A 3D, finite element model for baroclinic circulation on the Vancouver Island continental shelf
R. A. Walters, M.G.G. Foreman
1992, Journal of Marine Systems (3) 507-518
This paper describes the development and application of a 3-dimensional model of the barotropic and baroclinic circulation on the continental shelf west of Vancouver Island, Canada. A previous study with a 2D barotropic model and field data revealed that several tidal constituents have a significant baroclinic component (the K1 in...
Determination of subsurface fluid contents at a crude-oil spill site
K.M. Hess, W.N. Herkelrath, H.I. Essaid
1992, Journal of Contaminant Hydrology (10) 75-96
Measurement of the fluid-content distribution at sites contaminated by immiscible fluids, including crude oil, is needed to better understand the movement of these fluids in the subsurface and to provide data to calibrate and verify numerical models and geophysical methods. A laboratory...
Dioctahedral smectite reactions at elevated temperatures: Effects of K-availability, Na/K ratio and ionic strength
Gene Whitney
1992, Applied Clay Science (7) 97-112
Hydrothermal experiments were conducted to measure the effects of K availability, Na/K ratio and ionic strength in chloride solutions on the rate and extent of the reaction of smectite to interstratified illite/smectite. The < 2 μm fraction of a bentonite was treated hydrothermally at temperatures of 200, 250, 300, 350, 400 and...
The structure, dynamics, and chemical composition of noneruptive plumes from Mount St. Helens, 1980-1988
K.A. McGee
1992, Journal of Volcanology and Geothermal Research (51) 269-282
From May 1980 to September 1988, more than 1000 fixed-wing aircraft flights were made with a correlation spectrometer to measure the sulfur dioxide flux from Mount St. Helens volcano. These flights also provided valuable data on the structure and dynamics of noneruptive plumes emanating from Mount St. Helens. During 1980...
Geothermal gas compositions in yellowstone National Park, USA
D.S. Sheppard, A.H. Truesdell, C. J. Janik
1992, Journal of Volcanology and Geothermal Research (51) 79-93
Gas samples collected between 1974 and 1986 have been analysed for the ten major components. Samples have been collected almost exclusively from the tops of pools, which has degraded the value of the data, and limited inter-comparisons to the relatively insoluble components, Ar, N2, CH4, H2 and He. A general...
Sr-Isotope record of Quaternary marine terraces on the California coast and off Hawaii
K.R. Ludwig, D.R. Muhs, K. R. Simmons, J.G. Moore
1992, Quaternary Research (37) 267-280
Strontium-isotopic ratios of dated corals have been obtained from submerged reefs formed during Quaternary glacial periods off the Hawaiian islands. These data, combined with data from deep-sea sediments, tightly constrain the secular variation of marine 87Sr 86Sr for the past 800,000 yr. Although long-term trends are apparent, no significant...
The dynamic relationship between ground water and the Columbia River: Using deuterium and oxygen-18 as tracers
K. A. McCarthy, W. D. McFarland, J.M. Wilkinson, L. D. White
1992, Journal of Hydrology (135) 1-12
Deuterium and oxygen-18 were used as natural tracers to investigate the hydraulic relationship between the Columbia River and the Blue Lake gravel aquifer near Portland, Oregon. A time series of stable-isotope data collected from surface and ground waters during a March 1990 aquifer test confirms that the river and aquifer...
Ground water chemistry and geochemical modeling of water-rock interactions at the Osamu Utsumi mine and the Morro do Ferro analogue study sites, Poços de Caldas, Minas Gerais, Brazil
D. Kirk Nordstrom, R.H. McNutt, I. Puigdomenech, John A.T. Smellie, M. Wolf
1992, Journal of Geochemical Exploration (45) 249-287
Surface and ground waters, collected over a period of three years from the Osamu Utsumi uranium mine and the Morro do Ferro thorium/rare-earth element (Th/REE) deposits, were analyzed and interpreted to identify the major hydrogeochemical processes. These results provided information on the current geochemical evolution of ground...
Evidence for the reversal of gradients in the uppermost parts of silicic magma reservoirs
W. A. Duffield, J. Ruiz
1992, Geology (20) 1115-1118
Evidence from large-volume ignimbrites indicates that the source-magma reservoirs for most of these voluminous silicic pyroclastic deposits contained monotonic vertical chemical gradients at the time of eruption. However, gradients from a large-volume magma reservoir that produced a group of penecontemporaneous silicic lava domes,...
Lead isotopes in iron and manganese oxide coatings and their use as an exploration guide for concealed mineralization
B.L. Gulson, S. E. Church, K.J. Mizon, A. L. Meier
1992, Applied Geochemistry (7) 495-511
Lead isotopes from Fe and Mn oxides that coat stream pebbles from around the Mount Emmons porphyry molybdenum deposit in Colorado were studied to assess the feasibility of using Pb isotopes to detect concealed mineral deposits. The Fe/Mn oxide coatings were analyzed to determine their elemental concentrations using ICP-AES. The...
Two-dimensional circulation modeling of the Pamlico River estuary, North Carolina
G. L. Giese, Jerad Bales
1992, Conference Paper
A two dimensional, vertically averaged, unsteady flow model was applied to a 50- kilometer reach of the Pamlico River estuary, North Carolina. The model computational grid, which consists of about 16,000 square cells, each 200 meters on a side, was developed from more than one million depth soundings. Information from...
Study of salt transport processes in Delaware Bay
Roy Walters
1992, Conference Paper
The study described here is a subset of a broader climate-related study, and is focused primarily on salinity intrusion into Delaware Bay and River. Given changes in freshwater discharge into the Delaware River as determined from the larger study, and given probable sea level rise estimates, the purpose here is...
Energy budgets and resistances to energy transport in sparsely vegetated rangeland
William D. Nichols
1992, Agricultural and Forest Meteorology (60) 221-247
Partitioning available energy between plants and bare soil in sparsely vegetated rangelands will allow hydrologists and others to gain a greater understanding of water use by native vegetation, especially phreatophytes. Standard methods of conducting energy budget studies result in measurements of latent and sensible heat fluxes above the plant canopy...
Electromagnetic methods for mapping freshwater lenses on Micronesian atoll islands
S. S. Anthony
1992, Journal of Hydrology (137) 99-111
The overall shape of freshwater lenses can be determined by applying electromagnetic methods and inverse layered-earth modeling to the mapping of atoll island freshwater lenses. Conductivity profiles were run across the width of the inhabited islands at Mwoakilloa, Pingelap, and Sapwuahfik atolls of the Pohnpei State, Federated States...
Statistical analysis of the radon-222 potential of rocks in Virginia, U.S.A.
C. Erwin Brown, D.G. Mose, G.W. Mushrush, C.E. Chrosniak
1992, Environmental Geology and Water Sciences (19) 193-203
More than 3,200 indoor radon-222 (222Rn) measurements were made seasonally in an area of about 1,000 square kilometers of the Coastal Plain and Piedmont physiographic provinces in Virginia, U.S.A. Results of these measurements indicate that some geological units are associated, on the average, with twice as much indoor222Rn as other...
Implementation of softcopy photogrammetric workstations at the US Geological Survey
C.D. Skalet, G.Y.G. Lee, L. J. Ladner
1992, Photogrammetric Engineering and Remote Sensing (58) 57-63
The US Geological Survey has provided the Nation with primary quadrangle maps and map products for the last 50 years. The Survey recently completed initial coverage of the conterminous United States and Hawaii at 1:24 000 scale. In Alaska, complete coverage exists at 1:63 360 scale. Effort is underway to...
Geochemical evolution of Jurassic diorites from the Bristol Lake region, California, USA, and the role of assimilation
E.D. Young, J. L. Wooden, Y.-N. Shieh, D. Farber
1992, Contributions to Mineralogy and Petrology (110) 68-86
Late Jurassic dioritic plutons from the Bristol Lake region of the eastern Mojave Desert share several geochemical attributes with high-alumina basalts, continental hawaiite basalts, and high-K are andesites including: high K2O concentrations; high Al2O3 (16-19 weight %); elevated Zr/TiO2; LREE (light-rare-earth-element) enrichment (La/YbCN=6.3-13.3); and high Nb. Pearce element ratio analysis...
Residence times in river basins as determined by analysis of long-term tritium records
R. L. Michel
1992, Journal of Hydrology (130) 367-378
The US Geological Survey has maintained a network of stations to collect samples for the measurement of tritium concentrations in precipitation and streamflow since the early 1960s. Tritium data from outflow waters of river basins draining 4500–75000 km2 are used to determine average residence times of water within the basins. The...
Rhenium-osmium isotope systematics in meteorites I: Magmatic iron meteorite groups IIAB and IIIAB
J. W. Morgan, R.J. Walker, J. N. Grossman
1992, Earth and Planetary Science Letters (108) 191-202
Using resonance ionization mass spectrometry (RIMS), Re and Os abundances were determined by isotope dilution (ID) and 187Os/186Os ratios measured in nineteen iron meteorites: eight from group IIAB, ten from group IIIAB, and Treysa (IIIB anomalous). Abundances range from 1.4 to 4800...
Phase relations in the system NaCl-KCl-H2O: IV. Differential thermal analysis of the sylvite liquidus in the KCl-H2O binary, the liquidus in the NaCl-KCl-H2O ternary, and the solidus in the NaCl-KCl binary to 2 kb pressure, and a summary of experimental data for thermodynamic-PTX analysis of solid-liquid equilibria at elevated P-T conditions
I.-M. Chou, S.M. Sterner, Kenneth S. Pitzer
1992, Geochimica et Cosmochimica Acta (56) 2281-2293
The sylvite liquidus in the binary system KCl-H2O and the liquidus in the ternary system NaCl-KCl-H2O were determined by using isobaric differential thermal analysis (DTA) cooling scans at pressures up to 2 kbars. Sylvite solubilities along the three-phase curve in the binary system KCl-H2O were obtained by the intersection of...
Hydrogeochemical exploration of geothermal prospects in the Tecuamburro Volcano region, Guatemala
C. J. Janik, F. Goff, L. Fahlquist, A.I. Adams, Roldan M. Alfredo, S.J. Chipera, P.E. Trujillo, D. Counce
1992, Geothermics (21) 447-481
Chemical and isotopic analyses of thermal and nonthermal waters and of gases from springs and fumaroles are used to evaluate the geothermal potential of the Tecuamburro Volcano region, Guatemala. Chemically distinct geothermal surface manifestations generally occur in separate hydrogeologic areas within this 400 km2 region: low-pressure fumaroles with temperatures near local...
Experimental study of iron-chloride complexing in hydrothermal fluids
J.B. Fein, J.J. Hemley, W. M. d’Angelo, A. Komninou, D.A. Sverjensky
1992, Geochimica et Cosmochimica Acta (56) 3179-3190
Mineral assemblage solubilities were measured in cold-seal pressure vessels as a function of pressure, temperature, and potassium chloride concentration in order to determine the nature and thermodynamic properties of iron-chloride complexes under hydrothermal conditions. The assemblage pyritepyrrhotite-magnetite was used to buffer ƒS2">ƒS2 and <span...
A model for the assessment of aquifer contamination potential based on regional geologic framework
D. R. Soller, R. C. Berg
1992, Environmental Geology and Water Sciences (19) 205-213
The texture and three-dimensional framework of geologic materials should be considered in assessments of groundwater's vulnerability to contamination because geology controls the movement of contaminants and groundwater and influences groundwater quality. Contaminants are introduced into, transmitted through, and stored by geologic materials. We present a model that identifies aquifers and...
Interference fringes on GLORIA side-scan sonar images from the Bering Sea and their implications
Q.J. Huggett, A. K. Cooper, M. L. Somers, A.R. Stubbs
1992, Marine Geophysical Research (14) 47-63
GLORIA side-scan sonographs from the Bering Sea Basin show a complex pattern of interference fringes sub-parallel to the ship's track. Surveys along the same trackline made in 1986 and 1987 show nearly identical patterns. It is concluded from this that the interference patterns are caused by features in the shallow...
Simultaneous parameter estimation and contaminant source characterization for coupled groundwater flow and contaminant transport modelling
B.J. Wagner
1992, Journal of Hydrology (135) 275-303
Parameter estimation and contaminant source characterization are key steps in the development of a coupled groundwater flow and contaminant transport simulation model. Here a methodologyfor simultaneous model parameter estimation and source characterization is presented. The parameter estimation/source characterization inverse model combines groundwater flow and contaminant transport simulation with non-linear maximum...