Geology 140 - Environmental Geology
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Groundwater Notes
water table: surface of groundwater, top of saturated zone underground
Groundwater flow tends to mimic shape of the land -
It flows away from pressure, and so usually downhill (
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porosity: volume of empty space in a rock
permeability: ability of rock to transmit fluids
aquifer: water-bearing rock
water is in rock like water in a sponge - in the holes
Pumping groundwater can change direction of groundwater flow
Pumped well lowers water table at the well
can cause contamination of wells
near coast, can cause saltwater to flow into wells (
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groundwater overdrafting (using water faster than it enters the aquifer):
using groundwater faster than it returns to the ground (recharges)
Can contaminate wells, salt-water intrusion
Impacting flow in surrounding rivers
Depletion of water resources
Land subsidence (
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