地表河网-地下水流系统耦合模拟Ⅱ:应用实例  

Coupled modeling of surface water-groundwater system Ⅱ.Application

作　　者：武强[1] 徐军祥[1] 张自忠[1] 马振民[1] 

机构地区：[1]中国矿业大学(北京)水资源与环境研究所,北京100083

出　　处：《水利学报》2005年第6期754-758,共5页Journal of Hydraulic Engineering

基　　金：教育部科技重大项目 (2 0 0 4 2 95 );国家自然科学基金项目 (4 9872 0 80 );国土资源部西部专项课题资助项目 (2 0 0 10 3 0 1-0 6)

摘　　要：本文将作者提出的地表河网-地下水流系统耦合模型应用于中国黑河流域下游水资源合理开发利用评价中。通过方案的比较得出研究区较为理想的水资源开发方案,即维持在1987～1988年间的水平,它基本可以保证黑河下游潜水含水层处于正均衡的运行状态。The coupled model for simulating the surface water-groundwater system developed by the authors are applied to assess the development and utilization of the water resources in the downstream reaches of Heihe River, China. The best development scheme for maintaining the equilibrium of phreatic aquifer is found by comparison of different schemes. It is found that the development and utilization of water resources must be kept at the level of 1987～1988,so that a healthy hydro-ecosystem can be realized.

关 键 词：耦合评价 黑河流域 一维明渠流 地下水流 

分 类 号：P641.2[天文地球—地质矿产勘探]