Hydrology of the unconfined aquifer system, Rancocas Creek area, Rancocas, Crosswicks, Assunpink, Blacks, and Crafts Creek Basins, New Jersey, 1996
Martha K. Watt, A.C. Kane, E. G. Charles, D. A. Storck
2003, Water-Resources Investigations Report 2002-4280
No abstract available....
In situ arsenic remediation in a fractured, alkaline aquifer
A. H. Welch, Kenneth G. Stollenwerk, D. K. Maurer, Lawrence S. Feinson
A. H. Welch, Kenneth G. Stollenwerk, editor(s)
2003, Book chapter, Arsenic in ground water
No abstract available. ...
Effects of stormwater infiltration on quality of groundwater beneath retention and detention basins
D. Fischer, Emmanuel G. Charles, Arthur L. Baehr
2003, Journal of Environmental Engineering (129) 464-471
Infiltration of storm water through detention and retention basins may increase the risk of groundwater contamination, especially in areas where the soil is sandy and the water table shallow, and contaminants may not have a chance to degrade or sorb onto soil particles before reaching the saturated zone. Groundwater from...
Simulation of the Ground-Water Flow System in 1992, and Simulated Effects of Projected Ground-Water Withdrawals in 2020 in the New Jersey Coastal Plain
Alison D. Gordon
2003, Water-Resources Investigations Report 2003-4000
In 1992, ground-water withdrawals from the unconfined and confined aquifers in the New Jersey Coastal Plain totaled about 300 million gallons per day, and about 70 percent (200 million galllons per day) of this water was pumped from confined aquifers. The withdrawals have created large cones of depression in several...
Review of Selected References and Data sets on Ambient Ground- and Surface-Water Quality in the Metedeconk River, Toms River, and Kettle Creek Basins, New Jersey, 1980-2001
Robert S. Nicholson, Kathryn Hunchak-Kariouk, Stephen J. Cauller
2003, Water-Resources Investigations Report 2003-4259
Surface water and ground water from unconfined aquifers are the primary sources of drinking water for much of the population, about 391,000, in the Metedeconk River, Toms River, and Kettle Creek watersheds in the New Jersey Coastal Plain. The quality of these sources of drinking water is a concern because...
Evaluation of Streamflow, Water Quality, and Permitted and Nonpermitted Loads and Yields in the Raritan River Basin, New Jersey, Water Years 1991-98
Robert G. Reiser
2003, Water-Resources Investigations Report 2003-4207
Seventeen water-quality constituents were analyzed in samples collected from 21 surface-water sampling sites in the Raritan River Basin during water years 1991-97. Loads were computed for seven constituents. Thirteen constituents have associated instream water-quality standards that are used as reference levels when evaluating the data. Nine of the 13 constituents...
Ground-water levels and potentiometric surfaces, Naval Air Warfare Center, West Trenton, New Jersey, 2000
Pierre J. Lacombe
2002, Water-Resources Investigations Report 2001-4197
Water levels were measured in wells at the decommissioned Naval Air Warfare Center in West Trenton, N.J., during 2000. Water-level hydrographs prepared from data collected at seven observation wells on the base show changes caused by seasonal and daily climate conditions and by the pumping of contaminated water from recovery...
Real-time ground-water-level monitoring in New Jersey
Walter D. Jones, Anthony S. Navoy, Daryll A. Pope
2002, Fact Sheet 011-02
A network of seven observation wells that transmit ground-water-level data on a real-time basis through satellite telemetry is operating (started May 2001) in New Jersey through a cooperative effort of the U.S. Geological Survey (USGS) and the New Jersey Department of Environmental Protection (NJDEP). The water-level data from these observation...
Simulation of Transient Ground-Water Flow in the Valley-Fill Aquifers of the Upper Rockaway River Basin, Morris County, New Jersey
Alison D. Gordon
2002, Water-Resources Investigations Report 2001-4174
More than 90 percent of the public water supply in the upper Rockaway River Valley in Morris County, New Jersey, is obtained from ground-water withdrawals from the valley-fill aquifers. During 1997, an average of 9.6 million gallons per day of ground water was withdrawn from these aquifers. The aquifer system...
Effects of Pumping on Ground-Water Flow Near Water-Supply Wells in the Lower Potomac-Raritan-Magothy Aquifer, Pennsauken Township, Camden County, New Jersey
Richard L. Walker
2001, Water-Resources Investigations Report 2000-4012
Since the 1970's, hexavalent chromium has been detected in concentrations as great as 1.0 milligram per liter in wells at the Puchack well field operated by the Camden City Department of Utilities, Water Division (Water Department), forcing the Water Department to progressively remove five of its six wells from service...
Effects of land use and travel time on the distribution of nitrate in the Kirkwood-Cohansey aquifer system in southern New Jersey
Leon J. Kauffman, Arthur L. Baehr, Mark A. Ayers, Paul E. Stackelberg
2001, Water-Resources Investigations Report 2001-4117
Residents of the southern New Jersey Coastal Plain are increasingly reliant on the unconfined Kirkwood-Cohansey aquifer system for public water supply as a result of increasing population and restrictions on withdrawals from the deeper, confined aquifers. Elevated nitrate concentrations above background levels have been found in wells in the surficial...
Relation of Mercury to Other Chemical Constituents in Ground Water in the Kirkwood-Cohansey Aquifer System, New Jersey Coastal Plain, and Mechanisms for Mobilization of Mercury from Sediments to Ground Water
Julia L. Barringer, Cecilia L. MacLeod
2001, Water-Resources Investigations Report 2000-4230
Water from 265 domestic wells that tap the unconfined Kirkwood-Cohansey aquifer system in the Coastal Plain of New Jersey contained concentrations of mercury that are equal to or exceed the U.S. Environmental Protection Agency maximum contaminant level (MCL) of 2 ug/L (micrograms per liter). The wells range in depth from...
Hydrology of the unconfined aquifer system, Maurice River area: Maurice and Cohansey River Basins, New Jersey, 1994-95
Emmanuel G. Charles, Donald A. Storck, Rick M. Clawges
2001, Water-Resources Investigations Report 2001-4229
No abstract available....
Frequently co‐occurring pesticides and volatile organic compounds in public supply and monitoring wells, southern New Jersey, USA
Paul E. Stackelberg, Leon J. Kauffman, Mark A. Ayers, Arthur L. Baehr
2001, Environmental Toxicology and Chemistry (20) 853-865
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...
Variation in aluminum, iron, and particle concentrations in oxic ground-water samples collected by use of tangential-flow ultrafiltration with low-flow sampling
Zoltan Szabo, J.H. Oden, J. Gibs, D.E. Rice, Y. Ding
Jensen J LBurggraf L W, editor(s)
2001, Conference Paper, Proceedings of SPIE - The International Society for Optical Engineering
Particulates that move with ground water and those that are artificially mobilized during well purging could be incorporated into water samples during collection and could cause trace-element concentrations to vary in unfiltered samples, and possibly in filtered samples (typically 0.45-um (micron) pore size) as well, depending on the particle-size fractions...
Water quality and occurrence of methyl-tert butyl ether (MTBE) and other fuel related compounds in lakes and ground water at lakeside communities in Sussex and Morris Counties, New Jersey, 1998-1999
Arthur L. Baehr, Timothy J. Reilly
2001, Water-Resources Investigations Report 2001-4149
Densely populated communities surround many of the larger lakes in northwestern New Jersey. These communities derive most of their water supply from wells. The lakes can be navigated by gasoline-powered watercraft, can be in various stages of eutrophication, may contain pathogens associated with bathing and waterfowl, and are periodically subjected...
Simulated Effects of Alternative Pumping Strategies on Ground-Water-Flow Patterns and Areas Contributing Recharge to Selected Wells near Kenvil, Morris County, New Jersey
Frederick J. Spitz, Robert S. Nicholson
2001, Water-Resources Investigations Report 2001-4180
Ground-water-flow patterns and areas contributing recharge to supply wells change in response to new or altered pumping stresses. An understanding of these potential changes is essential for the effective evaluation of possible future water-supply alternatives, especially if the supply wells may be vulnerable to contamination from the land surface. Demand...
Water Resources Data - New Jersey, Water Year 1999, Volume 3, Water-Quality Data
M.J. DeLuca, K.M. Romanok, M.L. Riskin, G.L. Mattes, A.M. Thomas, B.J. Gray
2000, Water Data Report NJ-99-3
Water-resources data for the 1999 water year for New Jersey are presented in three volumes, and consists of records of stage, discharge, and water quality of streams; stage and contents of lakes and reservoirs; and water levels and water quality of ground water. Volume 3 contains a summary of surface...
Analysis of persistent organic pollutants in the Newark Bay Estuary, New Jersey, U.S.A.
D. I. Thal, S. A. Mills, Timothy P. Wilson, Jennifer L. Bonin
2000, Organohalogen Compounds (45) 74-77
No abstract available....
Change in field turbidity and trace element concentrations during well purging
J. Gibs, Zoltan Szabo, T. Ivahnenko, F.D. Wilde
2000, Ground Water (38) 577-588
Various physical and chemical properties were monitored sequentially in the field during well purging as indicators of stabilization of the composition of the water in the well. Turbidity was monitored on site during purging of oxic water from three wells with screened intervals open to an unconfined aquifer system in...
Use of Low-Flow Trend and Transfer-Function Models to Determine Relation of Low Flows to Regional Urbanization and Precipitation, Rahway River Basin, New Jersey, 1940-91
Thomas H. Barringer, Robert G. Reiser, Curtis V. Price
2000, Open-File Report 99-257
The Rahway River Basin in northern New Jersey has become heavily urbanized. The importance of the Rahway River as a water-supply source for the region led to an investigation of trends in the river's low-flow characteristics over time and their relation to regional urbanization and precipitation. Since 1950, low flows...
Water quality in the Long Island-New Jersey coastal drainages, New York and New Jersey, 1996–98
Mark A. Ayers, Jonathan G. Kennen, Paul E. Stackelberg
2000, Circular 1201
No abstract available....
Water Resources Data: New Jersey, Water Year 1998, Volume 1, Surface-Water Data
T.J. Reed, G.L. Centinaro, J.F. Dudek, V. Corcino, G.C. Stekroadt, R.C. McTigure
1999, Water Data Report NJ-98-1
This volume of the annual hydrologic data report of New Jersey is one of a series of annual reports that document hydrologic data gathered from the U.S. Geological Survey's surface- and ground-water data-collection networks in each State, Puerto Rico, and the Trust Territories. These records of streamflow, ground-water levels, and...
Relation of pesticide concentrations to season, streamflow, and land use in seven New Jersey streams
Robert G. Reiser
1999, Water-Resources Investigations Report 99-4154
The presence and variability of pesticides in seven New Jersey streams was documented by analyzing 146 samples collected from the streams from April 1996 through June 1998. The samples were analyzed for 85 pesticides, including 50 herbicides, 28 insecticides, and 7 degradation products, at method detection limits that ranged from...
Simulation of ground-water flow and movement of the freshwater-saltwater interface in the New Jersey coastal plain
Daryll A. Pope, Alison D. Gordon
1999, Water-Resources Investigations Report 98-4216
The confined aquifers of the New Jersey Coastal Plain are sands that range in thickness from 50 to 600 feet and are separated by confining units. The confining units are composed of silts and clays that range in thickness from 500 to 1,000 feet. The aquifers are recharged by precipitation...