开都河河道渗透补给地下水分析  

Analysis on Exchanging Relationship Between Kaidu River Water and Groundwater

作　　者：彭秋燕[1] 周玉良[2] 姜卉芳[1] 

机构地区：[1]新疆农业大学水利与土木工程学院,新疆乌鲁木齐830052 [2]合肥工业大学土木与水利工程学院,安徽合肥230009

出　　处：《水利与建筑工程学报》2013年第3期103-106,共4页Journal of Water Resources and Architectural Engineering

基　　金：新疆水文学及水资源重点学科基金资助(xjsxszyzdxk20101202)

摘　　要：干旱典型区焉耆盆地的农业灌溉可持续发展,受制于开都河河水以及开都河流域地下水的有效利用。在总结河道渗透补给地下水量计算方法的基础上,选用河道水量平衡法对开都河枯水期河道渗透补给地下水量做了分析,得出该河流河水与地下水的补排关系及补排量。以期对焉耆盆地合理利用水资源、改善生态环境、农业灌溉可持续发展提供一定的依据。The sustainable development of agricultural irrigation in the typically arid utilization of both Kaidu river water and groundwater. Here, based on summarizing exchanging amount between the river water and groundwater, the fiver water balance area Yanqi Basin is subjective to the the methods for calculating the water method is adopted to analyze the interaction between Kaidu fiver water and groundwater in drought periods, and the exchanging relationship and volume between the fiver water and groundwater are also derived, so as to provide a theoretic basis for reasonably utilizing the precious water resourees, improving the ecological environment and the sustainable development of agricultural irrigation in Yanqi Basin.

关 键 词：焉耆盆地 开都河 河道 渗透补给 地下水 

分 类 号：P333.1[天文地球—水文科学]