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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. Category:Aquifers - Wikipedia

    en.wikipedia.org/wiki/Category:Aquifers

    Aquifers and Groundwater Aquifer types and locations - and Groundwater hydrology and hydrogeology ; pollution and remediation ; and conservation management and recharge . Wikimedia Commons has media related to Aquifers .

  6. 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]

  7. Principal aquifers of California - Wikipedia

    en.wikipedia.org/wiki/Principal_aquifers_of...

    The California Department of Water Resources has detailed descriptions (online in PDF format, etc.) of each of the 515 state-recognized groundwater basins. [ 2 ] The principal aquifers of the United States are organized by national principal aquifer codes and names assigned by the National Water Information System (NWIS) of the United States ...

  8. 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 ...

  9. Leaky Acres Recharge Facility - Wikipedia

    en.wikipedia.org/wiki/Leaky_Acres_Recharge_Facility

    The Leaky Acres Recharge Facility is a groundwater recharge facility located in Fresno, California. The facility began as a joint research project by the City of Fresno water division and the US Department of Agriculture. It first began percolating water in 1971 and was subsequently expanded and duplicated in other areas of the city.