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  2. Potentiometric surface - Wikipedia

    en.wikipedia.org/wiki/Potentiometric_surface

    For groundwater "potentiometric surface" is a synonym of "piezometric surface" which is an imaginary surface that defines the level to which water in a confined aquifer would rise were it completely pierced with wells. [1] If the potentiometric surface lies above the ground surface, a flowing artesian well results.

  3. Drawdown (hydrology) - Wikipedia

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

    Aquifer test (or a pumping test) is a field experiment in which a well is pumped at a controlled rate and the aquifer's response (drawdown) is measured in one or more observation wells. [5] Cone of depression is a conically-shaped depression that is produced in a water table as a result of pumping water from a well at a given rate. [4]

  4. Aquifer test - Wikipedia

    en.wikipedia.org/wiki/Aquifer_test

    Aquifer testing is a common tool that hydrogeologists use to characterize a system of aquifers, aquitards and flow system boundaries. A slug test is a variation on the typical aquifer test where an instantaneous change (increase or decrease) is made, and the effects are observed in the same well.

  5. List of aquifers - Wikipedia

    en.wikipedia.org/wiki/List_of_aquifers

    Cambro-Ordovician aquifer system; California Central Valley aquifer system; Eastern Snake River Plain Aquifer; Edwards Aquifer; Englishtown aquifer; Floridan aquifer; Great Miami aquifer; Kirkwood–Cohansey aquifer; Lloyd aquifer; Magothy aquifer – largest of Long Island's aquifers; Mahomet Aquifer; Medina aquifer; Mt. Laurel–Wenonah ...

  6. Groundwater model - Wikipedia

    en.wikipedia.org/wiki/Groundwater_model

    Typical aquifer cross-section. An unambiguous definition of "groundwater model" is difficult to give, but there are many common characteristics. A groundwater model may be a scale model or an electric model of a groundwater situation or aquifer. Groundwater models are used to represent the natural groundwater flow in the environment.

  7. Groundwater flow equation - Wikipedia

    en.wikipedia.org/wiki/Groundwater_flow_equation

    In an unconfined aquifer, the saturated thickness is defined as the vertical distance between the water table surface and the aquifer base. If ∂ h / ∂ z = 0 {\displaystyle \partial h/\partial z=0} , and the aquifer base is at the zero datum, then the unconfined saturated thickness is equal to the head, i.e., b=h .

  8. Oklahoma Water Resources Board - Wikipedia

    en.wikipedia.org/wiki/Oklahoma_Water_Resources_Board

    In Oklahoma, streamwater is defined to include “water in ponds, lakes, reservoirs, and playa lakes” [2] (or dry lakes). Streamwater is considered to be publicly owned; the Oklahoma Water Resources board is responsible for appropriation for all areas of the State of Oklahoma except the Grand River basin, where the Grand River Dam Authority (GRDA) has responsibility for allocation on a use ...

  9. List of aquifers in the United States - Wikipedia

    en.wikipedia.org/wiki/List_of_aquifers_in_the...

    Aquifers of the United States Withdrawal rates from the Ogallala Aquifer.. This is a list of some aquifers in the United States.. Map of major US aquifers by rock type. An aquifer is a geologic formation, a group of formations, or a part of a formation that contains sufficient saturated permeable material to yield significant quantities of water to groundwater wells and springs.