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  2. Hydrogeology - Wikipedia

    en.wikipedia.org/wiki/Hydrogeology

    Analytic solutions typically are also simply an equation that can give a quick answer based on a few basic parameters. The Theis equation is a simple (yet still very useful) analytic solution to groundwater flow and level around pumping or injecting wells, typically used to analyze the results of an aquifer test or slug test.

  3. Aquifer test - Wikipedia

    en.wikipedia.org/wiki/Aquifer_test

    Type Curves for Selected Problems of Flow to Wells in Confined Aquifers (PDF). Book 3, Applications of Hydraulics. U.S. Geological Survey. Franke, 0.L.; Reilly, T.E.; Bennett, G.D. (1987). "Chapter B5". Definition of Boundary and Initial Conditions in the Analysis of Saturated Ground-Water Flow Systems — An Introduction (PDF). Book 3 ...

  4. Flow net - Wikipedia

    en.wikipedia.org/wiki/Flow_net

    The method is often used in civil engineering, hydrogeology or soil mechanics as a first check for problems of flow under hydraulic structures like dams or sheet pile walls. As such, a grid obtained by drawing a series of equipotential lines is called a flow net. The flow net is an important tool in analysing two-dimensional irrotational flow ...

  5. Groundwater flow equation - Wikipedia

    en.wikipedia.org/wiki/Groundwater_flow_equation

    Used in hydrogeology, the groundwater flow equation is the mathematical relationship which is used to describe the flow of groundwater through an aquifer.The transient flow of groundwater is described by a form of the diffusion equation, similar to that used in heat transfer to describe the flow of heat in a solid (heat conduction).

  6. Rayleigh problem - Wikipedia

    en.wikipedia.org/wiki/Rayleigh_problem

    In fluid dynamics, Rayleigh problem also known as Stokes first problem is a problem of determining the flow created by a sudden movement of an infinitely long plate from rest, named after Lord Rayleigh and Sir George Stokes. This is considered as one of the simplest unsteady problems that have an exact solution for the Navier-Stokes equations.

  7. Fault zone hydrogeology - Wikipedia

    en.wikipedia.org/wiki/Fault_zone_hydrogeology

    Fault zone hydrogeology is the study of how brittlely deformed rocks alter fluid flows in different lithological settings, such as clastic, igneous and carbonate rocks. [1] Fluid movements, that can be quantified as permeability , can be facilitated or impeded due to the existence of a fault zone . [ 1 ]

  8. HEC-RAS - Wikipedia

    en.wikipedia.org/wiki/HEC-RAS

    3D view. HEC-RAS is simulation software used in computational fluid dynamics – specifically, to model the hydraulics of water flow through natural rivers and other channels.. The program was developed by the United States Army Corps of Engineers in order to manage the rivers, harbors, and other public works under their jurisdiction; it has found wide acceptance by many others since its ...

  9. Oscar Edward Meinzer - Wikipedia

    en.wikipedia.org/wiki/Oscar_Edward_Meinzer

    Cuban well diggers at Guantanamo Base in 1920 Camp in Craters of the Moon National Monument, 1921 photo by Meinzer. Casa Techo in San Antonio, Cuba (1920). Oscar Edward Meinzer (November 28, 1876 – June 14, 1948) was an American hydrogeologist who has been called the "father of modern groundwater hydrology".