Formation of High-Fluorine Water of Yangshapao Reservoir in Western Jilin Province
详细信息
- 责任者：Liang Xiujuan (Key Laboratory of Groundwater Resources and Environment ; Ministry of Education ; Jilin University ; Changchun 130021 ; China) ; Xiao Ran
- 刊名：Journal of Jilin University
- 出版年：2012
- 卷期：42(3)
- 关键词：水库 ; reservoirs ; 高氟水 ; high-fluorine water ; 吉林 ; Jilin Province
- 页码：p.798-804
- 图表：3 illus., 6 tables, 13 refs.
- 分类号：1800
- issnNo：ISSN1671-5888
- isbnNo：CN22-1343/P
摘要
The genesis of the high-fluorien water in Yangshapao reservoir was studied on the basis of investigation and analysis of the surrounding geological condition,hydrogeological condition and the characteristics of soil and fluorine as well as the simulating experimental results for Yangshapao reservoir.The results showed that the formation of the high-fluorine area in Yangshapao reservoir is the results of long-term evolution of the surface environment.The magmatic rocks in the Daxing’anling mountain and unconsolidated deposits in Songnen low plain provide abundant fluorine-rich matter.The river and groundwater provides dynamic condition for fluorine transportation.The typical low-lying topology becomes the geographic condition for high-fluorine formation.The dry and semi-dry climatic condition is the promotion condition for the high-fluorine environment.The fluorine in Yanshapao reservoir mainly comes from the runoff of Erlongtao river,which brings about 99% of the total fluorine annually into the reservoir.The fluorine from the surrounding runoff is 0.014%-0.28% annually.The fluorine from the rainout is 0.012%.The evaporation-concentration process can increase the concentration of fluorine in water.The release of fluorine from the bottom mud is one cause of the increase of fluorine concentration in Yangshapao reservoir,which will have some impacts on the water quality of the reservoir after the Water diversion project from Nenjiang river to Baicheng city brings into practice.It will take about 5 years for the fluorine concentration of the water body in the reservoir decreasing below 1.0 mg/L under conditions of annual water diversion.Otherwise,the strong wind and human activities also have impacts on the fluorine in Yangshapao reservoir.
© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号 地址：北京市海淀区学院路29号 邮编：100083 电话：办公室：(+86 10)66554848；文献借阅、咨询服务、科技查新：66554700 |