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Ground-water recharge in humid areas of the United States: A summary of Ground-Water Resources Program studies, 2003-2006
Increased demands on water resources by a growing population and recent droughts have raised awareness about the adequacy of ground-water resources in humid areas of the United States. The spatial and temporal variability of ground-water recharge are key factors that need to be quantified to determine the sustainability of ground-water resources. Ground-water recharge is defined herein as the entry into the saturated zone of water made available at the water-table surface, together with the associated flow away from the water table within the saturated zone (Freeze and Cherry, 1979). In response to the need for better estimates of ground-water recharge, the Ground-Water Resources Program (GWRP) of the U.S. Geological Survey (USGS) began an initiative in 2003 to estimate ground-water recharge rates in the relatively humid areas of the United States.
Suggested Citation
Delin, G.N., and Risser, D.W., 2007, Ground-water recharge in humid areas of the United States: A summary of Ground-Water Resources Program studies, 2003-2006: U.S. Geological Survey Fact Sheet 2007-3007, 4 p., https://doi.org/10.3133/fs20073007.
ISSN: 2327-6932 (online)
Study Area
Publication type
Report
Publication Subtype
USGS Numbered Series
Title
Ground-water recharge in humid areas of the United States: A summary of Ground-Water Resources Program studies, 2003-2006
Series title
Fact Sheet
Series number
2007-3007
DOI
10.3133/fs20073007
Year Published
2007
Language
English
Publisher
U.S. Geological Survey
Publisher location
Reston, VA
Contributing office(s)
Groundwater Resources Program, Pennsylvania Water Science Center, Toxic Substances Hydrology Program