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On non-artesian groundwater flow

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Summary

The present paper deals with certain problems of non-artesian aquifers, with special reference to non-steady flow due to replenishment from the ground surface. Solutions are obtained by direct integration ofBoussinesq's differential equation (transformed), taking also the inclination of the groundwater surface and the slope of the bottom of the aquifer into account. — The study has some bearing on hydrological investigations. For example, it may be desired to find the location of a moving groundwater divide between two water courses, or to determine the quantity of groundwater passing between them. Problems of this nature are also often met with in water supply (artificial infiltration, etc.) and other fields of engineering practice.

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References

  • Baumann Paul,Ground-water movement controlled through spreading, Trans. ASCE, Vol. 117 (1952).

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Werner, P.W. On non-artesian groundwater flow. Geofisica Pura e Applicata 25, 37–43 (1953). https://doi.org/10.1007/BF02014053

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  • DOI: https://doi.org/10.1007/BF02014053

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