摘要
在分析龙子祠泉域多年降水量、泉流量及人工岩溶水开采量等资料的基础上,对龙子祠泉流量动态特征及衰减原因进行了研究。结果表明,龙子祠泉流量呈整体下降趋势,泉流量的衰减主要受降水量的减少和人类开采量的增大及泉域内采煤排水三方面共同影响。
Based on the analysis on the data of many years such as the average annual precipitation,spring flow rate,and artificial withdrawal of Karst water,etc.,this paper analyzes the dynamic characteristics and the attenuation causes of the flow rate of Longzici Spring.The results show that the flow rate of the spring is in drop tendency overall,and the attenuation of the flow rate of the spring is influenced mainly by three aspects of the decrease of precipitation,the increase of artificial withdrawal and the drainage of coal mining.
出处
《科技情报开发与经济》
2010年第25期137-139,共3页
Sci-Tech Information Development & Economy
关键词
龙子祠泉
泉流量
动态特征
衰减
岩溶水
Longzici Spring
flow rate of spring
dynamic characteristics
attenuation
Karst water
作者简介
王红全，男，1970年生，1993年毕业于太原理工大学水利系，工程师，临汾市汾西水利管理局，山西省临汾市．041000．
