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GES 101 Handout: Groundwater
Amount and movement of groundwater governed by porosity and permeability of host.
Water Table: surface separating zones of aeration and saturation
-subdued replica of topography
-perched water table
-depth of water table: balance between recharge and discharge
Aquifer vs aquiclude
Movement of groundwater governed by
-Darcy's Law: Velocity = K(hydraulic head/distance)
-movement is very slow (= 45 feet per year)
Cone of Depression
Artesian Water System: water under pressure rises above level of aquifer
-artesian pressure surface
Groundwater "erosion": Dissolution occurs in the zone of saturation and produces caves, caverns and sinkholes
- Karst topography
Groundwater Deposition
Stalactites
Dripstone: stalagmites
Columns
Hot springs and Geysers
Groundwater Resources
- groundwater use is significant and expanding
-difficult to manage
Water law and Water Policy
East - Riparian rights
West - Prior Appropriation
Groundwater Problems
I) "Mining" of finite resource
Ex: Ogallala aquifer - High Plains -underlies - 174,000 mi2 -irrigates - 25,000 mi2 of farmland
II) Preservation of Water Quality
a) "Point" sources of pollution
-septic tanks
-municipal treatment plants
-feed lots
-landfills and dumps
-mine dumps
-industrial waste impoundments
-round salt piles
-buried fuel tanks
b) Non-point Sources
-suburban "grassed" areas
-agricultural land
-road salting
-urban "spills" (oil, gas, etc.)
Review Questions Groundwater
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