摘要
通过对宿州市市区水源地的水文地质条件分析,认为为了满足城市供水需求,一方面新生界松散层水源地应向周家、陈营孜、杨庙、小武家、直至大吴家一带发展;另一方面必须开发宿州市市区北部符篱集一带寒武系石灰岩为新的水源地,以满足宿州市城市发展的需求。
By analyzing the hydrogeological condition of city water supply source for Suzhou City, it is supposed that water contained in Cenozoic loose bed may developed in such areas as Zhoujia, Chengyingzi, Xiaowu-jia and Dawujia, and water contained in Cambrain lime stone are another source for city water supply.
出处
《甘肃地质》
2009年第3期72-75,共4页
Gansu Geology
关键词
水源地
石灰岩
城市发展
宿州市
source of city water supply
lime stone
city development
Suzhou city
