摘要
以阿克苏地区水文地质普查报告和温宿县地下水资源开发利用规划等相关资料及实地调查、测量等工作取得的原始资料为基础，说明了研究区的水文地质条件，确定计算研究区的地下水水量均衡方程和计算参数，利用搜集到相关数据进行地下水水量均衡计算，计算结果表明：该区地下水补给量略大于排泄量，主要的补给源为河流渠系的入渗和山前侧向人渗；主要排泄量为向下游的排泄量和潜入蒸发量。
This paper is written base on the hydro-geological survey report in the Akesu area and the exploitation and utilization planning of water resources of Wensu county and on-the-spot investigation and measurement, records of the original data. The paper introduces the hydrological, and geological conditions of groundwater, confirms water balance equation and the calculated parameters. Using the data collected, the final calculating results are analyzed. Through water balance calculation, we can understand the relations between the groundwater recharge and discharge,and the main supply source and discharge flows to.
出处
《南水北调与水利科技》
CAS
CSCD
北大核心
2012年第A01期57-59,共3页
South-to-North Water Transfers and Water Science & Technology
关键词
温宿县
地下水
水量均衡计算
Wensu county
groundwater
water-balance calculation
