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Page 1203, results 30051 - 30075

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Formation evaluation of gas hydrate-bearing marine sediments on the Blake Ridge with downhole geochemical log measurements
T. S. Collett, R. F. Wendlandt
2000, Conference Paper, Proceedings of the Ocean Drilling Program: Scientific Results
The analyses of downhole log data from Ocean Drilling Program (ODP) boreholes on the Blake Ridge at Sites 994, 995, and 997 indicate that the Schlumberger geochemical logging tool (GLT) may yield useful gas hydrate reservoir data. In neutron spectroscopy downhole logging, each element has a characteristic gamma ray that...
Interaction of infection with Renibacterium salmoninarum and physical stress in juvenile chinook salmon: Physiological responses, disease progression, and mortality
M.G. Mesa, A.G. Maule, C.B. Schreck
2000, Transactions of the American Fisheries Society (129) 158-173
We experimentally infected juvenile spring chinook salmon Oncorhynchus tshawytscha with Renibacterium salmoninarum (Rs), the causative agent of bacterial kidney disease (BKD), in order to compare the physiological responses of Rs-infected and Rs-noninfected fish to a series of multiple, acute stressors and to determine whether exposure to these stressors worsens the...
Geochemical variations in Peoria Loess of western Iowa indicate paleowinds of midcontinental North America during last glaciation
D.R. Muhs, E. Arthur Bettis III
2000, Quaternary Research (53) 49-61
Peoria Loess deposited in western Iowa during the last glacial maximum (LGM) shows distinct geochemical and particle-size variations as a function of both depth and distance east of the Missouri River. Geochemical and particle-size data indicate that Peoria Loess in western Iowa probably had two sources: the Missouri River valley,...
Uncertainty estimation for resource assessment-an application to coal
J.H. Schuenemeyer, H.C. Power
2000, Mathematical Geology (32) 521-541
The U.S. Geological Survey is conducting a national assessment of coal resources. As part of that assessment, a geostatistical procedure has been developed to estimate the uncertainty of coal resources for the historical categories of geological assurance: measured, indicated, inferred, and hypothetical coal. Data consist of spatially clustered coal thickness...
Development and evaluation of consensus-based sediment effect concentrations for polychlorinated biphenyls
Donald D. MacDonald, Lisa M. Dipinto, Jay Field, Christopher G. Ingersoll, Edward R. Long, Richard C. Swartz
2000, Environmental Toxicology and Chemistry (19) 1403-1413
Sediment-quality guidelines (SQGs) have been published for polychlorinated biphenyls (PCBs) using both empirical and theoretical approaches. Empirically based guidelines have been developed using the screening-level concentration, effects range, effects level, and apparent effects threshold approaches. Theoretically based guidelines have been developed using the equilibrium-partitioning approach. Empirically-based guidelines were classified into...
Estimating the variance and integral scale of the transmissivity field using head residual increments
Li Zheng, Stephen E. Silliman
2000, Water Resources Research (36) 1353-1358
A modification of previously published solutions regarding the spatial variation of hydraulic heads is discussed whereby the semivariogram of increments of head residuals (termed head residual increments HRIs) are related to the variance and integral scale of the transmissivity field. A first‐order solution is developed for the case of a...
Modeling the effects of snowpack on heterotrophic respiration across northern temperate and high latitude regions: Comparison with measurements of atmospheric carbon dioxide in high latitudes
A. D. McGuire, J. M. Melillo, J. T. Randerson, W.J. Parton, Martin Heimann, R.A. Meier, Joy S. Clein, D. W. Kicklighter, W. Sauf
2000, Biogeochemistry (48) 91-114
Simulations by global terrestrial biogeochemical models (TBMs) consistently underestimate the concentration of atmospheric carbon dioxide (CO2) at high latitude monitoring stations during the nongrowing season. We hypothesized that heterotrophic respiration is underestimated during the nongrowing season primarily because TBMs do not generally consider the insulative effects of snowpack on soil...
Identifying fracture‐zone geometry using simulated annealing and hydraulic‐connection data
Frederick D. Day-Lewis, Paul A. Hsieh, Steven M. Gorelick
2000, Water Resources Research (36) 1707-1721
A new approach is presented to condition geostatistical simulation of high‐permeability zones in fractured rock to hydraulic‐connection data. A simulated‐annealing algorithm generates three‐dimensional (3‐D) realizations conditioned to borehole data, inferred hydraulic connections between packer‐isolated borehole intervals, and an indicator (fracture zone or background‐K bedrock) variogram model of spatial variability. We apply...
Crustal deformation associated with glacial fluctuations in the eastern Chugach Mountains, Alaska
Jeanne Sauber, George Plafker, Bruce F. Molnia, Mark A. Bryant
2000, Journal of Geophysical Research B: Solid Earth (105) 8055-8077
The changes of the solid Earth in south central Alaska in response to two major glacial fluctuations on different temporal and spatial scales have been estimated and we evaluated their influence on the stress state and ongoing tectonic deformation of the region. During the recent (1993–1995) Bering Glacier surge, a...
Guidelines for model calibration and application to flow simulation in the Death Valley regional groundwater system
M. C. Hill, F. A. D’Agnese, C.C. Faunt
2000, Conference Paper, IAHS-AISH Publication
Fourteen guidelines are described which are intended to produce calibrated groundwater models likely to represent the associated real systems more accurately than typically used methods. The 14 guidelines are discussed in the context of the calibration of a regional groundwater flow model of the Death Valley region in the southwestern...
Colorado River sediment transport: 2. Systematic bed‐elevation and grain‐size effects of sand supply limitation
David J. Topping, David M. Rubin, Jonathan M. Nelson, Paul J. Kinzel III, Ingrid C. Corson
2000, Water Resources Research (36) 543-570
The Colorado River in Marble and Grand Canyons displays evidence of annual supply limitation with respect to sand both prior to [Topping et al, this issue] and after the closure of Glen Canyon Dam in 1963. Systematic changes in bed elevation and systematic coupled changes in suspended‐sand concentration and grain...
Effects of neck bands on survival of greater snow geese
S. Menu, J.B. Hestbeck, G. Gauthier, A. Reed
2000, Journal of Wildlife Management (64) 544-552
Neck bands are a widely used marker in goose research. However, few studies have investigated a possible negative effect of this marker on survival. We tested the effect of neck bands on the survival of adult female greater snow geese (Chen caerulescens atlantica) by marking birds with either a neck...
Using a metal detector to determine lead sinker abundance in waterbird habitat
A.E. Duerr, S. DeStefano
2000, Wildlife Society Bulletin (27) 952-958
Waterbirds have died of lead poisoning from ingesting lead fishing sinkers in the United States and Europe. Estimating abundance and distribution of sinkers in the environment will help researchers to understand the potential effects of lead poisoning from sinker ingestion. We used a metal detector to test how environmental conditions...
A comparison of delta change and downscaled GCM scenarios for three mountainous basins in the United States
L.E. Hay, R.L. Wilby, G.H. Leavesley
2000, Journal of the American Water Resources Association (36) 387-397
Simulated daily precipitation, temperature, and runoff time series were compared in three mountainous basins in the United States: (1) the Animas River basin in Colorado, (2) the East Fork of the Carson River basin in Nevada and California, and (3) the Cle Elum River basin in Washington State. Two methods...
Parent brine of the castile evaporites (Upper Permian), Texas and New Mexico
Douglas W. Kirkland, Rodger E. Denison, Walter E. Dean
2000, Journal of Sedimentary Research (70) 749-761
The Upper Permian (lower Ochoan) Castile Formation is a major evaporite sequence (∼10,000 km3) of calcite, anhydrite, and halite in west Texas and southeastern New Mexico. Traditionally the Castile brine has been considered to have been derived from seawater. This tradition has recently been challenged by two versions of the...
Spatial modeling of the geographic distribution of wildlife populations: A case study in the lower Mississippi River region
W. Ji, C. Jeske
2000, Ecological Modelling (132) 95-104
A geographic information system (GIS)-based spatial modeling approach was developed to study environmental and land use impacts on the geographic distribution of wintering northern pintails (Arias acuta) in the Lower Mississippi River region. Pintails were fitted with backpack radio transmitter packages at Catahoula Lake, LA, in October 1992-1994 and located...
Reservoir characterization of marine and permafrost associated gas hydrate accumulations with downhole well logs
T. S. Collett, Myung W. Lee
2000, Conference Paper, Annals of the New York Academy of Sciences
Gas volumes that may be attributed to a gas hydrate accumulation depend on a number of reservoir parameters, one of which, gas-hydrate saturation, can be assessed with data obtained from downhole well-logging devices. This study demonstrates that electrical resistivity and acoustic transit-time downhole log data can be used to quantify...
Formation of natural gas hydrates in marine sediments. Gas hydrate growth and stability conditioned by host sediment properties
M. B. Clennell, P. Henry, M. Hovland, J.S. Booth, W.J. Winters, M. Thomas
2000, Conference Paper, Annals of the New York Academy of Sciences
The stability conditions of submarine gas hydrates (methane clathrates) are largely dictated by pressure, temperature, gas composition, and pore water salinity. However, the physical properties and surface chemistry of the host sediments also affect the thermodynamic state, growth kinetics, spatial distributions, and growth forms of clathrates. Our model presumes that...
Identification of a basaltic component on the Martian surface from Thermal Emission Spectrometer data
P. R. Christensen, J. L. Bandfield, M. D. Smith, V.E. Hamilton, Roger N. Clark
2000, Journal of Geophysical Research: Planets (105) 9609-9621
The Mars Global Surveyor Thermal Emission Spectrometer (TES) instrument collected 4.8×106 spectra of Mars during the initial aerobraking and science‐phasing periods of the mission (September 14, 1997, through April 29, 1998). Two previously developed atmosphere‐removal models were applied to data from Cimmeria Terra (25°S, 213°W). The surface spectra derived for these...
Geochemical and mineralogical evidence from eolian sediments for northwesterly mid-Holocene paleowinds, central Kansas, USA
A.F. Arbogast, D.R. Muhs
2000, Quaternary International (67) 107-118
A prominent (4500 km2) dune field in the Great Plains is the Great Bend Sand Prairie of south-central Kansas. Dunes here overlie late Quaternary alluvium and were reactivated extensively in the late Holocene. Geomorphic and soil evidence suggests that the most likely eolian sand source is the Arkansas River valley...
Responses of stable bay-margin and barrier-island systems to Holocene sea-level highstands, western Gulf of Mexico
Robert A. Morton, Jeffrey G. Paine, Michael D. Blum
2000, Journal of Sedimentary Research (70) 478-490
The microtidal, wave-dominated coast of the western Gulf of Mexico displays a variety of Holocene geomorphic features indicating higher-than-present water levels that were previously attributed to storm processes while geoidal sea level was at its present position. Field and aerial-photograph examinations of bay margins, barrier islands, and beach-ridge plains following...
Dynamics of prey moving through a predator field: a model of migrating juvenile salmon
J.H. Petersen, D.L. DeAngelis
2000, Mathematical Biosciences (165) 97-114
The migration of a patch of prey through a field of relatively stationary predators is a situation that occurs frequently in nature. Making quantitative predictions concerning such phenomena may be difficult, however, because factors such as the number of the prey in the patch, the spatial length and velocity of...
Historical eruptions of Merapi Volcano, Central Java, Indonesia, 1768-1998
B. Voight, E.K. Constantine, S. Siswowidjoyo, R. Torley
2000, Journal of Volcanology and Geothermal Research (100) 69-138
Information on Merapi eruptive activity is scattered and much is remotely located. A concise and well-documented summary of this activity has been long needed to assist researchers and hazard-mitigation efforts, and the aim of this paper is to synthesize information from the mid-1700s to the present. A descriptive chronology is...
Detection of crystalline hematite mineralization on Mars by the Thermal Emission Spectrometer: evidence for near-surface water
P. R. Christensen, J. L. Bandfield, R. N. Clark, K.S. Edgett, V.E. Hamilton, T. Hoefen, H. H. Kieffer, R.O. Kuzmin, M. D. Lane, M. C. Malin, R.V. Morris, J.C. Pearl, R. Pearson, T. L. Roush, S. W. Ruff, M. D. Smith
2000, Journal of Geophysical Research E: Planets (105) 9623-9642
The Thermal Emission Spectrometer (TES) instrument on the Mars Global Surveyor (MGS) mission has discovered a remarkable accumulation of crystalline hematite (α-Fe2O3) that covers an area with very sharp boundaries approximately 350 by 350–750 km in size centered near 2°S latitude between 0° and 5°W longitude (Sinus Meridiani). Crystalline hematite...