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Published byCecilia Lee Modified over 9 years ago
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Groundwater
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Porosity & Permeability Porosity: - the percentage of the total volume of a rock consisting of voids. - pore spaces: spaces between mineral gains, fractures, solution cavities, vesicles - for example: vesicles & fractures in a basalt = 30-40% solution cavities in limestone = 30% spaces between grains in cemented sandstone = 5% spaces between grains in conglomerate = 20% fractures in granite = <1% Permeability: - the capacity of a rock to transmit fluids - depends on the size of the voids, and whether the voids are interconnected. - a rock can have high porosity but low permeability if the voids are not connected so as to allow water to flow. - velocity of gw averages 1 m/day to 1 m/year.
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Water Table
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Flow Groundwater flows downhill and into areas of low pressure. Stream beds are areas of low pressure: Natural springs.
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Effluent and Influent Water table drops below level of stream bottom Water table is at or above level of stream bottom.
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Spring
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Spring Pic
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Well Picture Groundwater Well: An artificial area of low pressure
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Wells
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Cone of Depression
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Contaminated Wells
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Vermillion GW flows N to S Town wells Wastewater treatment plant
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Ogallala Ogallala Formation: A trillion gallons of water put in the ground by melting glaciers 10K years ago. This water is used for irrigation in the midwest.
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Center Pivot 128 Acres
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Center Pivot II
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Circles
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Garden City, Kansas
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San Joaquin Valley
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Subsidence
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Artesian Water Pressurized groundwater rises from an aquifer
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Blow Out
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Water Tower
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Water Reservoir Table Rock Reservoir, South Carolina
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New York Drought 52% decrease in capacity in two years One reservoir in the Catskill Mountains
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Lake Mead
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Wastewater Treatment
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Karst Topography
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Karst I Limestone Bedrock Acidic groundwater slowly dissolves bedrock
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Karst II
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Small Sink
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Medium Sink
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Large Sink
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Stalactite Water percolating through the ground leaves behind calcite (CaCO 3 ) deposits.
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Cave Stalactite Stalagmite Column
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Cave II
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Geysers & Hot Springs
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Geyser Formation Groundwater percolates downward; as it approaches magma at depth, it heats up. When it flashes into steam, the steam rushes back up to the surface forming a geyser. Then the process repeats. Sometime this process repeats at a regular interval, sometimes not.
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Old Faithful
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Colorado River Delta River ends here Only 10% of river water makes it into Mexico
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Aral Sea Reduced in size by 60% in 30 years Commercial fishing eliminated
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Lake Chad
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1/20th of its size 20 yrs ago!
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