导图社区 Groundwater
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Groundwater
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Para 1 lead in
information about groundwater
stored in pores and fractures in rocks
50 times as much water under ground than above ground
the deeper, the less water rocks can occupy
Para 2 Aquifers, Porosity and Permeability
Aquifers A groundwater reservoir from which water can be extracted
Porosity
pore space between sediment grains that can be filled with water
expressed as a percentage of the total rock volume
Permeability
the ability of water to flow through the interconnected pore spaces
Para 3 Sediment sorting
poorly sorted& tightly compacted→low porosity and permeability
sedimentary rocks
contain the most space→most connom reservoirs
sandstones
good aquifers
finer-grained mudstones
impermeable
Igneous and metamorphic
more compact, no space between
may become groundwater reservoirs if extensive fracturing occurs and the fracture system is interconnected
Para 4&5: water table
the underground boundary below which all the cracks and pores are filled with water
reach the Earth's surface→rivers, lakes and marshes
usually follows the contours of the topography
vadose zone
above the water table
where rainwater percolates
supplies plant roots near the surface with water