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  2. U.S. Bank Stadium - Wikipedia

    en.wikipedia.org/wiki/U.S._Bank_Stadium

    U.S. Bank Stadium is an enclosed stadium located in downtown Minneapolis, Minnesota. Built on the former site of the Hubert H. Humphrey Metrodome , the indoor stadium opened in 2016 and is the home of the Minnesota Vikings of the National Football League (NFL); it also hosts early season college baseball games of the University of Minnesota ...

  3. Field capacity - Wikipedia

    en.wikipedia.org/wiki/Field_capacity

    Field capacity. Field capacity is the amount of soil moisture or water content held in the soil after excess water has drained away and the rate of downward movement has decreased. This usually takes place 2–3 days after rain or irrigation in pervious soils of uniform structure and texture. The physical definition of field capacity (expressed ...

  4. 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.

  5. Taum Sauk Hydroelectric Power Station - Wikipedia

    en.wikipedia.org/wiki/Taum_Sauk_Hydroelectric...

    The Taum Sauk pumped storage plant is a power station in the St. Francois mountain region of Missouri, United States about 90 miles (140 km) south of St. Louis near Lesterville, Missouri, in Reynolds County. It is operated by Ameren Missouri . The pumped-storage hydroelectric plant was constructed from 1960–1962 and was designed to help meet ...

  6. Soil water (retention) - Wikipedia

    en.wikipedia.org/wiki/Soil_water_(retention)

    Available water is that which the plants can utilize from the soil within the range between field capacity and wilting point. Roughly speaking for agriculture (top layer soil), soil is 25% water , 25% air , 45% mineral , 5% other; water varies widely from about 1% to 90% due to several retention and drainage properties of a given soil.

  7. Non-revenue water - Wikipedia

    en.wikipedia.org/wiki/Non-revenue_water

    The American Water Works Association (AWWA) has developed Water Audit Software which allows utilities to rate the overall degree of validity of their water audit data. Guidance on loss control planning is given based upon the credibility of the data and the measure of losses displayed by the water audit.

  8. Groundwater banking - Wikipedia

    en.wikipedia.org/wiki/Groundwater_banking

    Groundwater banking is a water management mechanism designed to increase water supply reliability. [1] Groundwater can be created by using dewatered aquifer space to store water during the years when there is abundant rainfall. It can then be pumped and used during years that do not have a surplus of water. [1]

  9. Moisture equivalent - Wikipedia

    en.wikipedia.org/wiki/Moisture_equivalent

    Moisture equivalent is proposed by Lyman Briggs and McLane (1910) as a measure of field capacity for fine-textured soil materials. Moisture equivalent is defined as the percentage of water which a soil can retain in opposition to a centrifugal force 1000 times that of gravity. It is measured by saturating sample of soil 1 cm thick, and ...