基于康平县地下水可动用储量计算方法探讨

摘要

地下水动态是指在有关因素影响下，地下水的水位、水量、水化学成分、水温等随时间的变化状况。地下水动态提供含水层或含水系统的系列信息。在验证所作出的水文地质结论或所采取的水文地质措施是否正确时，地下水动态是十分重要的。地下水动态受气候、水文、地质和人类活动等因素的影响，受气候、水文、地质等因素影响的，称“天然因素影响的地下水动态”，受人类活动影响的称“人类活动影响下的地下水动态”。文中运用水均衡分析对该地区的地下水可动用储量计算的方法进行了探讨。%Groundwater regime refers to the changes in groundwater level,quantity,water,chemical composition,water temperature etc.,with time influenced by relevant factors.Groundwater dynamic provides series information of aquifer or aqueous system.It is very important to verify if hydrogeological measures taken or hydrogeological conclusions made by hydrogeologist correct.Climate,hydrological, geological factors and human activities etc.,all have impact on groundwater,in which climate, hydrology,geology and other factors are called “groundwater regime influenced by natural factors”,the groundwater regime affected by human activities is called “groundwater regime influenced by human activities”.Groundwater reserves are calculated by using water balance analysis method in this area.