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Problem - Several supply wells in Oswego County were evaluated by the USGS in 1999 by using stable oxygen and hydrogen isotopes and chlorofluorocarbon (CFC) age dating techniques. For two municipal well sites (the Villages of Sandy Creek and Lacona, and the Village of Pulaski) that tap a shallow, unconfined aquifer (typically 20-50 ft thick) there were significant discrepancies between ground-water recharge ages determined by chemical data and those determined by ground-water-flow models developed by independent studies. The significant discrepancies between the times of travel of ground water as determined by numerical ground-water-flow modeling and geochemical dating techniques in Oswego County need to be understood...
Categories: Data,
Project;
Types: Downloadable,
Map Service,
OGC WFS Layer,
OGC WMS Layer,
Shapefile;
Tags: Completed,
Cooperative Water Program,
GW Model,
GW Model,
GW model, All tags...
Geophysics,
Geophysics,
Groundwater-Flow Modeling,
Groundwater-Flow Modeling,
Groundwater-Flow Modeling,
Hydrogeologic Characterization,
Hydrogeologic Characterization,
Hydrogeologic Characterization,
Hydrogeologic Characterization,
New York,
Oswego County, Tug Hill, hydrogeology, aquifer,
USGS New York Water Science Center,
WSC,
Water Use and Availability Science,
Water Use and Availability Science, Fewer tags
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