西辽河平原区地下水水位动态与水资源可持续发展  

Groundwater level trend and sustainable development of water resources in West Liaohe River Plain

作　　者：陈志云[1,2] 林岚[2] 王晓昕[2] 

机构地区：[1]吉林大学环境与资源学院,吉林长春130012 [2]松辽水利委员会流域规划与政策研究中心,吉林长春130021

出　　处：《水利经济》2012年第2期57-59,76,共3页Journal of Economics of Water Resources

摘　　要：根据西辽河平原区地下水位动态及气象、水文等资料,分析了地下水水位动态,确定了该区的地下水位动态类型:人工开采型,降水入渗开采型,降水入渗型,降水入渗蒸发型,径流型,降水入渗径流型。结果表明,西辽河平原区地下水动态主要影响因素为气象因素及人为因素,地下水的大量开采对该区水资源可持续利用产生了极大的影响。The groundwater water trend in West Liaohe River Plain is analyzed according to its groundwater level state and meteorological and hydrological data. The groundwater in this area is divided into six types： manual extraction, rainfall infiltration extraction, rainfall infiltration, rainfall infiltration evaporation, runoff and rainfall infiltration runoff. The results show that the main factors for the groundwater level trend in West Liaohe River Plain are meteorological and artificial ones. The large extraction of groundwater in the area has great influences on its water resources.

关 键 词：地下水资源 水位动态 动态特征 西辽河平原 

分 类 号：TV211.1[水利工程—水文学及水资源]