Skip to main content
U.S. flag

An official website of the United States government

Publications

Publications are crucial for the dissemination of the Virginia and West Virginia Water Science Center's scientific data and conclusions. View journal articles authored by our Center's scientists here. The full, searchable catalog of USGS publications can be accessed through the USGS Publications Warehouse.

Filter Total Items: 267

The Virginia Beach shallow ground-water study

IntroductionVirginia Beach is a rapidly growing city of more than 425,000 people. Sources of fresh water within the city, however, are limited. Prior to 1998, the Virginia Beach Public Utilities Department met the city's water needs by purchasing treated drinking water from the City of Norfolk. Because Norfolk had to meet its own requirements, the amount of water available to Virginia Beach was li
Authors
Henry M. Johnson

USGS ground-water flow model : an essential tool for managing the water supply of the Virginia Coastal Plain

Virginia needs a reliable water supply to sustain its growing population and expanding economy. In 1990, the aquifers in the Coastal Plain supplied about 100 million gallons per day (mgd) to the citizens, businesses, and industries of Virginia. It is estimated that by the year 2000, demand will increase by another 10 mgd and likely will continue to increase in future years.Ground water is the only
Authors
Martha L. Erwin, Randolph E. McFarland, Bruce T. Scott

Measuring streamflow in Virginia (1999 revision)

The U.S. Geological Survey (USGS), U.S. Department of the Interior, is the Nation's largest Earth-science information agency. Among its many responsibilities, such as map making and providing information on earthquakes and other natural hazards, the USGS provides information on the Nation's water resources. The USGS has collected and analyzed hydrologic (water-related) information for more than 10
Authors
Roger M. Moberg, Karen C. Rice, Eugene D. Powell

Hydrology and geochemistry of carbonate springs in Mantua Valley, northern Utah

Water chemistry, tritium data, precipitation-discharge relations, geology, topography, and dye tracing were used to determine recharge areas, ground-water residence times, factors influencing ground-water flow, and aquifer characteristic for five springs that discharge from Paleozoic limestones and dolostones along the margin of Manuta Valley, northern Utah.Temperature of Mantua Valley spring wate
Authors
Karen C. Rice, Lawrence E. Spangler

Trace-element concentrations in streambed sediment across the conterminous United States

Trace-element concentrations in 541 streambed-sediment samples collected from 20 study areas across the conterminous United States were examined as part of the National Water-Quality Assessment Program of the U.S. Geological Survey. Sediment samples were sieved and the <63-μm fraction was retained for determination of total concentrations of trace elements. Aluminum, iron, titanium, and organic ca
Authors
Karen C. Rice

Natural processes for managing nitrate in ground water discharged to Chesapeake Bay and other surface waters: More than forest buffers

Ground-water discharge is a significant source of nitrate load to tidal creeks, coastal estuaries, and Chesapeake Bay. Different studies have found that forest buffers greater than 200 feet wide remove most of the nitrate from passing ground water. These buffers are commonly included in regional nutrient-management strategies. Results of a U.S. Geological Survey study on the Eastern Shore of Virgi
Authors
Gary K. Speiran, Pixie A. Hamilton, Michael D. Woodside

A demonstration of the instream flow incremental methodology, Shenandoah River, Virginia

Current and projected demands on the water resources of the Shenandoah River have increased concerns for the potential effect of these demands on the natural integrity of the Shenandoah River system. The Instream Flow Incremental Method (IFIM) process attempts to integrate concepts of water-supply planning, analytical hydraulic engineering models, and empirically derived habitat versus flow functi
Authors
Humbert Zappia, Donald C. Hayes

Transmission of atmospherically deposited trace elements through an undeveloped, forested Maryland watershed

Retention and transmission of atmospherically-derived major (H+, Na+, K+, Ca2+, Mg2+, HCO3-, NO3-, SO4-2, Cl-, SiO2) and trace (Al, As, Cd, Cr, Cu, Fe, Mn, Ni, Pb, Se, and Zn) species were evaluated in an undeveloped forested watershed underlain by a rather inert quartzite lithology (Bear Branch, Catoctin State Forest, Thrumont, Maryland). These comparisons were based on atmospheric input to stre
Authors
T.M. Church, J.R. Scudlark, Kathryn M. Conko, Owen P. Bricker, Karen C. Rice

Comparison of hydrochemical tracers to estimate source contributions to peak flow in a small, forested, headwater catchment

Three-component (throughfall, soil water, groundwater) hydrograph separations at peak flow were performed on 10 storms over a 2-year period in a small forested catchment in north-central Maryland using an iterative and an exact solution. Seven pairs of tracers (deuterium and oxygen 18, deuterium and chloride, deuterium and sodium, deuterium and silica, chloride and silica, chloride and sodium, and
Authors
Karen C. Rice, George M. Hornberger

Use of geochemical mass balance modelling to evaluate the role of weathering in determining stream chemistry in five mid-Atlantic watersheds on different lithologies

The importance of mineral weathering was assessed and compared for five mid-Atlantic watersheds receiving similar atmospheric inputs but underlain by differing bedrock. Annual solute mass balances and volume-weighted mean solute concentrations were calculated for each watershed for each year of record. In addition, primary and secondary mineralogy were determined for each of the watersheds through
Authors
Anne K. O'Brien, Karen C. Rice, Owen P. Bricker, Margaret M. Kennedy, R. Todd Anderson

Acid Rain

Acid deposition, or acid rain as it is more commonly referred to, has become a widely publicized environmental issue in the U.S. over the past decade. The term usually conjures up images of fish kills, dying forests, "dead" lakes, and damage to monuments and other historic artifacts. The primary cause of acid deposition is emission of S02 and NOx to the atmosphere during the combustion of fossil f
Authors
Owen P. Bricker, Karen C. Rice