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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. Vadose zone - Wikipedia

    en.wikipedia.org/wiki/Vadose_zone

    The vadose zone, also termed the unsaturated zone, is the part of Earth between the land surface and the top of the phreatic zone, the position at which the groundwater (the water in the soil's pores) is at atmospheric pressure ("vadose" is from the Latin word for "shallow").

  4. Groundwater - Wikipedia

    en.wikipedia.org/wiki/Groundwater

    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.

  5. Water table - Wikipedia

    en.wikipedia.org/wiki/Water_table

    The groundwater may be from precipitation or from groundwater flowing into the aquifer. In areas with sufficient precipitation, water infiltrates through pore spaces in the soil, passing through the unsaturated zone. At increasing depths, water fills in more of the pore spaces in the soils, until a zone of saturation is reached.

  6. Aquifer - Wikipedia

    en.wikipedia.org/wiki/Aquifer

    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 ...

  7. 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]

  8. Today’s NYT ‘Strands’ Hints, Spangram and Answers for ...

    www.aol.com/today-nyt-strands-hints-spangram...

    According to the New York Times, here's exactly how to play Strands: Find theme words to fill the board. Theme words stay highlighted in blue when found.

  9. 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 ...