THE DUAL FORMULATION OF FLOW FOR CONTAMINANT TRANSPORT MODELING .1. REVIEW OF THEORY AND ACCURACY ASPECTS

被引:112
作者
FRIND, EO
MATANGA, GB
机构
[1] Univ of Waterloo, Dep of Earth, Sciences, Waterloo, Ont, Can, Univ of Waterloo, Dep of Earth Sciences, Waterloo, Ont, Can
关键词
FLOW OF WATER - Underground - HYDROLOGY - Computer Simulation;
D O I
10.1029/WR021i002p00159
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Steady state groundwater flow systems can be described by means of either potentials or stream functions. If the objective is the definition of migration paths and the identification of hydrogeologic parameters in the context of a contaminant transport study, stream functions can give results that are both more useful and more accurate than those obtained with potentials alone. In this paper the dual theory that links potentials and stream functions is reviewed with a focus on physical relevance in practical situations, and a dual finite element solution is developed. Advantages of the dual method, including the ease with which advective transport components can be evaluated, are discussed. It is shown by means of an example that the stream function solution can give superior accuracy in the definition of the velocity field required for transport simulations. Refs.
引用
收藏
页码:159 / 169
页数:11
相关论文
共 18 条
[1]  
Bear J., 2012, HYDRAULICS GROUNDWAT
[2]  
CHERRY JA, 1983, J HYDROL, V63, P1
[3]  
Freeze A.R., 1979, GROUNDWATER
[4]   Simulation of long-term transient density-dependent transport in groundwater [J].
Frind, Emil O. .
ADVANCES IN WATER RESOURCES, 1982, 5 (02) :73-88
[5]   THE DUAL FORMULATION OF FLOW FOR CONTAMINANT TRANSPORT MODELING .1. REVIEW OF THEORY AND ACCURACY ASPECTS [J].
FRIND, EO ;
MATANGA, GB .
WATER RESOURCES RESEARCH, 1985, 21 (02) :159-169
[6]  
FRIND EO, 1982, 10TH P WORLD C INT A
[7]  
FRIND EO, 1982, 4TH P INT C FIN EL W
[8]  
HILDEBRAND FB, 1965, ADV CALCULAUS APPLIC
[9]  
KIMMEL GE, 1980, 1085 US GEOL SURV PR
[10]  
Milne-Thomson L.M., 1968, THEORETICAL HYDRODYN