摘要
对未切至含水层的底板以三维流形式补给承压含水层的"非完整河",在有限单元法计算时,若直接按切至含水层底板以二维流方式补给的已知水位一类边界来处理,会夸大河流的补给量,不能较真实地模拟水源地水文地质模型。本文以武汉市武钢地下水水源地为例,阐述了用"贴边法"对此类边界的处理尝试。
The author deals with the underground water source in Wuhan Iron & Steel Corporation,where exists an imperfect river whose water is recharged in three dimensions,instead of in two dimensions in perfect river.The boundary-adding method,a finite element one,is used.
出处
《湖北地矿》
2003年第1期23-26,56,共5页
Hubei Geology & Mineral Resources
