摘要
在西北干旱区内陆河流域盆地, 地表水与地下水转化频繁, 研究地表水与地下水转化对于有效地开发利用水资源和预测地下水环境的变化具有重要的意义. 运用地下水和地表水中稳定同位素δ18O值存在明显差异的特点, 在黑河中游盆地沿不同河段地表水和地下水现场取样, 进行同位素分析.结果表明: 在黑河中游盆地绿洲灌溉区, 农田灌溉严重影响了地下水和地表水之间的转化, 导致地下水补给地表水的增加. 运用质量守恒原理, 定量分析了黑河中游盆地黑河地下水与地表水转化的转化量, 为正确评价和合理利用水资源奠定了基础.
In arid regions of western China, water resources come from mountain watersheds and disappear in the desert plains. The exchange of surface water and groundwater takes place two or three times in a basin. It is essential to analyze the interaction between groundwater and surface water, so as to use water resources effectively and predict the change in the water environment. The conventional method of analysis, however, measures only the flow of a stream and cannot determine groundwater seepage accurately. Because of the distinct difference of {δ^(18)O} between groundwater and surface water, the method of using {{}^(18)O} was examined as an indicator for analyzing the interaction. With the addition of the mass balance equation, the composite proportion of different mixing components can be calculated. A conclusion was drawn from the computed result that, in the oases of the middle Heihe River, flood irrigation on vast farmlands has made a great impact on the transform between groundwater and surface water. The irrational irrigation has caused some problems, such as environmental deterioration and land subsidence.
出处
《冰川冻土》
CSCD
北大核心
2005年第1期106-110,共5页
Journal of Glaciology and Geocryology
基金
国家自然科学基金重大研究计划项目(90102003)
中国科学院知识创新工程重大项目(KZCX1 10 03)
2000年教育部科学技术研究重点项目(00233)资助
关键词
黑河
稳定同位素
质量守恒原理
地下水与地表水转化
Heihe River
stable isotope
water balance
interaction between groundwater and surface water
