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Page 455, results 11351 - 11375

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Modelling within the stream-catchment continuum
Kenneth E. Bencala, John H. Duff, Judson W. Harvey, A. P. Jackman, F.J. Triska
A.J. Jakeman, M. Beck, Ryan J. McAleer, editor(s)
1993, Book chapter, Modeling change in environmental systems
No abstract available....
High-precision measurement of chlorine stable isotope ratios
A. Long, C.J. Eastoe, R.S. Kaufmann, J.G. Martin, L. Wirt, J.B. Finley
1993, Geochimica et Cosmochimica Acta (57) 2907-2912
We present an analysis procedure that allows stable isotopes of chlorine to be analyzed with precision sufficient for geological and hydrological studies. The total analytical precision is ≤±0.09%., and the present known range of chloride in the surface and near-surface environment is 3.5‰. As Cl− is essentially nonreactive in natural aquatic...
Dissolved inorganic nitrogen composition, transformation, retention, and transport in naturally phosphate-rich and phosphate-poor tropical streams
F.J. Triska, C. M. Pringle, G. W. Zellweger, J.H. Duff, R.J. Avanzino
1993, Canadian Journal of Fisheries and Aquatic Sciences (50) 665-675
The composition, transformation, and transport of dissolved inorganic nitrogen (DIN) was compared in waters associated with two lowland streams in Costa Rica. The Salto River is enriched by geothermal-based soluble reactive phosphorus (SRP), which raises the concentration up to 200 μg/L whereas Pantano...
A finite-volume Eulerian-Lagrangian Localized Adjoint Method for solution of the advection-dispersion equation
R. W. Healy, T.F. Russell
1993, Water Resources Research (29) 2399-2413
A new mass-conservative method for solution of the one-dimensional advection-dispersion equation is derived and discussed. Test results demonstrate that the finite-volume Eulerian-Lagrangian localized adjoint method (FVELLAM) outperforms standard finite-difference methods, in terms of accuracy and efficiency, for solute transport problems that are dominated by advection. For dispersion-dominated problems, the performance...
Simulation and mapping of soil-water conditions in the Great Plains
R. B. Zelt, J. T. Dugan
1993, Water Resources Bulletin (29) 939-948
Soil-water conditions provide valuable insight into the hydrologic system in an area. A soil-water balance quantitatively summarizes soil-water conditions and is based on climatic, soil, and vegetation characteristics that vary spatially and temporally. Soil-water balances in the Great Plains of the central United States were simulated for 1951-1980. Results of...
Hydrology and chemistry of groundwater and seasonal ponds in the Atlantic Coastal Plain in Delaware, USA
P. J. Phillips, R. J. Shedlock
1993, Journal of Hydrology (141) 157-178
The hydrochemistry of small seasonal ponds was investigated by studying relations between ground-water and surface water in a forested Coastal Plain drainage basin. Observation of changes in the water table in a series of wells equipped with automatic water-level recorders showed that the relation between water-table configuration and basin topography...
Seasonal relationships between planktonic microorganisms and dissolved organic material in an alpine stream
Diane M. McKnight, R. L. Smith, R.A. Harnish, C.L. Miller, K.E. Bencala
1993, Biogeochemistry (21) 39-59
The relationships between the abundance and activity of planktonic, heterotrophic microorganisms and the quantity and characteristics of dissolved organic carbon (DOC) in a Rocky Mountain stream were evaluated. Peak values of glucose uptake, 2.1 nmol L−1 hr−1, and glucose concentration, 333 nM, occurred during spring snowmelt when the water temperature...
Crude oil in a shallow sand and gravel aquifer—I. Hydrogeology and inorganic geochemistry
P.C. Bennett, D.E. Siegel, M.J. Baedecker, M. F. Hult
1993, Applied Geochemistry (8) 529-549
Changes in the distribution of inorganic solutes in a shallow ground water contaminated by crude oil document a series of geochemical reactions initiated by biodegradation of the oil. Upgradient of an oil body floating on the water table, oxidation of oil to carbonic acid dissolves carbonate minerals in the aquifer...
Using borehole geophysics and cross-borehole flow testing to define hydraulic connections between fracture zones in bedrock aquifers
Frederick L. Paillet
1993, Journal of Applied Geophysics (30) 261-279
Nearly a decade of intensive geophysical logging at fractured rock hydrology research sites indicates that geophysical logs can be used to identify and characterize fractures intersecting boreholes. However, borehole-to-borehole flow tests indicate that only a few of the apparently open fractures found to intersect boreholes conduct flow under test conditions....
Manganese minerals and associated fine particulates in the streambed of Pinal Creek, Arizona, U.S.A.: a mining-related acid drainage problem
Carol J. Lind, J.D. Hem
1993, Applied Geochemistry (8) 67-80
The Pinal creek drainage basin in Arizona is a good example of the principal non-coal source of mining-related acid drainage in the U.S.A., namely copper mining. Infiltration of drainage waters from mining and ore refining has created an acid groundwater plume that has reacted with calcite during passage through the...
Prediction by regression and intrarange data scatter in surface-process studies
T.J. Toy, W. R. Osterkamp, K.G. Renard
1993, Environmental Geology (22) 121-128
Modeling is a major component of contemporary earth science, and regression analysis occupies a central position in the parameterization, calibration, and validation of geomorphic and hydrologic models. Although this methodology can be used in many ways, we are primarily concerned with the prediction of values for one variable from another...
Tidal, Residual, Intertidal Mudflat (TRIM) Model and its Applications to San Francisco Bay, California
R. T. Cheng, V. Casulli, J. W. Gartner
1993, Estuarine, Coastal and Shelf Science (36) 235-280
A numerical model using a semi-implicit finite-difference method for solving the two-dimensional shallow-water equations is presented. The gradient of the water surface elevation in the momentum equations and the velocity divergence in the continuity equation are finite-differenced implicitly, the remaining terms are finite-differenced explicitly. The convective terms are treated using...
A brief history of the American radium industry and its ties to the scientific community of its early twentieth century
E. R. Landa
1993, Environment International (19) 503-508
Federally funded remedial action projects are presently underway in New Jersey and Colorado at sites containing 226Ra and other radionuclides from radium-uranium ore extraction plants that operated during the early twentieth century. They are but the latest chapter in the story of an American industry that emerged and perished in...
Use of principal-component, correlation, and stepwise multiple-regression analyses to investigate selected physical and hydraulic properties of carbonate-rock aquifers
C. Erwin Brown
1993, Journal of Hydrology (147) 169-195
Correlation analysis in conjunction with principal-component and multiple-regression analyses were applied to laboratory chemical and petrographic data to assess the usefulness of these techniques in evaluating selected physical and hydraulic properties of carbonate-rock aquifers in central Pennsylvania. Correlation and principal-component analyses were used to establish relations and associations among variables,...
Flood elevation limits in the rocky mountains
Robert D. Jarrett
1993, Conference Paper, Proceedings of the Symposium on Engineering Hydrology
An analysis of 77,987 station-years of streamflow-gaging station data from 3,748 stations in the Rocky Mountains indicates that there is a latitude-dependent elevation limit to substantial rainfall-produced flooding. The elevation limit ranges from about 1,650 m in Montana to about 2,350 m in New Mexico. Above this elevation limit, large...
Characterizing the hydrogeologic framework of the Death Valley region, Southern Nevada and California
Claudia Faunt, Frank D'Agnese, Joe S. Downey, A. Keith Turner
1993, Conference Paper, High Level Radioactive Waste Management
Three-dimensional (3-D) hydrogeologic modeling of the complex geology of the Death Valley region requires the application of a number of Geoscientific Information System (GSIS) techniques. This study, funded by United States Department of Energy as a part of the Yucca Mountain Project, focuses on an area of approximately 100,000 square...
Selected precipitation characteristics in Antelope Valley, Mojave Desert, CA
James C. Blodgett, Iraj Nasseri
1993, Conference Paper, Proceedings of the Symposium on Engineering Hydrology
An urban hydrology study currently in progress in Antelope Valley, California, includes the collection and analyses of precipitation and runoff data. Storms in Antelope Valley are most prevalent during the months of December, January, February, and March, but major storms have occurred during all months of the year except April,...
Crude oil in a shallow sand and gravel aquifer-II. Organic geochemistry
R.P. Eganhouse, M.J. Baedecker, I.M. Cozzarelli, G. R. Aiken, K. A. Thorn, T.F. Dorsey
1993, Applied Geochemistry (8) 551-567
Crude oil spilled from a pipeline break in a remote area of north-central Minnesota has contaminated a shallow glacial outwash aquifer. Part of the oil was sprayed over a large area to the west of the pipeline and part of it accumulated...
Tectonic characterization of a potential high-level nuclear waste repository at Yucca Mountain, Nevada
John W. Whitney, Dennis W. O’Leary
1993, Conference Paper, Dynamic Analysis and Design Considerations for High-Level Nuclear Waste Repositories
Tectonic characterization of a potential high-level nuclear waste repository at Yucca Mountain, Nevada, is needed to assess seismic and possible volcanic hazards that could affect the site during the preclosure (next 100 years) and the behavior of the hydrologic system during the postclosure (the following 10,000 years) periods. Tectonic characterization...
Analysis of flow in an observation well intersecting a single fracture
P.A. Lapcevic, K.S. Novakowski, Frederick L. Paillet
1993, Journal of Hydrology (151) 229-239
A semi-analytical model is developed to determine transmissivity and storativity from the interpretation of transient flow in an observation well due to pumping in a source well where the two wells are connected by a single fracture. Flow rate can be determined using a heat-pulse flowmeter located above the intersection...