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Sources and occurrence of chloroform and other trihalomethanes in drinking-water supply wells in the United States, 1986-2001
Tamara Ivahnenko, J.S. Zogorski
2006, Scientific Investigations Report 2006-5015
Chloroform and three other trihalomethanes (THMs)--bromodichloromethane, dibromochloromethane, and bromoform--are disinfection by-products commonly produced during the chlorination of water and wastewater. Samples of untreated ground water from drinking-water supply wells (1,096 public and 2,400 domestic wells) were analyzed for THMs and other volatile organic compounds (VOCs) during 1986-2001, or compiled, as...
Geohydrology of the lower Apalachicola-Chattahoochee-Flint River basin, southwestern Georgia, northwestern Florida, and southeastern Alabama
Lynn J. Torak, Jaime A. Painter
2006, Scientific Investigations Report 2006-5070
The lower Apalachicola-Chattahoochee-Flint (ACF) River Basin contains about 4,600 square miles of karstic and fluvial plains and nearly 100,000 cubic miles of predominantly karst limestone connected hydraulically to the principal rivers and lakes in the Coastal Plain of southwestern Georgia, northwestern Florida, and southwestern Alabama. Sediments of late-middle Eocene to...
Water-quality characteristics of Montana streams in a statewide monitoring network, 1999-2003
John H. Lambing, Thomas E. Cleasby
2006, Scientific Investigations Report 2006-5046
A statewide monitoring network of 38 sites was operated during 1999-2003 in cooperation with the Montana Department of Environmental Quality to provide a broad geographic base of water-quality information on Montana streams. The purpose of this report is to summarize and describe the water-quality characteristics for those sites. Samples were...
Simulation of nutrient and sediment concentrations and loads in the Delaware inland bays watershed: Extension of the hydrologic and water-quality model to ungaged segments
Angelica L. Gutierrez-Magness
2006, Scientific Investigations Report 2006-5038
Rapid population increases, agriculture, and industrial practices have been identified as important sources of excessive nutrients and sediments in the Delaware Inland Bays watershed. The amount and effect of excessive nutrients and sediments in the Inland Bays watershed have been well documented by the Delaware Geological Survey, the Delaware Department...
Hydrogeology of the upper and middle Verde River watersheds, central Arizona
Kyle W. Blasch, John P. Hoffmann, Leslie F. Graser, Jeannie R. Bryson, Alan L. Flint
2006, Scientific Investigations Report 2005-5198
The upper and middle Verde River watersheds in central Arizona are primarily in Yavapai County, which in 1999 was determined to be the fastest growing rural county in the United States; by 2050 the population is projected to more than double its current size (132,000 in 2000). This study combines...
Water quality and relation to taste-and-odor compounds in the North Fork Ninnescah River and Cheney Reservoir, south-central Kansas, 1997-2003
Victoria G. Christensen, Jennifer L. Graham, Chad R. Milligan, Larry M. Pope, Andrew C. Ziegler
2006, Scientific Investigations Report 2006-5095
Cheney Reservoir, the primary water supply for the city of Wichita in south-central Kansas, and its main source of inflow, the North Fork Ninnescah River, were sampled between 1997 and 2003 for sediment, nutrients, and the taste-and-odor-causing compounds geosmin and 2-methylisoborneol (MIB). It is believed that objectionable tastes and odors...
A thermal profile method to identify potential ground-water discharge areas and preferred salmonid habitats for long river reaches
J. J. Vaccaro, K.J. Maloy
2006, Scientific Investigations Report 2006-5136
The thermal regime of riverine systems is a major control on aquatic ecosystems. Ground water discharge is an important abiotic driver of the aquatic ecosystem because it provides preferred thermal structure and habitat for different types of fish at different times in their life history. In large diverse river basins...
A system for calibrating seepage meters used to measure flow between ground water and surface water
Donald O. Rosenberry, Michael A. Menheer
2006, Scientific Investigations Report 2006-5053
A system has been developed for generating controlled rates of seepage across the sediment-water interface representing flow between ground water and surface water. The seepage- control system facilitates calibration and testing of seepage measurement devices commonly called seepage meters. Two slightly different seepage-control systems were evaluated. Both designs make use...
Ground-water levels near the top of the water-table mound, western Cape Cod, Massachusetts, 2002-04
Andrew J. Massey, Carl S. Carlson, Denis R. LeBlanc
2006, Scientific Investigations Report 2006-5054
In January 2002 the U.S. Geological Survey began continuous water-level monitoring in three wells in the vicinity of the Southeast Ranges of Camp Edwards, near the Impact Area of the Massachusetts Military Reservation on Cape Cod. The purpose of this effort was to examine how water levels at sites with...
Questa baseline and pre-mining ground-water quality investigation. 21. Hydrology and water balance of the Red River Basin, New Mexico, 1930-2004
Cheryl A. Naus, Douglas P. McAda, Nathan C. Myers
2006, Scientific Investigations Report 2006-5040
A study of the hydrology of the Red River Basin of northern New Mexico, including development of a pre- mining water balance, contributes to a greater understanding of processes affecting the flow and chemistry of water in the Red River and its alluvial aquifer. Estimates of mean annual precipitation for...
Regionalized equations for bankfull-discharge and channel characteristics of streams in New York State—Hydrologic Region 7 in western New York
Christiane I. Mulvihill, Anne G. Ernst, Barry P. Baldigo
2006, Scientific Investigations Report 2006-5075
Computation of bankfull discharge and channel dimensions (width, depth, and cross-sectional area) at ungaged sites requires equations that relate bankfull discharge and channel dimensions to drainage-area at gaged sites. Bankfull-channel information commonly is needed for watershed assessments, stream channel classification, and the design of stream-restoration projects. Such equations are most...
Geohydrological characterization, water-chemistry, and ground-water flow simulation model of the Sonoma Valley area, Sonoma County, California
Christopher D. Farrar, Loren F. Metzger, Tracy Nishikawa, Kathryn M. Koczot, Eric G. Reichard, Victoria E. Langenheim
2006, Scientific Investigations Report 2006-5092
The Sonoma Valley, located about 30 miles north of San Francisco, is one of several basins in Sonoma County that use a combination of ground water and water delivered from the Russian River for supply. Over the past 30 years, Sonoma Valley has experienced rapid population growth and land-use changes....
Atlas of climatic controls of wildfire in the western United States
S. W. Hostetler, P. J. Bartlein, J.O. Holman
2006, Scientific Investigations Report 2006-5139
Wildfire behavior depends on several factors including ecologic characteristics, near-term and antecedent climatic conditions,fuel availability and moisture level, weather, and sources of ignition (lightning or human). The variability and interplay of these factors over many spatial and temporal scales present an ongoing challenge to our ability to forecast a given...
A preliminary evaluation of vertical separation between production intervals of coalbed-methane wells and water-supply wells in the Raton basin, Huerfano and Las Animas Counties, Colorado, 1999-2004
Kenneth R. Watts
2006, Scientific Investigations Report 2006-5109
The Raton Basin in southern Colorado and northern New Mexico is undergoing increased development of its coalbed-methane resources. Annual production of methane from coalbeds in the Raton Basin in Huerfano and Las Animas Counties, Colorado, increased from about 28,000,000 thousand cubic feet from 478 wells to about 80,000,000 thousand cubic...
Is amplitude loss of sonic waveforms due to intrinsic attenuation or source coupling to the medium?
Myung W. Lee
2006, Scientific Investigations Report 2006-5120
Sonic waveforms acquired in gas-hydrate-bearing sediments indicate strong amplitude loss associated with an increase in sonic velocity. Because the gas hydrate increases sonic velocities, the amplitude loss has been interpreted as due to intrinsic attenuation caused by the gas hydrate in the pore space, which apparently contradicts conventional wave propagation...
A method of Shaly sand correction for estimating gas hydrate saturations using downhole electrical resistivity log data
Myung W. Lee, Timothy S. Collett
2006, Scientific Investigations Report 2006-5121
Estimation of the amount of nonconductive and conductive constituents in the pore space of sediments, using electrical resistivity logs, generally loses accuracy when clays are present in the reservoir. Many different methods and clay models have been proposed to account for the conductivity of clay (for example, the shaly sand...
Geology and resources of some world oil-shale deposits
John R. Dyni
2006, Scientific Investigations Report 2005-5294
Oil-shale deposits are in many parts of the world. They range in age from Cambrian to Tertiary and were formed in a variety of marine, continental, and lacustrine depositional environments. The largest known deposit is in the Green River Formation in the western United States; it contains an estimated 213...
Characterization of surface-water resources in the Great Basin National Park area and their susceptibility to ground-water withdrawals in adjacent valleys, White Pine County, Nevada
Peggy E. Elliott, David A. Beck, David E. Prudic
2006, Scientific Investigations Report 2006-5099
Eight drainage basins and one spring within the Great Basin National Park area were monitored continually from October 2002 to September 2004 to quantify stream discharge and assess the natural variability in flow. Mean annual discharge for the stream drainages ranged from 0 cubic feet per second at Decathon Canyon...
Development and application of a screening model for simulating regional ground-water flow in the St. Croix River basin, Minnesota and Wisconsin
Daniel T. Feinstein, Cheryl A. Buchwald, Charles P. Dunning, Randall J. Hunt
2006, Scientific Investigations Report 2005-5283
A series of databases and an accompanying screening model were constructed by the U.S. Geological Survey, in cooperation with the National Park Service, to better understand the regional ground-water-flow system and its relation to stream drainage in the St. Croix River Basin. The St. Croix River and its tributaries drain...
Modeling water quality effects of structural and operational changes to Scoggins Dam and Henry Hagg Lake, Oregon
Annett B. Sullivan, Stewart A. Rounds
2006, Scientific Investigations Report 2006-5060
To meet water quality targets and the municipal and industrial water needs of a growing population in the Tualatin River Basin in northwestern Oregon, an expansion of Henry Hagg Lake is under consideration. Hagg Lake is the basin's primary storage reservoir and provides water during western Oregon's typically dry summers....
Vulnerability of recently recharged ground water in the High Plains aquifer to nitrate contamination
Jason J. Gurdak, Sharon L. Qi
2006, Scientific Investigations Report 2006-5050
Nitrate concentrations greater than background levels have been detected in ground water of the High Plains aquifer. Empirically based models and corresponding maps were developed that predict the vulnerability of the aquifer to nonpoint-source nitrate contamination. The models predict the probability of detecting nitrate concentrations larger than 4 milligrams per...
Comparison of macroinvertebrate community structure between two riffle-based sampling protocols in Wyoming, Colorado, and Montana, 2000-2001
David A. Peterson, Jeremy R. Zumberge
2006, Scientific Investigations Report 2006-5117
Samples of benthic macroinvertebrates were collected side-by-side from riffles at 12 stream sites in Wyoming, Colorado, and Montana during 2000-2001, following protocols established by the U.S. Geological Survey National Water-Quality Assessment (NAWQA) Program and the U.S. Environmental Protection Agency Environmental Monitoring and Assessment Program (EMAP). Samples from riffles were collected...
Computer program for the Kendall family of trend tests
Dennis R. Helsel, David K. Mueller, James R. Slack
2006, Scientific Investigations Report 2005-5275
The Seasonal Kendall (SK) test for trend was developed by the U.S. Geological Survey and has become the most frequently used test for trend in the environmental sciences. Recently the test was modified to form the Regional Kendall (RK) test for trend. In this form, trends at numerous locations within...
Synthesis of monthly and annual streamflow records (water years 1950-2003) for Big Sandy, Clear, Peoples, and Beaver Creeks in the Milk River basin, Montana
Charles Parrett
2006, Scientific Investigations Report 2005-5216
To address concerns expressed by the State of Montana about the apportionment of water in the St. Mary and Milk River basins between Canada and the United States, the International Joint Commission requested information from the United States government about water that originates in the United States but does not...