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  2. Aquifer test - Wikipedia

    en.wikipedia.org/wiki/Aquifer_test

    The Theis equation was created by Charles Vernon Theis (working for the US Geological Survey) in 1935, [1] from heat transfer literature (with the mathematical help of C.I. Lubin), for two-dimensional radial flow to a point sink in an infinite, homogeneous aquifer. It is simply

  3. Slug test - Wikipedia

    en.wikipedia.org/wiki/Slug_test

    Because the flow rate into or out of the well is not constant, as is the case in a typical aquifer test, the standard Theis solution does not work. Mathematically , the Theis equation is the solution of the groundwater flow equation for a step increase in discharge rate at the pumping well; a slug test is instead an instantaneous pulse at the ...

  4. Hydrogeology - Wikipedia

    en.wikipedia.org/wiki/Hydrogeology

    The Theis equation is one of the most commonly used and fundamental solutions to the groundwater flow equation; it can be used to predict the transient evolution of head due to the effects of pumping one or a number of pumping wells. The Thiem equation is a solution to the steady state groundwater flow equation (Laplace's Equation) for flow to ...

  5. Well test - Wikipedia

    en.wikipedia.org/wiki/Well_test

    where s is drawdown (units of length e.g., m), is the pumping rate (units of volume flowrate e.g., m³/day), is the aquifer loss coefficient (which increases with time — as predicted by the Theis solution) and is the well loss coefficient (which is constant for a given flow rate).

  6. Groundwater flow equation - Wikipedia

    en.wikipedia.org/wiki/Groundwater_flow_equation

    The above groundwater flow equations are valid for three dimensional flow. In unconfined aquifers, the solution to the 3D form of the equation is complicated by the presence of a free surface water table boundary condition: in addition to solving for the spatial distribution of heads, the location of this surface is also an unknown. This is a ...

  7. Specific storage - Wikipedia

    en.wikipedia.org/wiki/Specific_storage

    These equations relate a change in total or water volume (or ) per change in applied stress (effective stress — or pore pressure — ) per unit volume. The compressibilities (and therefore also S s ) can be estimated from laboratory consolidation tests (in an apparatus called a consolidometer), using the consolidation theory of soil mechanics ...

  8. Theis was held on a parole detainer, awaiting sentencing on convictions of first-degree home invasion, larceny of vehicles and other crimes, according to the Morning Sun. A bedsheet was reportedly used. Jail or Agency: Isabella County Jail; State: Michigan; Date arrested or booked: UNKNOWN; Date of death: 5/31/2016; Age at death: 36; Sources ...

  9. Exponential integral - Wikipedia

    en.wikipedia.org/wiki/Exponential_integral

    Nonequilibrium groundwater flow in the Theis solution (called a well function) Radiative transfer in stellar and planetary atmospheres; Radial diffusivity equation for transient or unsteady state flow with line sources and sinks; Solutions to the neutron transport equation in simplified 1-D geometries [18]