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ES 9.2 Groundwater

TermDefinition
Groundwater 0.30% of all water
Porosity amount of pore spaces
Water Table upper boundary
Zone of Aeration Air in pores, above water table
Permeability ability of material to let water pass
Aquifers permeable sediments with large pores
Aquicludes barriers to groundwater flow, silt, clay, shale, clay-lined ponds+landfills
Hot Springs >37 degrees C, near igneous activity and deep aquifers
Geyser explosive hot spring
Carbonic Acid makes groundwater slightly acidic
Hard Water high amounts of Ca, Mg, Fe; can clog pipes
Wells holes in ground to reach an aquifer
Ordinary Well reaches below water table
Artesian Well drilled into aquifer under pressure, water spurts like fountain
Calcite dissolved by acid water in limestone
Stalactites formed by calcite precipitation
Cone of Depression What happens when there is overpumping in an aquifer
Recharge Aquifer needs to recharge using precipitation
Threats to Water Supply overuse, pollution, chemicals, salt, radon
Springs natural discharge of groundwater
Created by: ejs_21
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