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Cooper-Jacob Solution for Confined AquifersDescriptionA mathematical solution by Cooper and Jacob (1946) is useful for determining the hydraulic properties (transmissivity and storativity) of confined aquifers. Analysis involves matching a straight line to water-level displacement data as a function of the logarithm time since the start of pumping.
AQTESOLV also includes Jacob's correction for partial dewatering of water-table aquifers, thereby allowing use of the Cooper-Jacob solution for unconfined aquifers. For variable rate pumping tests, the implementation of the Cooper-Jacob solution in AQTESOLV is equivalent to the method of Birsoy and Summers (1980) which applies the principle of superposition to the Cooper-Jacob approximation of the Theis equation. AssumptionsThe following assumptions apply to the use of the Cooper-Jacob solution:
Solution OptionsAQTESOLV provides the following options for the Cooper-Jacob solution:
ReferencesBirsoy, Y.K. and W.K. Summers, 1980. Determination of aquifer parameters from step tests and intermittent pumping data, Ground Water, vol. 18, pp. 137-146. Cooper, H.H. and C.E. Jacob, 1946. A generalized graphical method for evaluating formation constants and summarizing well field history, Am. Geophys. Union Trans., vol. 27, pp. 526-534. |
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