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Theis Step Drawdown Test Solution for Confined AquifersDescriptionA mathematical solution by Theis (1935) is useful for determining the hydraulic properties (transmissivity and storativity) of confined aquifers. Analysis involves matching the solution to water-level displacement data collected during a step test. The Theis step test solution also includes linear and nonlinear well losses for the pumping well (Jacob 1947; Rorabaugh 1953; Ramey 1982).
AssumptionsThe following assumptions apply to the use of the Theis step test solution:
Solution OptionsAQTESOLV for Windows provides the following options for the Theis step test solution:
ReferencesTheis, C.V., 1935. The relation between the lowering of the piezometric surface and the rate and duration of discharge of a well using groundwater storage, Am. Geophys. Union Trans., vol. 16, pp. 519-524. Jacob, C.E., 1947. Drawdown test to determine effective radius of artesian well, Trans. Amer. Soc. of Civil Engrs., vol. 112, paper 2321, pp. 1047-1064. Ramey, H.J., 1982. Well-loss function and the skin effect: A review. In: Narasimhan, T.N. (ed.) Recent trends in hydrogeology, Geol. Soc. Am., special paper 189, pp. 265-271. Rorabaugh, M.J., 1953. Graphical and theoretical analysis of step-drawdown test of artesian well, Proc. Amer. Soc. Civil Engrs., vol. 79, separate no. 362, 23 pp. |
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