Ground-Water Pumpage and Artificial Recharge Estimates for Calendar Year 2000 and Average Annual Nat-2025

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Groundwater recharge is defined as the downward movement of water from the unsaturated (vadose) zone of soil or rock and into the groundwater saturated (phreatic) zone (Fetter, 2001).
The equation is R = K (P X), where K is a constant and P is the annual precipitation in mm. For locations with P between 400 and 600 mm, R = 0.20 (P 400). For locations with P between 600 and 1,000 mm, R = 0.25 (P 400).
In coastal areas, intentional recharge prevents salty ocean water from entering freshwater aquifers. Recharge can also help prevent impacts from groundwater pumping, such as dry wells or sinking lands, while providing wetland habitat for birds, reducing flood risk, and storing water for droughts.
Groundwater recharge or the rate at which aquifers are replenished is one of the most difficult components of the water budget to quantify. Recharge rates are impacted by the amount and intensity of precipitation, soil and vegetation types, geology and topography. Recharge rates are highly variable in space and time.
Recharge Definition: A recharge rate is a charge for goods/services provided by your unit to other internal users of that service. The focus is on direct costs when establishing rates, with the intention for the activity to break even. Rates need to be consistently applied to internal users.
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