高寒地区傍河型地下水水源地论证  

Demonstration on Riverside Groundwater Resource Field in Frigid Area

作　　者：高淑琴[1] 戴长雷[2] 邓国立[3] 

机构地区：[1]吉林大学环境与资源学院/吉林大学水资源与环境研究所 [2]黑龙江大学水利电力学院 [3]黑龙江省水利水电勘测设计研究院,黑龙江哈尔滨150080

出　　处：《水文》2008年第2期30-33,共4页Journal of China Hydrology

基　　金：黑龙江大学青年科学基金(QT01);黑龙江省水利厅项目(HSKY2005-16);黑龙江省教育厅科技项目(11511298);国土资源部水资源与水环境问题重点实验室的联合资助

摘　　要：地下水水源地论证是新建和扩建地下水水源地的前提,高寒地区傍河型地下水水源地论证在关注地下水质量和允许开采量的同时,非常注重水源地含水层开采对水环境及其它用水户的影响。本文以黑龙江省孙吴县热电厂供水水源地为例,从论证目标、约束条件和论证方法等方面对高寒地区傍河型地下水水源地进行了论证。结果表明,高寒地区傍河型浅薄含水层地下水水源地的补给来源在冬季主要为含水层侧向径流补给;孙吴县热电厂供水水源地可以满足热电厂正常运转对水质和水量的要求,并且不会对区域水资源和其它用水户产生影响。The demonstration on the groundwater resource field is the precondition for construction or extension of this kind field. The demonstration on the groundwater resource field along river in frigid area focuses not only on quality and available yields of groundwater, but also on affection of exploitation on water resource environment and other users. This paper demonstrated the riverside groundwater resource field in frigid area, taking example for water supply field of thermoelectricity company in Sunwu County. The results indicate that the main recharge resource of riverside groundwater resource field in frigid area in winter is sidely runoff of aquifer. The water supply field of thermoelectricity company in Sunwu County can satisfy the need of water quantity and quality, and will not effect regional water resource and other users.

关 键 词：高寒地区 浅薄含水层 傍河型地下水水源地 

分 类 号：P641.8[天文地球—地质矿产勘探]