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Publications

This list of Water Resources Mission Area publications includes both official USGS publications and journal articles authored by our scientists. A searchable database of all USGS publications can be accessed at the USGS Publications Warehouse.

Filter Total Items: 19021

Nanoparticles formed from bacterial oxyanion reduction of toxic Group 15 and 16 metalloids Nanoparticles formed from bacterial oxyanion reduction of toxic Group 15 and 16 metalloids

This chapter presents some examples of nanoparticles formed by only a few microbial species that are cultivated in only a handful of laboratories worldwide. The investigations so far have just scratched the surface of the potential of the natural world to yield bionanomineral producers. While future research should involve screening surveys of the prokaryotes for this biomineralizing...
Authors
C.I. Pearce, S. Baseman, J.W. Fellowes, Ronald S. Oremland

Hydrology and biogeochemistry linkages Hydrology and biogeochemistry linkages

This chapter provides an overview of the linkages between hydrology and biogeochemistry in terrestrial and aquatic systems. Selected topics include hydrological pathways on drainage basin slopes, mountain environments, within-river (or in-stream) processes, wetlands, groundwater (and groundwater–surface water interactions), and lakes. Beginning from catchment headwaters, This chapter...
Authors
Norman E. Peters, J. K. Bohlke, P. D. Brooks, T.P. Burt, Michael N. Gooseff, David P. Hamilton, P. J. Mulholland, Nigel Roulet, J.V. Turner

Long-term natural attenuation of crude oil in the subsurface Long-term natural attenuation of crude oil in the subsurface

The time frame for natural attenuation of crude oil contamination in the subsurface has been studied for the last 27 years at a spill site located near Bemidji, Minnesota, USA. Data from the groundwater contaminant plume show that dissolved benzene concentrations adjacent to the oil decreased by 50% between 1993 and 2007. To assess how this decrease is related to benzene concentrations...
Authors
Barbara A. Bekins, Mary Jo Baedecker, Robert P. Eganhouse, William N. Herkelrath

Arsenic Arsenic

No abstract available.
Authors
John F. Stolz, Ron Oremland

Nutrient inputs to the Laurentian Great Lakes by source and watershed estimated using SPARROW watershed models Nutrient inputs to the Laurentian Great Lakes by source and watershed estimated using SPARROW watershed models

Nutrient input to the Laurentian Great Lakes continues to cause problems with eutrophication. To reduce the extent and severity of these problems, target nutrient loads were established and Total Maximum Daily Loads are being developed for many tributaries. Without detailed loading information it is difficult to determine if the targets are being met and how to prioritize rehabilitation...
Authors
Dale M. Robertson, David A. Saad

Changes in low-flow frequency from 1976-2006 at selected streamgages in New York, excluding Long Island Changes in low-flow frequency from 1976-2006 at selected streamgages in New York, excluding Long Island

Many Federal, State, and local agencies use low-flow data to establish water-use policy and help determine the total maximum daily loads and effluent limits of point and nonpoint sources of contamination of surface water during periods of decreased streamflow. Low-flow magnitude and frequency are used often by water-supply planners, reservoir managers, and hydroelectric facilities to...
Authors
Thomas P. Suro, Christopher L. Gazoorian

National Acid Precipitation Assessment Program Report to Congress: An integrated assessment National Acid Precipitation Assessment Program Report to Congress: An integrated assessment

Acid deposition, more commonly known as acid rain, occurs when emissions of sulfur dioxide (SO2) and nitrogen oxides (NOx) react in the atmosphere with water, oxygen, and oxidants to form various acidic compounds. Prevailing winds transport the acidic compounds hundreds of miles, often across state and national borders. These acidic compounds then fall to earth in either a wet form (rain...
Authors
Douglas A. Burns, Mark E. Fenn, Jill Baron, Jason A. Lynch, Bernard J. Cosby

Comment on “An unconfined groundwater model of the Death Valley Regional Flow System and a comparison to its confined predecessor” by R.W.H. Carroll, G.M. Pohll and R.L. Hershey [Journal of Hydrology 373/3–4, pp. 316–328] Comment on “An unconfined groundwater model of the Death Valley Regional Flow System and a comparison to its confined predecessor” by R.W.H. Carroll, G.M. Pohll and R.L. Hershey [Journal of Hydrology 373/3–4, pp. 316–328]

Carroll et al. (2009) state that the United States Geological Survey (USGS) Death Valley Regional Flow System (DVRFS) model, which is based on MODFLOW, is “conceptually inaccurate in that it models an unconfined aquifer as a confined system and does not simulate unconfined drawdown in transient pumping simulations.” Carroll et al. (2009) claim that “more realistic estimates of water...
Authors
Claudia C. Faunt, Alden M. Provost, Mary C. Hill, Wayne R. Belcher

Vegetation history along the eastern, desert escarpment of the Sierra San Pedro Mártir, Baja California, Mexico Vegetation history along the eastern, desert escarpment of the Sierra San Pedro Mártir, Baja California, Mexico

Plant macrofossils from 38 packrat middens spanning the last ~ 33,000 cal yr BP record vegetation between ~ 650 and 900 m elevation along the eastern escarpment of the Sierra San Pedro Mártir, northern Baja California. The middens span most of the Holocene, with a gap between ~ 4600 and 1800 cal yr BP, but coverage in the Pleistocene is uneven with a larger hiatus between 23,100 and 14...
Authors
Camille A. Holmgren, Julio L. Betancourt, Kate A. Rylander

South Cascade (USA/North Cascades) South Cascade (USA/North Cascades)

The U.S. Geological Survey has closely monitored this temperate mountain glacier since the late 1950s. During 1958-2007, the glacier retreated about 0.7 km and shrank in area from 2.71 to 1.73 km2, although part of the area change was due to separation of contributing ice bodies from the main glacier. Maximum and average glacier thicknesses are about 170 and 80 m, respectively. Year-to...
Authors
William R. Bidlake

Applications of Groundwater Helium Applications of Groundwater Helium

Helium abundance and isotope variations have widespread application in groundwater-related studies. This stems from the inert nature of this noble gas and the fact that its two isotopes ? helium-3 and helium-4 ? have distinct origins and vary widely in different terrestrial reservoirs. These attributes allow He concentrations and 3He/4He isotope ratios to be used to recognize and...
Authors
Justin T. Kulongoski, David R. Hilton
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