recharge area
Any area of land allowing water to pass through it and into an aquifer. See aquifer, natural recharge.
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Any area of land allowing water to pass through it and into an aquifer. See aquifer, natural recharge.
Legal principle by which the first user of water from a stream establishes a legal right to continued use of the amount originally withdrawn. Compare riparian rights.
Percentage of space in rock or soil occupied by voids, whether the voids are isolated or connected. Compare permeability.
Degree to which underground rock and soil pores are interconnected and thus a measure of the degree to which water can flow freely from one pore to another. Compare porosity.
Natural replenishment of an aquifer by precipitation, which percolates downward through soil and rock. See recharge area.
Biogeochemical cycle that collects, purifies, and distributes the earth's fixed supply of water from the environment to living organisms and then back to the environment.
Water that sinks into the soil and is stored in slowly flowing and slowly renewed underground reservoirs called aquifers; underground water in the zone of saturation, below the water table. Compare runoff, surface water.
Flat valley floor next to a stream channel. For legal purposes, the term often applies to any low area that has the potential for flooding, including certain coastal areas.
Condition in which an area does not get enough water because of (1) lower-than normal precipitation or (2) higher-than-normal temperatures that increase evaporation.
See watershed.
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