Steady-state analysis of water movement in a semi-infinite unconfined aquifer under constant accretion

被引：1

作者：

Kalin, L ^{[1
]}

Govindaraju, RS

Parlange, JY

机构：

[1] Purdue Univ, Sch Civil Engn, W Lafayette, IN 47907 USA

[2] Cornell Univ, Dept Agr & Biol Engn, Ithaca, NY 14853 USA

来源：

TRANSPORT IN POROUS MEDIA | 2000年 / 40卷 / 02期

关键词：

Boundary Condition; Steady State; Civil Engineer; Water Movement; Water Flux;

D O I：

10.1023/A:1006652007287

中图分类号：

TQ [化学工业];

学科分类号：

0817 ;

摘要：

A partial analysis of the stream-aquifer interaction problem at steady state for a semi-infinite unconfined aquifer was presented by Bear (1979). This analysis was restricted to the case of influent boundary condition where the water flux is directed from the boundary into the aquifer. Here, we extend the analysis to provide analytical solutions for both influent and effluent conditions. Comparisons with numerical solutions are also presented for further validation.

引用

页码：165 / 169

页数：5

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