Publications
New York Water Science Center publications
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Filter Total Items: 715
Concentrations of pesticides and pesticide degradates in the Croton River Watershed in southeastern New York, July-September 2000 Concentrations of pesticides and pesticide degradates in the Croton River Watershed in southeastern New York, July-September 2000
Thirty-seven pesticides and (or) pesticide degradates were detected in baseflow samples collected from 47 stream sites in the Croton River Watershed (374 square miles) in southeastern New York in the summer of 2000. The Croton Reservoir provides about 10 percent of New York City's water supply. Maximum concentrations of most pesticides detected did not exceed 0.1 μg/L (micrograms per...
Authors
Patrick J. Phillips, Robert W. Bode
Characterization of fractures and flow zones in a contaminated shale at the Watervliet Arsenal, Albany County, New York Characterization of fractures and flow zones in a contaminated shale at the Watervliet Arsenal, Albany County, New York
Flow zones in a fractured shale in and near a plume of volatile organic compounds at the Watervliet Arsenal in Albany County, N. Y. were characterized through the integrated analysis of geophysical logs and single- and cross-hole flow tests. Information on the fracture-flow network at the site was needed to design an effective groundwater monitoring system, estimate offsite contaminant...
Authors
John Williams, Frederick L. Paillet
Hydrogeology of the Tully Lakes area in southern Onondaga and northern Cortland Counties, New York Hydrogeology of the Tully Lakes area in southern Onondaga and northern Cortland Counties, New York
Water levels in a series of kettlehole lakes and ponds known as the Tully Lakes respond to seasonal water-level changes in the surrounding aquifer but often differ from ground-water levels in the aquifer because the lakebed sediments are poorly permeable and inhibit the exchange of water. Three sets of ground-water-level measurements were made from the spring recharge period of 2000...
Authors
William M. Kappel, Todd S. Miller, Kari K. Hetcher
Frequently co‐occurring pesticides and volatile organic compounds in public supply and monitoring wells, southern New Jersey, USA Frequently co‐occurring pesticides and volatile organic compounds in public supply and monitoring wells, southern New Jersey, USA
One or more pesticides were detected with one or more volatile organic compounds (VOCs) in more than 95% of samples collected from 30 public supply and 95 monitoring wells screened in the unconsolidated surficial aquifer system of southern New Jersey, USA. Overall, more than 140,000 and more than 3,000 unique combinations of pesticides with VOCs were detected in two or more samples from...
Authors
Paul E. Stackelberg, Leon J. Kauffman, Mark A. Ayers, Arthur L. Baehr
Controls of stream chemistry and fish populations in the Neversink watershed, Catskill Mountains, New York Controls of stream chemistry and fish populations in the Neversink watershed, Catskill Mountains, New York
The Neversink Watershed Study was initiated in 1991 to develop an understanding of the key natural processes that control water quality within the forested, 166 km 2 (64 mi 2), Neversink River watershed; part of the New York City drinking water supply system, in the Catskill Mountain region of New York. The study entailed (1) hydrological investigations of water movement from the...
Authors
Gregory B. Lawrence, Douglas A. Burns, Barry P. Baldigo, Peter S. Murdoch, Gary M. Lovett
Hydrogeology and extent of saltwater intrusion of the Great Neck peninsula, Great Neck, Long Island, New York Hydrogeology and extent of saltwater intrusion of the Great Neck peninsula, Great Neck, Long Island, New York
Great Neck, a peninsula, in the northwestern part of Nassau County, N.Y., is underlain by unconsolidated deposits that form a sequence of aquifers and confining units. Seven public-supply wells have been affected by the intrusion of saltwater from the surrounding embayments (Little Neck Bay, Long Island Sound, Manhasset Bay). Fifteen observation wells were drilled in 1991–96 for the...
Authors
Frederick Stumm
Copper avoidance and mortality of juvenile brown trout (Salmo trutta) in tests with copper-sulfate-treated water from West Branch Reservoir, Putnam County, New York Copper avoidance and mortality of juvenile brown trout (Salmo trutta) in tests with copper-sulfate-treated water from West Branch Reservoir, Putnam County, New York
Copper-avoidance tests and acute-toxicity (mortality) tests on hatchery-reared, young-of- the-year brown trout (salmo trutta) were conducted with water from West Branch Reservoir to assess the avoidance response to copper sulfate treatment, which is used occasionally by New York City Department of Environmental Protection to decrease phytoplankton populations in the reservoir. Avoidance...
Authors
Barry P. Baldigo, T.P. Baudanza
Salt-front movement in the Hudson River estuary, New York — Simulations by one-dimensional flow and solute-transport models Salt-front movement in the Hudson River estuary, New York — Simulations by one-dimensional flow and solute-transport models
The Hudson River is being considered for use as a supplemental source of water supply for New York City during droughts. One proposal entails withdrawal of Hudson River water from locations near Newburgh, Chelsea, or Kingston, but the extent to which this could cause the salt front to advance upstream to points where it could adversely affect community water supplies is unknown. The U.S
Authors
M. Peter de Vries, Lawrence A. Weiss
Water resources of Monroe County, New York, water years 1994-96, with emphasis on water quality in the Irondequoit Creek basin: Atmospheric deposition, ground water, streamflow, trends in water quality, and chemical loads to Irondequoit Bay Water resources of Monroe County, New York, water years 1994-96, with emphasis on water quality in the Irondequoit Creek basin: Atmospheric deposition, ground water, streamflow, trends in water quality, and chemical loads to Irondequoit Bay
Irondequoit Creek drains 169 square miles in the eastern part of Monroe County. Nutrients transported by Irondequoit Creek to Irondequoit Bay on Lake Ontario have contributed to the eutrophication of the Bay. Sewage-treatment-plant effluent, a major source of nutrients to the creek and its tributaries, was eliminated from the basin in 1979 by diversion to a regional wastewater-treatment...
Authors
Donald A. Sherwood
Simulated effects of 1994 salt-mine collapse on ground-water flow and land subsidence in a glacial aquifer system, Livingston County, New York Simulated effects of 1994 salt-mine collapse on ground-water flow and land subsidence in a glacial aquifer system, Livingston County, New York
This report describes the hydrogeology of the Genesee Valley and the effects of the ceiling collapse of the Retsof salt mine on the aquifer system. It discusses the origin and character of glacial sediments; the occurrence, flow directions, and chemical quality of water in the aquifer system before the collapse; the effects of the collapse on the aquifer system in terms of land...
Authors
Richard M. Yager, Todd S. Miller, William M. Kappel
Effects of stream acidification and habitat on fish populations of a North American river Effects of stream acidification and habitat on fish populations of a North American river
Water quality, physical habitat, and fisheries at sixteen reaches in the Neversink River Basin were studied during 1991-95 to identify the effects of acidic precipitation on stream-water chemistry and on selected fish-species populations, and to test the hypothesis that the degree of stream acidification affected the spatial distribution of each fish-species population. Most sites on the...
Authors
Barry P. Baldigo, Gregory B. Lawrence
Ground-water age dating in community wells in Oswego County, New York Ground-water age dating in community wells in Oswego County, New York
Officials in Oswego County, in north-central New York, have been concerned about potential contamination of community wells. Many of these wells are completed in unconfined glacial sand-and-gravel aquifers, although some are finished in till or in the underlying fractured and jointed bedrock of Late Ordovician and Early Silurian ages. Local shallow ground-water flow is affected by the...
Authors
Stephen C. Komor