滨海潜水含水层是滨海地区开采淡水的重要目的层。
Unconfind aquifers are important for supplying of fresh water in coastal area.
但由滨海潜水含水层的性质所决定，它极易因抽水过量而遭受海水入侵。
Determined by its character, it is very easy to cause sea water intrusion to the layer by over extraction of fresh water.
揭示了沟谷潜水含水层内水资源存贮规律，为合理开发利用沟谷潜水水资源提供了可靠依据。
Storage low of water resources in aquifer of clench and sloping land for provide scientific basis of developing phreatic water resources in clench and sloping land.
减小井间距，增加上层滞水和潜水的入流通道，尤其要在潜水含水层底板低洼处设置降水井将低洼处的残留水引走。
Minish the well space and increase transflux routeways upper backwater and driving, especially setup precipitation well and drain residual water at the bottom of diving layer.
含水层有三种形态，分别是上层滞水、潜水和承压水。
There are three types of aquifers: perched, unconfined, and confined.
对于许多区域水资源问题，用数值方法进行潜水水流模拟时，需要给出每个节点上含水层底板标高值。
In many cases of regional water resources issues, when numerical method is often adopted in groundwater flow modeling lower bed level value of aquifer on each node should be given.
对于许多区域水资源问题，用数值方法进行潜水水流模拟时，需要给出每个节点上含水层底板标高值。
In many cases of regional water resources issues, when numerical method is often adopted in groundwater flow modeling lower bed level value of aquifer on each node should be given.
应用推荐