Põhjaveekihi paksus on kõige lihtsamalt mõistetav kui põhjaveekihi ja selle aluskihi vaheline kaugus, mis suureneb ja väheneb vastusena kõikuvale sademete mahule.
Saturated thickness of the groundwater resource – defined in simplest terms as the distance between the water table and the base of the aquifer – will increase and decrease in response to the fluctuating water table.
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