When water reaches the saturated zone beneath the water table, it oozes slowly downward, and laterally.
当水到达潜水面以下的饱和带时，它就缓慢地向下和侧向渗透。
The non-porous layer holds the water in an area called the saturated zone.
不渗透层将水蓄积在一个叫做“饱和层”的地方。
The upper level of water in the saturated zone is called the water table.
饱和层里的上水平线叫做地下水位。
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