Identification of hydraulic conductivity distributions in density dependent flow fields of submarine groundwater discharge modeling using adjoint-state sensitivities

被引:0
|
作者
HU Bill X [1 ,2 ]
CAO YanZhao [3 ]
ZHAO WeiDong [4 ]
BAO Feng [3 ]
机构
[1] School of Water Resources and Environmental Sciences, China University of Geosciences
[2] Department of Geological Sciences, Florida State University
[3] Department of Mathematics and Statistics, Auburn University
[4] School of Mathematics, Shandong University
基金
中国国家自然科学基金;
关键词
Variable-density flow; Hydraulic conductivity; Inverse method; Adjoint partial differential equation; Submarine groundwater discharge;
D O I
暂无
中图分类号
P641.2 [地下水动力学];
学科分类号
0818 ; 081803 ;
摘要
A mathematical optimal control method is developed to identify a hydraulic conductivity distribution in a density dependent flow field. Using a variational method, the adjoint partial differential equations are obtained for the density-dependent state equations used for the saline aquifer water flow. The adjoint equations are numerically solved in through a finite difference method. The developed method is applied to identify the hydraulic conductivity distribution through the numerical solution of an optimal control problem. To demonstrate the effectiveness of the optimal control method, three numerical experiments are conducted with artificial observation data. The results indicate that the developed method has the potential to accurately identify the hydraulic conductivity distribution in a saline water aquifer flow system.
引用
收藏
页码:770 / 779
页数:10
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