High-Capacity Test Well Developed At The Air Force Base, Dover, Delaware

Author(s)Rasmussen, W.C.
Author(s)Groot, J.J.
Author(s)Depman, A.J.
Date Accessioned2008-03-11T19:48:11Z
Date Available2008-03-11T19:48:11Z
Publication Date1958-06
AbstractA thick aquifer of Eocene age underlies the Dover area, Delaware at depths ranging from 250 to 400 feet below the land surface. The aquifer is about 250 feet thick beneath the Dover Air Force Base and is composed of fairly uniform medium to fine glauconitic quartz sand. The static water level in a test well at the base was 18 feet below the land surface, or 5.7 feet above sea level, on April 17, 1957. The yield of the test well was about 300 gpm (gallons per minute), and the specific capacity at the end of a 12-hour pumping period was 8.3 gpm per foot of drawdown.en_US
SponsorU.S. Geological Survey and U.S. Army Corps of Engineersen_US
URLhttp://udspace.udel.edu/handle/19716/3096
Languageen_USen_US
PublisherNewark, DE: Delaware Geological Survey, University of Delawareen_US
Part of SeriesReport of Investigationsen_US
Part of Series2en_US
Keywordsaquiferen_US
Keywordsquality of wateren_US
Keywordsobservation wellen_US
KeywordsDover, Delawareen_US
Keywordsrechargeen_US
TitleHigh-Capacity Test Well Developed At The Air Force Base, Dover, Delawareen_US
TypeTechnical Reporten_US
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