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Page 1719, results 42951 - 42975

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Publication Extents

Not all publications have extents, not all extents are completely accurate
Worldwide distribution of subaquatic gas hydrates
K.A. Kvenvolden, G.D. Ginsburg, V.A. Soloviev
1993, Geo-Marine Letters (13) 32-40
Sediments containing natural gas hydrates occur worldwide on continental and insular slopes and rises of active and passive margins, on continental shelves of polar regions, and in deep-water (> 300 m) environments of inland lakes and seas. The potential amount of methane in natural gas hydrates is enormous, with current...
A geochemical atlas of North Carolina, USA
J.C. Reid
1993, Journal of Geochemical Exploration (47) 11-27
A geochemical atlas of North Carolina, U.S.A., was prepared using National Uranium Resource Evaluation (NURE) stream-sediment data. Before termination of the NURE program, sampling of nearly the entire state (48,666 square miles of land area) was completed and geochemical analyses were obtained.The NURE data are applicable to mineral exploration, agriculture,...
Variations in northern Sierra Nevada streamflow. Implications of climate change
A. Pupacko
1993, Water Resources Bulletin (29) 283-290
Historical records of streamflow for an eastward- and a westward-draining stream in the northern Sierra Nevada have been analyzed for evidence of changes in runoff characteristics and patterns of variability. A trend of increasing and more variable winter streamflow began in the mid-1960s. Mean monthly streamflow during December through March...
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...
Refinement of the evaluation of the role of CO2 in modifying estimates of the pressure of epithermal mineralization
P.B. Barton, I.-M. Chou
1993, Economic Geology (88) 873-884
Pressure is the most important of the intensive parameters for relating epithermal mineralization to the geologic setting. This paper describes the limitations on pressure (and therefore depth) of mineralization that may reasonably be derived from simple observations of the behavior of fluid inclusions (i.e., the existence of ice or CO 2 clathrate...
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...
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...
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...
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...
Flooding of Sinking Creek, Garretts Spring karst drainage basin, Jessamine and Woodford counties, Kentucky, USA
J.C. Currens, C.D.R. Graham
1993, Environmental Geology (22) 337-344
Tashamingo Subdivision in Sinking Creek karst valley, a tributary of the Garretts Spring drainage basin in Jessamine and Woodford counties, Kentucky, was flooded in February 1989. To determine the cause of flooding, the groundwater basin boundary was mapped, discharge data were measured to determine intake capacity of swallets, and hydrologic...
Calibrated models as management tools for stream-aquifer systems: The case of central Kansas, USA
M. Sophocleous, S.P. Perkins
1993, Journal of Hydrology (152) 31-56
We address the problem of declining streamflows in interconnected stream-aquifer systems and explore possible management options to address the problem for two areas of central Kansas: the Arkansas River valley from Kinsley to Great Bend and the lower Rattlesnake Creek-Quivira National Wildlife Refuge area. The approach we followed implements, calibrates,...
Pesticides in shallow groundwater in the Delmarva Peninsula
M.T. Koterba, W.S.L. Banks, R. J. Shedlock
1993, Journal of Environmental Quality (22) 500-518
A regional study of the areal and depth distribution of pesticides in shallow groundwater in the Delmarva Peninsula of Delaware, Maryland, and Virginia was done to (i) relate the pesticides detected to landscape and shallow subsurface features, and (ii) evaluate aquifer vulnerability and the potential...
Wind and tidal forcing of a buoyant plume, Mobile Bay, Alabama
R. P. Stumpf, G. Gelfenbaum, J.R. Pennock
1993, Continental Shelf Research (13) 1281-1301
AVHRR satellite imagery and in situ observations were combined to study the motion of a buoyant plume at the mouth of Mobile Bay, Alabama. The plume extended up to 30 km from shore, with a thickness of about 1 m. The inner plume, which was 3-8 m thick, moved between...
A late Pliocene to middle Pleistocene pluvial lake in Fish Lake Valley, Nevada and California
M.C. Reheis, J. L. Slate, A.M. Sarna-Wojcicki, C.E. Meyer
1993, Geological Society of America Bulletin (105) 953-967
The question of whether a pluvial lake existed in Fish Lake Valley, Nevada and California, has been debated for more than 100 yr. New stratigraphic evidence indicates that a lake did exist in this valley at intervals during late Pliocene to middle Pleistocene time. This lake may have drained northward,...
Rio Grande valley Colorado new Mexico and Texas
Sherman R. Ellis, Gary W. Levings, Lisa F. Carter, Steven F. Richey, Mary Jo Radell
1993, Water Resources Bulletin (29) 617-646
Two structural settings are found in the study unit: alluvial basins and bedrock basins. The alluvial basins can have through-flowing surface water or be closed basins. The discussion of streamflow and water quality for the surface-water system is based on four river reaches for the 750 miles of the main...
The effects of Hurricane Hugo on suspended-sediment loads, Lago Loiza Basin, Puerto Rico
A. Gellis
1993, Earth Surface Processes and Landforms (18) 505-517
In the two main tributaries that enter Lago Loiza, Rio Grande de Loiza and Rio Gurabo, 99 600 tonnes of suspended sediment was transported by 58.2??106 m3 of runoff in a 48 h period. The storm-average suspended-sediment concentration in the Rio Grande de Loiza for Hurricane Hugo was 2290 mgl-1,...
Crude oil in a shallow sand and gravel aquifer-III. Biogeochemical reactions and mass balance modeling in anoxic groundwater
M.J. Baedecker, I.M. Cozzarelli, R.P. Eganhouse, D. I. Siegel, P.C. Bennett
1993, Applied Geochemistry (8) 569-586
Crude oil floating on the water table in a sand and gravel aquifer provides a constant source of hydrocarbons to the groundwater at a site near Bemidji, Minnesota. The degradation of hydrocarbons affects the concentrations of oxidized and reduced aqueous species in the anoxic part of the contaminant plume that...
Large-scale deformation associated with ridge subduction
E.L. Geist, M. A. Fisher, D.W. Scholl
1993, Geophysical Journal International (115) 344-366
Continuum models are used to investigate the large-scale deformation associated with the subduction of aseismic ridges. Formulated in the horizontal plane using thin viscous sheet theory, these models measure the horizontal transmission of stress through the arc lithosphere accompanying ridge subduction. Modelling was used to compare the Tonga arc...
Distribution and mode of occurrence of selenium in US coals
L. Coleman, L. J. Bragg, R. B. Finkelman
1993, Environmental Geochemistry and Health (15) 215-227
Selenium excess and deficiency have been established as the cause of various health problems in man and animals. Combustion of fossil fuels, especially coal, may be a major source of the anthropogenic introduction of selenium in the environment. Coal is enriched in selenium relative to selenium's concentration in most other...
Regional flow in the Baltic Shield during Holocene coastal regression
Clifford I. Voss, Johan Andersson
1993, Groundwater (31) 989-1006
The occurrence of saline waters in the Baltic Shield in Sweden is consistent with ongoing but incomplete Holocene flushing and depends on the geometry and connectivity of conductive structures at both regional and local scales, and on the surface topography. Numerical simulation of regional...
Nonpoint source contamination of the Mississippi river and its tributaries by herbicides
W. E. Pereira, F. D. Hostettler
1993, Environmental Science & Technology (27) 1542-1552
A study of the Mississippi River and its tributaries during July-August 1991, October-November 1991, and April-May 1992 has indicated that the entire navigable reach of the river is contaminated with a complex mixture of agrochemicals and their transformation products derived from nonpoint sources. Twenty-three compounds were identified, including triazine, chloroacetanilide,...
Unique laminar-flow stability limit based shallow-water theory
Cheng-lung Chen
1993, Journal of Hydraulic Engineering (119) 816-829
Two approaches are generally taken in deriving the stability limit for the Froude number (𝐹𝑠) for laminar sheet flow: The first approach uses the Orr‐Sommerfeld equation, while the second uses the cross‐section‐averaged equations of continuity and motion. Because both approaches are based on shallow‐water theory, the values of 𝐹𝑠 obtained from both approaches should...
Evaluation of the extent of contaminated sediments in the west branch of the Grand Calumet river, Indiana-Illinois, USA
R.A. Cahill, M.T. Unger
1993, Conference Paper, Water Science and Technology
The extent of contamination in river sediments is often not rigorously evaluated. In many cases, only surface sediment samples are taken. In other cases, entire sediment cores are composited for analysis, an approach that limits the ability to identify discrete zones of contamination. In addition, few studies include information on...
The erosion of carbonate stone by acid rain: Laboratory and field investigations
P. A. Baedecker, M.M. Reddy
1993, Journal of Chemical Education (70) 104-108
One of the goals of research on the effects of acidic deposition on carbonate stone surfaces is to define the incremental impact of acidic deposition relative to natural weathering processes on the rate of carbonate stone erosion. If rain that impacts carbonate stone surfaces is resident on the surface long...
Miocene non-marine diatoms from the western Cordillera basins of northern Peru
Elisabeth Fourtainer, F. Gasse, O. Bellier, M. G. Bonhomme, I. Robles
1993, Diatom Research (8) 13-30
Diatom assemblages are documented from diatomite layers of two Miocene fluvio-lacustrine units from the basins of the western Cordillera of northern Peru: the Namora Formation and the Cajabamba Formation. Emphasis is given to taxa of particular stratigraphic interest. The diatom assemblages indicate for the Namora Formation the occurrence of swampy...