The Age of Shallow Groundwater in Henan Plain
详细信息
- 责任者：Shi Xufei (College of Environment and Resources ; Jilin University ; Changchun 130026 ; China) ; Dong Weihong
- 刊名：Journal of Jilin University
- 出版年：2012
- 卷期：42(1)
- 关键词：浅层含水层 ; shallow aquifers ; 河南 ; Henan Province
- 页码：p.190-197
- 图表：5 illus., 4 tables, 16 refs.
- 分类号：1701
- 出版序号：20130510
- issnNo：ISSN1671-5888
- isbnNo：CN22-1343/P
摘要
The 3H method and CFCs method were applied to date the Quaternary shallow groundwater in order to study the groundwater cycle and renewability evaluation of shallow groundwater in Henan Plain. It can be concluded that the fitting error was small (2 a) so that the ages calculation by the two methods can represent the shallow groundwater ages in Henan Plain.In general,the shallow groundwater was the modern recharged water which was younger than 50 a. The groundwater age was younger than 30 a in the piedmonts of Taihang Mountains, Funiu Mountains, Dabie Mountains and along two sides of the Yellow River on west of Kaifeng. The age increased along with the groundwater flow path. The exploration potential decreased from the piedmonts and the two sides of the Yellow River to the plain. In general, the groundwater cycle was faster in the northern groundwater system of which age was younger, followed by that in the southern groundwater system. The groundwater cycle was the slowest in central groundwater system of which age was the oldest.