Effect of cell physicochemical characteristics and motility on bacterial transport in groundwater
M.W. Becker, S.A. Collins, D.W. Metge, R.W. Harvey, A.M. Shapiro
2004, Journal of Contaminant Hydrology (69) 195-213
The influence of physicochemical characteristics and motility on bacterial transport in groundwater were examined in flow-through columns. Four strains of bacteria isolated from a crystalline rock groundwater system were investigated, with carboxylate-modified and amidine-modified latex microspheres and bromide as reference tracers. The bacterial isolates included a gram-positive rod (ML1), a...
Rare earth element partitioning between hydrous ferric oxides and acid mine water during iron oxidation
P. L. Verplanck, D. Kirk Nordstrom, Howard E. Taylor, B. A. Kimball
2004, Applied Geochemistry (19) 1339-1354
Ferrous iron rapidly oxidizes to Fe (III) and precipitates as hydrous Fe (III) oxides in acid mine waters. This study examines the effect of Fe precipitation on the rare earth element(REE) geochemistry of acid mine waters to determine the pH range over which REEs behave conservatively and the range...
Re-evaluation of heat flow data near Parkfield, CA: Evidence for a weak San Andreas Fault
P.M. Fulton, D.M. Saffer, Reid N. Harris, B.A. Bekins
2004, Geophysical Research Letters (31)
Improved interpretations of the strength of the San Andreas Fault near Parkfield, CA based on thermal data require quantification of processes causing significant scatter and uncertainty in existing heat flow data. These effects include topographic refraction, heat advection by topographically-driven groundwater flow, and uncertainty in thermal conductivity. Here, we re-evaluate...
Surface complexation model of uranyl sorption on Georgia kaolinite
T.E. Payne, J.A. Davis, G.R. Lumpkin, R. Chisari, T.D. Waite
2004, Applied Clay Science (26) 151-162
The adsorption of uranyl on standard Georgia kaolinites (KGa-1 and KGa-1B) was studied as a function of pH (3–10), total U (1 and 10 μmol/l), and mass loading of clay (4 and 40 g/l). The uptake of uranyl in air-equilibrated systems increased with pH and reached...
Formation of a paleothermal anomaly and disseminated gold deposits associated with the Bingham Canyon porphyry Cu-Au-Mo system, Utah
C. G. Cunningham, G.W. Austin, C. W. Naeser, R. O. Rye, G.H. Ballantyne, R.G. Stamm, C.E. Barker
2004, Economic Geology (99) 789-806
The thermal history of the Oquirrh Mountains, Utah, indicates that hydrothermal fluids associated with emplacement of the 37 Ma Bingham Canyon porphyry Cu-Au-Mo deposit extended at least 10 km north of the Bingham pit. An associated paleothermal anomaly enclosed the Barneys Canyon and Melco disseminated gold deposits and several smaller...
Mechanisms of electron acceptor utilization: Implications for simulating anaerobic biodegradation
M.E. Schreiber, G.R. Carey, D. T. Feinstein, J.M. Bahr
2004, Journal of Contaminant Hydrology (73) 99-127
Simulation of biodegradation reactions within a reactive transport framework requires information on mechanisms of terminal electron acceptor processes (TEAPs). In initial modeling efforts, TEAPs were approximated as occurring sequentially, with the highest energy-yielding electron acceptors (e.g. oxygen) consumed before those that yield less energy (e.g., sulfate). Within this framework in...
Relationships between wintering waterbirds and invertebrates, sediments and hydrology of coastal marsh ponds
F. Bolduc, A. D. Afton
2004, Waterbirds (27) 333-341
We studied relationships among sediment variables (carbon content, C:N, hardness, oxygen penetration, silt-clay fraction), hydrologic variables (dissolved oxygen, salinity, temperature, transparency, water depth), sizes and biomass of common invertebrate classes, and densities of 15 common waterbird species in ponds of impounded freshwater, oligohaline, mesohaline, and unimpounded mesohaline marshes during winters...
Comparison of in situ uranium KD values with a laboratory determined surface complexation model
G.P. Curtis, P. Fox, M. Kohler, J.A. Davis
2004, Applied Geochemistry (19) 1643-1653
Reactive solute transport simulations in groundwater require a large number of parameters to describe hydrologic and chemical reaction processes. Appropriate methods for determining chemical reaction parameters required for reactive solute transport simulations are still under investigation. This work compares U(VI) distribution coefficients (i.e. KD values) measured under field conditions with...
Stable metal isotopes reveal copper accumulation and loss dynamics in the freshwater bivalve Corbucula
M.-N. Croteau, S. N. Luoma, B.R. Topping, C.B. Lopez
2004, Environmental Science & Technology (38) 5002-5009
Characterization of uptake and loss dynamics is critical to understanding risks associated with contaminant exposure in aquatic animals. Dynamics are especially important in addressing questions such as why coexisting species in nature accumulate different levels of a contaminant. Here we manipulated copper (Cu) stable isotopic ratios (as...
Geochemistry, radiocarbon ages, and paleorecharge conditions along a transect in the central High Plains aquifer, southwestern Kansas, USA
P.B. McMahon, J.K. Böhlke, S. C. Christenson
2004, Applied Geochemistry (19) 1655-1686
Water samples from short-screen monitoring wells installed along a 90-km transect in southwestern Kansas were analyzed for major ions, trace elements, isotopes (H, B, C, N, O, S, Sr), and dissolved gases (He, Ne, N2, Ar, O2, CH4) to evaluate the geochemistry, radiocarbon ages, and paleorecharge conditions in the unconfined...
Persistence of pharmaceutical compounds and other organic wastewater contaminants in a conventional drinking-water-treatment plant
P. E. Stackelberg, E. T. Furlong, M. T. Meyer, S.D. Zaugg, A.K. Henderson, D.B. Reissman
2004, Science of the Total Environment (329) 99-113
In a study conducted by the US Geological Survey and the Centers for Disease Control and Prevention, 24 water samples were collected at selected locations within a drinking-water-treatment (DWT) facility and from the two streams that serve the facility to evaluate the potential for...
Using an ecoregion framework to analyze land-cover and land-use dynamics.
Alisa L. Gallant, Thomas R. Loveland, Terry L. Sohl, D.E. Napton
2004, Environmental Management (34) S89-S110
The United States has a highly varied landscape because of wide-ranging differences in combinations of climatic, geologic, edaphic, hydrologic, vegetative, and human management (land use) factors. Land uses are dynamic, with the types and rates of change dependent on a host of variables, including land accessibility, economic considerations, and the...
Are big basins just the sum of small catchments?
J. Shaman, M. Stieglitz, D. Burns
2004, Hydrological Processes (18) 3195-3206
Many challenges remain in extending our understanding of how hydrologic processes within small catchments scale to larger river basins. In this study we examine how low-flow runoff varies as a function of basin scale at 11 catchments, many of which are nested, in the 176 km2 Neversink River watershed in...
Baseflow contribution to nitrate-nitrogen export from a large, agricultural watershed, USA
K. Schilling, Y.-K. Zhang
2004, Journal of Hydrology (295) 305-316
Nitrate-nitrogen export from the Raccoon River watershed in west-central Iowa is among the highest in the United State and contributes to impairment of downstream water quality. We examined a rare long-term record of streamflow and nitrate concentration data (1972-2000) to evaluate annual and seasonal patterns of nitrate losses in streamflow...
An integrated geospatial approach to monitoring the Bering Glacier system, Alaska
E.G. Josberger, J. Payne, S. Savage, R. Shuchman, G. Meadows
2004, Conference Paper, International Geoscience and Remote Sensing Symposium (IGARSS)
The Bering Glacier is the largest and longest glacier in continental North America, with an area of approximately 5,175 km2, and a length of 190 km. It is also the largest surging glacier in America, having surged at least five times during the twentieth century. The last surge of the...
Winter orographic precipitation ratios in the Sierra Nevada: Large-scale atmospheric circulations and hydrologic consequences
M. Dettinger, K. Redmond, D. Cayan
2004, Journal of Hydrometeorology (5) 1102-1116
The extent to which winter precipitation is orographically enhanced within the Sierra Nevada of California varies from storm to storm, and season to season, from occasions when precipitation rates at low and high altitudes are almost the same to instances when precipitation rates at middle elevations (considered...
Simulated hydrologic responses to climate variations and change in the Merced, Carson, and American River basins, Sierra Nevada, California, 1900-2099
M. D. Dettinger, D.R. Cayan, M.K. Meyer, A. Jeton
2004, Climatic Change (62) 283-317
Hydrologic responses of river basins in the Sierra Nevada of California to historical and future climate variations and changes are assessed by simulating daily streamflow and water-balance responses to simulated climate variations over a continuous 200-yr period. The coupled atmosphere-ocean-ice-land Parallel Climate Model provides the simulated climate histories, and...
Enhanced gas-phase transport in a deep unsaturated zone, Amargosa Desert (U.S.A.)
Michelle Ann Walvoord, David A. Stonestrom
Karel Kovar, Z. Hrkal, J. Bruthans, editor(s)
2004, Conference Paper, International conference on finite element models, MODFLOW, and more: Solving groundwater problems
No abstract available....
Riparian ecosystem assessments
J. Stromberg, M. Briggs, M. Scott, P. Shafroth
M. B. Baker, P. F. Ffolliott, L. F. DeBano, D. G. Neary, editor(s)
2004, Book chapter, Riparian areas of the southwestern United States: Hydrology, ecology, and management
No abstract available....
Spring onset in the Sierra Nevada: When is snowmelt independent of elevation?
J.D. Lundquist, D.R. Cayan, M. D. Dettinger
2004, Journal of Hydrometeorology (5) 327-342
Short-term climate and weather systems can have a strong influence on mountain snowmelt, sometimes overwhelming the effects of elevation and aspect. Although most years exhibit a spring onset that starts first at lowest and moves to highest elevations, in spring 2002, flow in a variety of streams...
Hydrologic scales, cloud variability, remote sensing, and models: Implications for forecasting snowmelt and streamflow
James J. Simpson, M. D. Dettinger, F. Gehrke, T.J. McIntire, Gary L. Hufford
2004, Weather and Forecasting (19) 251-276
Accurate prediction of available water supply from snowmelt is needed if the myriad of human, environmental, agricultural, and industrial demands for water are to be satisfied, especially given legislatively imposed conditions on its allocation. Robust retrievals of hydrologic basin model variables (e.g., insolation or areal extent of...
Quality assurance report - Loch Vale watershed, 1999-2002
Jorin A. Botte, Jill Baron
2004, Open-File Report 2004-1306
The National Park Service initiated the Loch Vale Watershed (LVWS) project in 1980 with funding from the Aquatic Effects Research Program of the National Acid Precipitation Assessment Program. Long-term ecological research and monitoring address watershed-scale ecosystem processes, particularly as they respond to atmospheric deposition and climate variability. Monitoring of meteorological,...
Sensitivity to acidification of subalpine ponds and lakes in north-western Colorado
K. Campbell, E. Muths, J.T. Turk, P.S. Corn
2004, Hydrological Processes (18) 2817-2834
Although acidifying deposition in western North America is lower than in many parts of the world, many high-elevation ecosystems there are extremely sensitive to acidification. Previous studies determined that the Mount Zirkel Wilderness Area (MZWA) has the most acidic snowpack and aquatic ecosystems that are among the most sensitive in...
Pocomoke Sound Sedimentary and Ecosystem History
Thomas M. Cronin
2004, Open-File Report 2004-1350
Summary of Results: Pocomoke Sound Sediment and Sediment Processes Transport of sediment from coastal marshes. Analyses of pollen and foraminifera from surface sediments in Pocomoke Sound suggest that neither the upstream forested wetlands nor coastal marshes bordering the sound have contributed appreciably to particulate matter in the 10- to 1000-micron size...
Great Lakes clams find refuge from zebra mussels in restored, lake-connected marsh (Ohio)
S. Jerrine Nichols, Douglas A. Wilcox
2004, Ecological Restoration (22) 51-52
Since the early 1990s, more than 95 percent of the freshwater clams once found in Lake Erie have died due to the exotic zebara mussel (Dreissena polymorpha). Zebra mussels attach themselves to native clams in large numbers, impeding the ability of the clams to eat and burrow. However, in...