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  2. Groundwater recharge - Wikipedia

    en.wikipedia.org/wiki/Groundwater_recharge

    Groundwater recharge also encompasses water moving away from the water table farther into the saturated zone. [1] Recharge occurs both naturally (through the water cycle) and through anthropogenic processes (i.e., "artificial groundwater recharge"), where rainwater and/or reclaimed water is routed to the subsurface.

  3. Water table - Wikipedia

    en.wikipedia.org/wiki/Water_table

    The water table is the upper surface of the phreatic zone or zone of saturation. The zone of saturation is where the pores and fractures of the ground are saturated with groundwater, [1] which may be fresh, saline, or brackish, depending on the locality. It can also be simply explained as the depth below which the ground is saturated.

  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. 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.

  6. Groundwater banking - Wikipedia

    en.wikipedia.org/wiki/Groundwater_banking

    Groundwater banking and aquifer storage systems are being explored to control flooding during times of high precipitation. [7] The groundwater is being traded in many regions. There are trades even in the United States. The city of San Antonio, Texas is the largest city in the United States that relies solely on groundwater for its municipal ...

  7. Overdrafting - Wikipedia

    en.wikipedia.org/wiki/Overdrafting

    When groundwater is extracted from an aquifer, a cone of depression is created around the well.As the drafting of water continues, the cone increases in radius. Extracting too much water (overdrafting) can lead to negative impacts such as a drop of the water table, land subsidence, and loss of surface water reaching the streams.

  8. Category:Illinois city council members - Wikipedia

    en.wikipedia.org/wiki/Category:Illinois_city...

    Peoria, Illinois City Council members (9 P) Pages in category "Illinois city council members" The following 125 pages are in this category, out of 125 total.

  9. Spreading ground - Wikipedia

    en.wikipedia.org/wiki/Spreading_ground

    When natural percolation of precipitation is insufficient to replenish groundwater withdrawn for human use, artificial recharge helps prevent aquifer depletion, subsidence and saltwater intrusion. Spreading grounds are one of several available technologies, and are useful to harness storm water runoff in populated areas with low annual ...