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Hantush-Jacob Step Drawdown Test Solution for Leaky AquifersDescriptionA mathematical solution by Hantush-Jacob (1955) is useful for determining the hydraulic properties (transmissivity and storativity) of leaky confined aquifers. Analysis involves matching the solution to water-level displacement data collected during a step test. The Hantush-Jacob step test solution also includes linear and nonlinear well losses for the pumping well (Jacob 1947; Rorabaugh 1953; Ramey 1982). AQTESOLV for Windows provides visual and automatic methods for matching the Theis step test solution to pumping test data. This easy-to-use and intuitive software promotes rapid and accurate determination of aquifer properties. AssumptionsThe following assumptions apply to the use of the Hantush-Jacob step test solution:
Solution OptionsAQTESOLV for Windows provides the following options for the Hantush-Jacob step test solution:
ReferencesHantush, M.S. and C.E. Jacob, 1955. Non-steady radial flow in an infinite leaky aquifer, Am. Geophys. Union Trans., vol. 36, pp. 95-100. 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. Bear, J., 1979. Hydraulics of Groundwater, McGraw-Hill, New York, 569p. |
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