Analytical and Numerical Groundwater Flow Solutions for the FEMME-Modeling Environment

被引:10
|
作者
El-Rawy, Mustafa [1 ,2 ]
Batelaan, Okke [3 ]
Buis, Kerst [4 ]
Anibas, Christian [5 ,6 ]
Mohammed, Getachew [7 ]
Zijl, Wouter [8 ]
Salem, Ali [1 ,9 ]
机构
[1] Menia Univ, Fac Engn, Civil Engn Dept, Al Minya 61111, Egypt
[2] Shaqra Univ, Coll Engn, Civil Engn Dept, Dawadmi 11911, Ar Riyadh, Saudi Arabia
[3] Flinders Univ S Australia, Coll Sci & Engn, Natl Ctr Groundwater Res & Training, GPO Box 2100, Adelaide, SA 5001, Australia
[4] Univ Antwerp, Dept Biol, Ecosyst Management Res Grp ECOBE, Univ Pl 1, B-2610 Antwerp, Belgium
[5] UNSW Sydney, Water Res Lab, Sch Civil & Environm Engn, Sydney, NSW 2052, Australia
[6] UNSW Sydney, Connected Waters Initiat Res Ctr, Sydney, NSW 2052, Australia
[7] Golder Associates, 700 2 St Southwest, Calgary, AB T2P 2W2, Canada
[8] Vrije Univ Brussel, Dept Hydrol & Hydraul Engn, Pl Laan 2, B-1050 Brussels, Belgium
[9] Univ Pecs, Doctoral Sch Earth Sci, IfjUsag Utja 6, H-7624 Pecs, Hungary
关键词
groundwater-surface water interaction; analytical; numerical; FEMME; STRIVE; MODFLOW; SURFACE-WATER; BOUSSINESQ EQUATION; AQUIFER; STREAM; TRANSIENT; STATE; RIVER;
D O I
10.3390/hydrology7020027
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
Simple analytical and numerical solutions for confined and unconfined groundwater-surface water interaction in one and two dimensions were developed in the STRIVE package (stream river ecosystem) as part of FEMME (flexible environment for mathematically modelling the environment). Analytical and numerical solutions for interaction between one-dimensional confined and unconfined aquifers and rivers were used to study the effects of a 0.5 m sudden rise in the river water level for 24 h. Furthermore, a two-dimensional groundwater model for an unconfined aquifer was developed and coupled with a one-dimensional hydrodynamic model. This model was applied on a 1 km long reach of the Aa River, Belgium. Two different types of river water level conditions were tested. A MODFLOW model was set up for these different types of water level condition in order to compare the results with the models implemented in STRIVE. The results of the analytical solutions for confined and unconfined aquifers were in good agreement with the numerical results. The results of the two-dimensional groundwater model developed in STRIVE also showed that there is a good agreement with the MODFLOW solutions. It is concluded that the facilities of STRIVE can be used to improve the understanding of groundwater-surface water interaction and to couple the groundwater module with other modules developed for STRIVE. With these new models STRIVE proves to be a powerful example as a development and testing environment for integrated water modeling.
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页数:18
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