The water table is the underground boundary below which all the cracks and pores are filled with water.
地下水位是地层岩石裂缝和孔隙充满水的边界。
Above the water table is the vadose zone, through which rainwater percolates.
地下水位的上方是包气带,雨水从中渗透。
Water in the vadose zone drains down to the water table, leaving behind a thin coating of water on mineral grains.
包气带中的水会沉降到地下水位,只在矿物颗粒表面留下一层薄薄的水膜。
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