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- W8073544 abstract "An aquifer pump test with tracers was performed in Bear Creek Valley at the Oak Ridge Facility from October 6, 1986 to October 9, 1986. The objective of the test was to determine the principal values (maximum and minimum) of aquifer transmissivity, and their directions. The well field consisted of nine wells screened in the Nolichucky Shale, part of the Conasauga group of Upper Cambrian age. The test well was pumped at a constant rate of 2.5 gallons-per-minute. Once steady state conditions were approximated, a salt solution was introduced in three different observation wells at different times to evaluate the anisotropy of the system in terms of dispersivity and effective transport porosity. Drawdown data indicated that, hydraulically, the tested volume of the aquifer responded as an anisotropic porous media. The principal values of transmissivity are on the order on 10/sup -3/ ft/sup 2//s and 10/sup -5/ ft/sup 2//s and are oriented along strike and perpendicular to strike, respectively. The aquifer has a storage coefficient of about 6 x 10/sup -4/ which indicates partially confined to confined conditions. Observed tracer breakthrough curves were matched to analytical solutions to determine values of dispersivity and effective transport porosity. Along strike, these values aremore » about 10 feet and 4 x 10/sup -3/, respectively. Perpendicular to strike the values may be 10 feet and 8 x 10/sup -3/, respectively, although additional testing of longer duration will be required to confirm these results. No conclusive results could be interpreted with regard to scale and double porosity effects.« less" @default.
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- W8073544 date "1987-10-01" @default.
- W8073544 modified "2023-09-26" @default.
- W8073544 title "Aquifer pump test with tracers" @default.
- W8073544 hasPublicationYear "1987" @default.
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