地质与资源2009，Vol.18Issue(2)：140-143,4.
下辽河平原地下水多年动态变化特征分析
ANALYSIS ON THE MULTI-YEAR VARIATIONS OF GROUNDWATER IN LOWER LIAOHE PLAIN
李凯 1卞玉梅 1杨静 1张懿 2赵英3
作者信息
- 1. 辽宁省地质环境监测总站,辽宁,沈阳,110032
- 2. 辽宁省地质矿产研究院,辽宁,沈阳,110032
- 3. 辽宁省地质矿产局第三地质大队,辽宁,朝阳,122000
- 折叠
摘要
Abstract
The dynamic variation of groundwater level is actually a reflection of the change of groundwater resources in aquifer. The fluctuation of groundwater level directly reflects the variation in amounts of consumption and recharge of groundwater. Based on the monitoring data of groundwater level, the variation characters of phreatic water in Lower Liaohe Plain from 1996 to 2005 are analyzed. It is concluded that whether phreatic water or confined water, the groundwater levels change along with precipitation in non-exploitation area and dry farmland area. Besides the contribution of precipitation, the exploitation scale and layout of groundwater in exploitation area are also significant influential factors for the variation characters of groundwater level.关键词
下辽河平原/地下水动态变化/孔隙潜水/承压水Key words
Lower Liaohe Plain/dynamic variation of groundwater/phreatic water/confined water分类
天文与地球科学引用本文复制引用
李凯,卞玉梅,杨静,张懿,赵英..下辽河平原地下水多年动态变化特征分析[J].地质与资源,2009,18(2):140-143,4.
