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  2. Groundwater recharge - Wikipedia

    en.wikipedia.org/wiki/Groundwater_recharge

    Groundwater recharge or deep drainage or deep percolation is a hydrologic process, where water moves downward from surface water to groundwater. Recharge is the primary method through which water enters an aquifer. This process usually occurs in the vadose zone below plant roots and is often expressed as a flux to the water table surface.

  3. Groundwater recharge in California - Wikipedia

    en.wikipedia.org/wiki/Groundwater_Recharge_in...

    Groundwater recharge projects are expected to increase in number in future years throughout California due to the comparatively low cost and massive storage capabilities of aquifers. The total volume of groundwater capacity is estimated to be 850 million acre-feet, while there is only around 50 million acre-feet of available surface freshwater ...

  4. Groundwater - Wikipedia

    en.wikipedia.org/wiki/Groundwater

    This is an accepted version of this page This is the latest accepted revision, reviewed on 31 October 2024. Water located beneath the ground surface An illustration showing groundwater in aquifers (in blue) (1, 5 and 6) below the water table (4), and three different wells (7, 8 and 9) dug to reach it. Groundwater is the water present beneath Earth's surface in rock and soil pore spaces and in ...

  5. Groundwater banking - Wikipedia

    en.wikipedia.org/wiki/Groundwater_banking

    Direct recharge is storing water by allowing it to percolate directly to storage in the groundwater basin. [1] With direct recharge it floods an area so that water seeps through the ground to get to the aquifers. [3] The water is then pumped out when there is more of a demand with the use of recovery wells. [3]

  6. Coastal hydrogeology - Wikipedia

    en.wikipedia.org/wiki/Coastal_hydrogeology

    Precipitation and infiltration recharge the groundwater with an island. If rainfall recharge of an island aquifer is significant, the seepage zone might form and shift the interface towards the sea. Ghijben – Herzberg Principle can be used to estimate the depth of groundwater. [16] Confined Continental Coastal Aquifer

  7. Aquifer storage and recovery - Wikipedia

    en.wikipedia.org/wiki/Aquifer_storage_and_recovery

    The first agriculture ASR wells were put into service in Oregon in the autumn of 2006 and have injected well over 3,000 acre-feet (3,700,000 m 3) of water during the winter and spring flood flow times using artificial recharge (AR) of flood water as their water source. This shallow recharged water is then recovered as potable water and injected ...

  8. Recharge - Wikipedia

    en.wikipedia.org/wiki/Recharge

    Recharge or Recharged may refer to: Groundwater recharge, a hydrologic process where water moves to groundwater; Recharge (battery), the process to restore power or charge to a power storage device, such as a battery; Recharge, is a business news website and monthly magazine covering the global renewable energy industry

  9. Water reuse in California - Wikipedia

    en.wikipedia.org/wiki/Water_reuse_in_California

    Montebello Forebay Ground Water Recharge Project in Los Angeles, California. Water reuse in California is the use of reclaimed water for beneficial use. As a heavily populated state in the drought-prone arid west, water reuse is developing as an integral part of water in California enabling both the economy and population to grow.