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groundwater flow

   Also found in: Wikipedia 0.01 sec.
groundwater flow [′grau̇nd‚wȯd·ər ‚flō]
(hydrology)
That portion of the precipitation that has been absorbed by the ground and has become part of the groundwater.


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Groundwater flow, drawn by irrigation pumping, transports that pond water to the depth where dissolved arsenic concentrations are greatest and where it is then pumped up into the irrigation and drinking wells," Nature quoted Harvey as saying.
The groundwater flow inside the rocks resulted in connected long, wide and vertical spaces and runnels because of dissolution by water which deprives them from CO2 participating in the desolation and erosion of limestone and enlarging the cavern .
The direction of groundwater flow has also been changed in that region; natural groundwater flowed from the Pandivere upland to Lake Peipsi.
 
 
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