Results of pumping test of an artesian well near Battle Mountain, Lander County, Nevada
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Petrology and reservoir properties of South Barrow test wells no. 1 and no. 2, 1949
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Report on three specimens from South Barrow Test Well No. 1 with unusual permeability behavior, January 1949
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Reservoir characteristics indicated by thin section analyses of sand cores from Umiat Test No. 1, 1947
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Petrography and reservoir characteristics of Umiat Test Well 9, 1952
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Core analyses report on Simpson Test Well No. 1, 1948
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Core analysis on core samples from South Barrow Test Well No. 1, November 1948
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Core analysis on core samples from South Barrow Test Well No. 2, 1949
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Graphic and written logs, Gubik Test Well No. 2
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Graphic and written logs, Umiat Test Well No. 11
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The results of a pumping test at Foley, Taylor County, Florida
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The "slug test" for estimating transmissibility
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Records of test wells at Canyon Reservoir site in Comal County, Texas
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Additional notes on the multiple-step drawdown test
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Report on seismic survey at Ordnance Test Station, Maynard, Massachusetts
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Results of pumping tests in the Widefield area, Fountain Valley, Colorado
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An aquifer test in the southwestern part of the Louisville area, Kentucky
The unconsolidated sand and gravel deposits along the Ohio River at Louisville, Ky. contain a large quantity of ground water. Parts of the aquifer have been overdeveloped in recent years, however, and at the present time great emphasis is being placed on proper location, development, and use of ground-water supplies. The present trend of industrial growth is to the southwest of the city in the undeveloped area along the Ohio River, where the yields to individual wells are higher and relatively large supplies can be developed. The average coefficient of permeability and storage coefficient of the aquifer here are 1,500 gallons per day per square foot and 0.2, respectively.
Kentucky↗