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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. Water table - Wikipedia

    en.wikipedia.org/wiki/Water_table

    In the aquifer, groundwater flows from points of higher pressure to points of lower pressure, and the direction of groundwater flow typically has both a horizontal and a vertical component. The slope of the water table is known as the “hydraulic gradient”, which depends on the rate at which water is added to and removed from the aquifer and ...

  4. Check dam - Wikipedia

    en.wikipedia.org/wiki/Check_dam

    In arid areas, check dams are often built to increase groundwater recharge in a process called managed aquifer recharge. Winter runoff thus can be stored in aquifers, from which the water can be withdrawn during the dry season for irrigation, livestock watering, and drinking water.

  5. 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.

  6. Vadose zone - Wikipedia

    en.wikipedia.org/wiki/Vadose_zone

    Water in the vadose zone has a pressure head less than atmospheric pressure, and is retained by a combination of adhesion (funiculary groundwater), and capillary action (capillary groundwater). If the vadose zone envelops soil, the water contained therein is termed soil moisture. In fine grained soils, capillary action can cause the pores of ...

  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. Aquifer test - Wikipedia

    en.wikipedia.org/wiki/Aquifer_test

    VINMOD Multi-Well – Groundwater pollution analysis using pumping tests and pollution parameters from pumped groundwater; Hytool - Open source toolbox for pumping and build up tests interpretation on Matlab; SmartGEO - advanced commercial software for heterogeneous aquifers characterization, hydraulic tomography and multiple pumping tests

  9. Runoff (hydrology) - Wikipedia

    en.wikipedia.org/wiki/Runoff_(hydrology)

    This causes lowering of the water table (because groundwater recharge is lessened) and flooding since the amount of water that remains on the surface is greater. [11] [12] Most municipal storm sewer systems discharge untreated stormwater to streams, rivers, and bays. This excess water can also make its way into people's properties through ...