for water flow in a porous medium is proposed. A porous medium is discretized graph-theoretically into a discrete pipe network. Each pipe in the oriented network is defined as a weighted element with a starting node and an ending node. Equivalent hydraulic parameters are derived based on the Darcy's Law. A node law of flow rate and a pipe law of pressure are derived based on the conservation of mass and energy, as well as the graph-theoretic network theory. A unified governing equation for both the inner pipes and the boundary pipes are deduced. A conversion law of flow rate/velocity is proposed and discussed. A few case studies are analyzed and compared with those from analytical solutions and finite element analysis. It shows that the proposed Graph-theoretic Pipe Network Method (GPNM) is effective in analyzing water flow in a porous medium. The advantage of the proposed GPNM is that a continuous porous medium is discretized into a discrete pipe network, which is analyzed same as for a discrete fracture network. Solutions of water pressures and flow rates in the discrete pipe network are obtained by solving a system of nonhomogeneous linear equations. It is demonstrated with high efficiency and accuracy. The developed method can be extended to analyzing water flow in fractured and porous media in 3-D conditions. (C) 2013 Elsevier Inc. All rights reserved.
引用
收藏
页码:81 / 97
页数:17
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