Groundwater flow, quality (2007-10), and mixing in the Wind Cave National Park area, South Dakota
Andrew J. Long, Marc J. Ohms, Jonathan D.R.G. McKaskey
2012, Scientific Investigations Report 2011-5235
A study of groundwater flow, quality, and mixing in relation to Wind Cave National Park in western South Dakota was conducted during 2007-11 by the U.S. Geological Survey in cooperation with the National Park Service because of water-quality concerns and to determine possible sources of groundwater contamination in the Wind...
Water chemistry and electrical conductivity database for rivers in Yellowstone National Park, Wyoming
Laura E. Clor, R. Blaine McCleskey, Mark A. Huebner, Jacob B. Lowenstern, Henry P. Heasler, Dan L. Mahony, Tim Maloney, William C. Evans
2012, Data Series 632
Chloride flux has been used to estimate heat flow in volcanic environments since the method was developed in New Zealand by Ellis and Wilson (1955). The method can be applied effectively at Yellowstone, because nearly all of the water discharged from its thermal features enters one of four major rivers...
Uranium isotopes (234U/238U) in rivers of the Yukon Basin (Alaska and Canada) as an aid in identifying water sources, with implications for monitoring hydrologic change in arctic regions
Thomas F. Kraemer, Timothy P. Brabets
2012, Hydrogeology Journal (20) 469-481
The ability to detect hydrologic variation in large arctic river systems is of major importance in understanding and predicting effects of climate change in high-latitude environments. Monitoring uranium isotopes (234U and 238U) in river water of the Yukon River Basin of Alaska and northwestern Canada (2001–2005) has enhanced the ability to...
Preliminary assessment of channel stability and bed-material transport in the Rogue River basin, southwestern Oregon
Krista L. Jones, Jim E. O'Connor, Mackenzie K. Keith, Joseph F. Mangano, J. Rose Wallick
2012, Open-File Report 2011-1280
This report summarizes a preliminary assessment of bed-material transport, vertical and lateral channel changes, and existing datasets for the Rogue River basin, which encompasses 13,390 square kilometers (km2) along the southwestern Oregon coast. This study, conducted to inform permitting decisions regarding instream gravel mining, revealed that:The Rogue River in its...
Utilizing multichannel electrical resistivity methods to examine the dynamics of the fresh water–seawater interface in two Hawaiian groundwater systems
Natasha T. Dimova, Peter W. Swarzenski, Henrieta Dulaiova, Craig R. Glenn
2012, Journal of Geophysical Research C: Oceans (117)
Multichannel electrical resistivity (ER) measurements were conducted at two contrasting coastal sites in Hawaii to obtain new information on the spatial scales and dynamics of the fresh water–seawater interface and rates of coastal groundwater exchange. At Kiholo Bay (located on the dry, Kona side of the Big Island) and at...
Using micro-seismicity and seismic velocities to map subsurface geologic and hydrologic structure within the Coso geothermal field, California
Joern Ole Kaven, Stephen H. Hickman, Nicholas C. Davatzes
2012, Conference Paper, Proceedings, Thirty-Seventh Workshop on Geothermal Reservoir Engineering
Geothermal reservoirs derive their capacity for fluid and heat transport in large part from faults and fractures. Micro-seismicity generated on such faults and fractures can be used to map larger fault structures as well as secondary fractures that add access to hot rock, fluid storage and recharge capacity necessary to...
In situ quantification of spatial and temporal variability of hyporheic exchange in static and mobile gravel-bed rivers
Donald O. Rosenberry, P. Zion Klos, Andrew Neal
2012, Hydrological Processes (26) 604-612
Seepage meters modified for use in flowing water were used to directly measure rates of exchange between surface and subsurface water in a gravel‐ and cobble bed river in western Pennsylvania, USA (Allegheny River, Qmean = 190 m3/s) and a sand‐ and gravel‐bed river in Colorado, USA (South Platte River,...
Influence of a thin veneer of low-hydraulic-conductivity sediment on modelled exchange between river water and groundwater in response to induced infiltration
Donald O. Rosenberry, Richard W. Healy
2012, Hydrological Processes (26) 544-557
A thin layer of fine‐grained sediment commonly is deposited at the sediment–water interface of streams and rivers during low‐flow conditions, and may hinder exchange at the sediment–water interface similar to that observed at many riverbank‐filtration (RBF) sites. Results from a numerical groundwater‐flow model indicate that a low‐permeability veneer reduces the...
Preliminary analysis of the hydrologic effects of temporary shutdowns of the Rondout-West Branch Water Tunnel on the groundwater-flow system in Wawarsing, New York
Frederick Stumm, Anthony Chu, Michael D. Como, Michael L. Noll
2012, Scientific Investigations Report 2012-5015
Flooding of streets and residential basements, and bacterial contamination of private-supply wells with Escherichia coli (E. coli) are recurring problems in the Rondout Valley near the Town of Wawarsing, Ulster County, New York. Leakage from the Rondout-West Branch (RWB) Water Tunnel and above-normal precipitation have been suspected of causing elevated...
Survey of hydrologic models and hydrologic data needs for tracking flow in the Rio Grande, north-central New Mexico, 2010
Anne Tillery, Jack R. Eggleston
2012, Scientific Investigations Report 2011-5207
The six Middle Rio Grande Pueblos have prior and paramount rights to deliveries of water from the Rio Grande for their use. When the pueblos or the Bureau of Indian Affairs Designated Engineer identifies a need for additional flow on the Rio Grande, the Designated Engineer is tasked with deciding...
Selected water-quality data from the Cedar River and Cedar Rapids well fields, Cedar Rapids, Iowa, 2006-10
Gregory R. Littin
2012, Data Series 657
The Cedar River alluvial aquifer is the primary source of municipal water in the Cedar Rapids, Iowa area. Municipal wells are completed in the alluvial aquifer approximately 40 to 80 feet below land surface. The City of Cedar Rapids and the U.S. Geological Survey have been conducting a cooperative study...
Fluid geochemistry of Yucca Mountain and vicinity
Brian D. Marshall, Richard J. Moscati, Gary L. Patterson
John S. Stuckless, editor(s)
2012, Book chapter, Hydrology and geochemistry of Yucca Mountain and vicinity, Southern Nevada and California
Yucca Mountain, a site in southwest Nevada, has been proposed for a deep underground radioactive waste repository. An extensive database of geochemical and isotopic characteristics has been established for pore waters and gases from the unsaturated zone, perched water, and saturated zone waters in the Yucca Mountain area. The development...
Evidence from 12-year study links ecosystem changes in the Gulf of Maine with climate change
George R. Aiken, Thomas G. Huntington, William Balch, David Drapeau, Bruce Bowler
2012, EcoSystem Indicator Partnership Journal
Investigators at the Bigelow Laboratory for Ocean Sciences (East Boothbay, Maine) and the U.S. Geological Survey collaborated to study ecosystem changes in the Gulf of Maine. As part of the Gulf of Maine North Atlantic Time Series (GNATS), a comprehensive long-term study of hydrographic, biological, optical and chemical properties,...
Watershed modeling applications in south Texas
Diana E. Pedraza, Darwin J. Ockerman
2012, Fact Sheet 2012-3005
Watershed models can be used to simulate natural and human-altered processes including the flow of water and associated transport of sediment, chemicals, nutrients, and microbial organisms within a watershed. Simulation of these processes is useful for addressing a wide range of water-resource challenges, such as quantifying changes in water availability...
Anaerobic oxidation of arsenite by autotrophic bacteria: The view from Mono Lake, California
Ronald S. Oremland, John F. Stolz, Chad W. Saltikov
Joanne M. Santini, Seamus A. Ward, editor(s)
2012, Book chapter, The metabolism of arsenite
Introduction The phenomenon of arsenite [As(III)] oxidation by aerobic bacteria was first reported by Green (1918), and the many subsequent discoveries made in this realm, most occurring over the past three decades, are the primary focus of this book. In contrast, the fact that select anaerobes can also achieve this feat...
Restoration of freshwater cypress-tupelo wetlands in the southeastern U.S. following severe hurricanes
William H. Conner, Ken W. Krauss, Gary P. Shaffer
2012, Book chapter, A goal-oriented approach to forest landscape restoration
Freshwater forested wetlands commonly occur in the lower Coastal Plain of the southeastern US with baldcypress (Taxodium distichum [L.] L.C. Rich.) and water tupelo (Nyssa aquatica L.) often being the dominant trees. Extensive anthropogenic activities combined with eustatic sea-level rise and land subsidence have caused widespread hydrological changes...
Remote sensing of evapotranspiration for operational drought monitoring using principles of water and energy balance
Gabriel B. Senay, Stefanie Bohms, James P. Verdin, Martha C. Anderson, Christopher Hain, Brian D. Wardlow, Agustin Pimstein, John R. Mecikalski, William P. Kustas
Brian D. Wardlow, Martha C. Anderson, James P. Verdin, editor(s)
2012, Book chapter, Remote sensing of drought: Innovative monitoring approaches
Evapotranspiration (ET) is an important component of the hydrologic budget because it režects the exchange of mass and energy between the soil-water-vegetation system and the atmosphere. Prevailing weather conditions inžuence potential or reference ET through variables such as radiation, temperature, wind, and relativity humidity. In addition to these weather variables,...
Population dynamics of Corbicula fluminea (Müller, 1774) in mesohaline and oligohaline habitats: Invasion success in a Southern Europe estuary
J.N. Franco, F.R. Ceia, J. Patricio, Janet K. Thompson, J.C. Marques, J.M. Neto
2012, Estuarine, Coastal and Shelf Science (112) 31-39
Due to its range expansion and potential ecological effects, Corbicula fluminea is considered one of the most important non-indigenous species (NIS) in aquatic ecosystems. Its presence since 2003 in the upstream area of Mondego estuary (oligohaline and mesohaline sectors) was studied during thirteen months, from December 2007 to December 2008....
Future opportunities and challenges in remote sensing of drought
Brian D. Wardlow, Martha C. Anderson, Justin Sheffield, Brad Doorn, James Verdin, Xiwu Zhan, Matt Rodell
Brian D. Wardlow, Martha C. Anderson, James P. Verdin, editor(s)
2012, Book chapter, Remote sensing of drought: innovative monitoring approaches
The value of satellite remote sensing for drought monitoring was first realized more than two decades ago with the application of Normalized Difference Index (NDVI) data from the Advanced Very High Resolution Radiometer (AVHRR) for assessing the effect of drought on vegetation. Other indices such as the Vegetation Health Index...
Post-wildfire wind erosion in and around the Idaho National Laboratory Site
Matthew J. Germino
2012, Report
Wind erosion following large wildfires on and around the INL Site is a recurrent threat to human health and safety, DOE operations and trafficability, and ecological and hydrological condition of the INL Site and down-wind landscapes. Causes and consequences of wind erosion are mainly known from warm deserts (e.g., Southwest...
Endangered river fish: factors hindering conservation and restoration
Steven J. Cooke, Craig P. Paukert, Zeb Hogan
2012, Endangered Species Research (17) 179-191
Globally, riverine fish face many anthropogenic threats including riparian and flood plain habitat degradation, altered hydrology, migration barriers, fisheries exploitation, environmental (climate) change, and introduction of invasive species. Collectively, these threats have made riverine fishes some of the most threatened taxa on the planet. Although much effort has been devoted...
Introduction to phytoremediation of contaminated groundwater
James E. Landmeyer
2012, Book
This book provides the reader with the comprehensive view necessary to understand and critically evaluate the design, implementation, and monitoring of phytoremediation at sites characterized by contaminated groundwater. Part I presents the historical foundation of the interaction between plants and groundwater, introduces fundamental groundwater concepts for plant physiologists, and...
The effects of permafrost thaw on soil hydrologic, thermal, and carbon dynamics in an Alaskan peatland
Jonathan A. O’Donnell, M. Torre Jorgenson, Jennifer W. Harden, A. David McGuire, Mikhail Z. Kanevskiy, Kimberly P. Wickland
2012, Ecosystems (15) 213-229
Recent warming at high-latitudes has accelerated permafrost thaw in northern peatlands, and thaw can have profound effects on local hydrology and ecosystem carbon balance. To assess the impact of permafrost thaw on soil organic carbon (OC) dynamics, we measured soil hydrologic and thermal dynamics and soil OC stocks across a...
The science, information, and engineering needed to manage water availability and quality in 2050
Robert M. Hirsch
2012, Book chapter, Toward a sustainable water future: Visions for 2050
This chapter explores four water resources issues: 1) hydrologic variability, hazards, water supply and ecosystem preservation; 2) urban landscape design; 3) non-point source water quality, and 4) climate change, resiliency, and nonstationarity. It also considers what science, technology, and engineering practice may be needed in the coming decades to...
Preliminary physical stratigraphy, biostratigraphy, and geophysical data of the USGS South Dover Bridge Core, Talbot County, Maryland
Wilma B. Aleman Gonzalez, David S. Powars, Ellen Seefelt, Lucy E. Edwards, Jean M. Self-Trail, Colleen T. Durand, Arthur P. Schultz, Peter P. McLaughlin
2012, Open-File Report 2012-1218
The South Dover Bridge (SDB) corehole was drilled in October 2007 in Talbot County, Maryland. The main purpose for drilling this corehole was to characterize the Upper Cretaceous and Paleogene lithostratigraphy and biostratigraphy of the aquifers and confining units of this region. The data obtained from this core also will...
