水文地质工程地质2011，Vol.38Issue(4)：32-37,6.
乌东德水电站坝址区SO2-4成因与分布特征分析
An analysis of the source and distribution of SO(2-)4 in dam site area of the Wudongde Hydroelectric Station on Jinshajiang River
骆祖江 1张弘 1李会中 2王团乐2
作者信息
- 1. 河海大学水文地质研究所,南京,210098
- 2. 长江三峡勘测研究院有限公司,武汉,430010
- 折叠
摘要
Abstract
Difference in SO2- 4 contents exists in groundwater in two banks of the Wudongde Hydro- electric Station. In particular, the SO2- 4 contents in left side is generally higher than those in the right side. Combined with the study of water-rock interaction, hydrochemical data, temperature and hydrodynamic data, the characteristics of rock and mineral and hydrochemistry were analyzed. The cluster analysis was used to search the relativity of SO2- 4 and other ions. It is found ultimately that the source of SO2- 4 is related to the pyrite occurring in the formations. The difference in SO2- 4 contents in the two sides is mainly due to the different in groundwater circulation.关键词
乌东德/聚类分析/水化学场/水温场/水动力场Key words
Wudongde/ cluster analysis/ hydrochemistry field/ temperature field/ hydrodynamic field分类
天文与地球科学引用本文复制引用
骆祖江,张弘,李会中,王团乐..乌东德水电站坝址区SO2-4成因与分布特征分析[J].水文地质工程地质,2011,38(4):32-37,6.
