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Time, distance, and drawdown relationships in a pumped ground-water basin
Several reasonable values are assumed for coefficients of transmissibility and storage of lenticular alluvial deposits, These values when substituted in the Theis (1935) nonequilibrium formula as modified by Wenzel (1942) give curves from which time, distance, drawdown relationships are estimated.
Suggested Citation
Kunkel, F., 1960, Time, distance, and drawdown relationships in a pumped ground-water basin: U.S. Geological Survey Circular 433, 8 p. :ill. ;27 cm. + graphs in back pocket., https://doi.org/10.3133/cir433.
ISSN: 2330-5703 (online)
Publication type
Report
Publication Subtype
USGS Numbered Series
Title
Time, distance, and drawdown relationships in a pumped ground-water basin