unconfined aquifer

基本解釋

One of the two main types of aquifer is the unconfined aquifer.
非承壓含水層是兩種主要含水層之一。
The water table of the unconfined aquifer near the coast fluctuates following the tide movement, the aquifer also exchanges water with the sea.
近岸含水層水位隨潮水的波動而波動，同時(shí)還與海水之間發(fā)生著水量交換。
While groundwater flows through an unconfined aquifer due to heterogeneity, the vertical average saturated hydraulic conductivity is a function of hydraulic head.
地下水流於非拘限含水層流動時(shí)，因含水層之非均質(zhì)性，使得垂直平均之飽和水力傳導(dǎo)系數(shù)隨地下水水位高低而變化。