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Methane production and consumption monitored by stable H and C isotope ratios at a crude oil spill site, Bemidji, Minnesota
Kinga Revesz, Tyler B. Coplen, Mary J. Baedecker, Pierre D. Glynn
1995, Applied Geochemistry (10) 505-516
Stable isotopic ratios of C and H in dissolved CH4 and C in dissolved inorganic C in the ground water of a crude-oil spill near Bemidji, Minnesota, support the concept of CH4production by acetate fermentation with a contemporaneous increase in HCO3−concentration. Methane concentrations in the saturated zone decrease from 20.6...
Volcanic gas
Kenneth A. McGee, Terrance M. Gerlach
1995, Open-File Report 95-85
In Roman mythology, Vulcan, the god of fire, was said to have made tools and weapons for the other gods in his workshop at Olympus. Throughout history, volcanoes have frequently been identified with Vulcan and other mythological figures. Scientists now know that the “smoke" from volcanoes, once attributed by poets...
Postflood occurrence of selected agricultural chemicals and volatile organic compounds in near-surface unconsolidated aquifers in the upper Mississippi River basin, 1993
Dana W. Kolpin, E. Michael Thurman
1995, Circular 1120-G
The historic stream flooding and intense rainfall across the upper Mississippi River Basin during summer 1993 had an immediate effect on near-surface unconsolidated aquifers by raising the water levels closer to the land surface . The objective of this study was to determine if this flooding also had immediate effects...
Lithofacies and palynostratigraphy of some Cretaceous and Paleocene rocks, Surghar and Salt Range coal fields, northern Pakistan
Peter D. Warwick, Shahid Javed, S. Tahir A. Mashhadi, Tariq Shakoor, Asrar M. Khan, A. Latif Khan
1995, Bulletin 2096
The stratigraphic relation between the Cretaceous generally non-coal-bearing Lumshiwal Formation (64 to 150 m thick) and the Paleocene coal-bearing Hangu Formation (5 to 50 m thick) in the Surghar Range of north-central Pakistan is complex. Both formations contain remarkably similar lithofacies: one or two types of sandstone lithofacies; a combined...
Intraglacial volcanism in the Wells Gray–Clearwater volcanic field, east-central British Columbia, Canada
C.J. Hickson, James G. Moore, L. Calk, P. Metcalfe
1995, Canadian Journal of Earth Sciences (32) 838-851
Small-volume, subaerial, subaqueous and subglacial basaltic eruptions occurred in the Wells Gray–Clearwater area during Quaternary time. Part of this time, significant thicknesses of glacial ice were present. Dating of intraglacial volcanic features corroborates other evidence of an Early Pleistocene, Cordilleran-wide ice sheet. Of the intraglacial volcanoes investigated, three were studied...
Petrology of Submarine Lavas from Kilauea's Puna Ridge, Hawaii
D. A. Clague, James G. Moore, J.E. Dixon, W.B. Friesen
1995, Journal of Petrology (36) 299-349
We have studied 30 quenched tholeiitic lava flows recovered by 20 dredge hauls and one submersible dive along Puna Ridge, the submarine part of the East Rift Zone of Kilauea Volcano, Hawaii Glass grains from numerous additional flows were recovered in turbidite sands cored in the Hawaiian Trough. These quenched...
Topography of closed depressions, scarps, and grabens in the North Tharsis region of Mars: implications for shallow crustal discontinuities and graben formation
Philip A. Davis, Kenneth L. Tanaka, Matthew P. Golombek
1995, Icarus (114) 403-422
Using Viking Orbiter images, detailed photoclinometric profiles were obtained across 10 irregular depressions, 32 fretted fractures, 49 troughs and pits, 124 solitary scarps, and 370 simple grabens in the north Tharsis region of Mars. These data allow inferences to be made on the shallow crustal structure of this region. The...
Petrography, geochemistry, and depositional setting of the San Pedro and Santo Tomas coal zones: Anomalous algae-rich coals in the middle part of the Claiborne Group (Eocene) of Webb County, Texas
Peter D. Warwick, Robert W. Hook
1995, International Journal of Coal Geology (28) 303-342
Two coal zones, the San Pedro and the overlying Santo Tomas, are present for nearly 35 km in outcrop, surface and underground mines, and shallow drill holes along the strike of the middle part of the Claiborne Group (Eocene) in Webb County, Texas. A sandstone-dominated interval of 25 to 35...
Data on quantity and quality of water flowing in drainage systems of dry docks at Puget Sound Naval Shipyard, Bremerton, Washington, 1994
Edmund A. Prych
1995, Open-File Report 95-361
Data on the quantity and quality of ground water that drains into dry docks at the Puget Sound Naval Shipyard can be useful for planning environmental remediation work at the shipyard. Ground-water discharges into and total drain-water discharges from individual dry docks were computed from a single set of discharges...
A chemodynamic approach for estimating losses of target organic chemicals from water during sample holding time
P. D. Capel, S.J. Larson
1995, Chemosphere (30) 1097-1107
Minimizing the loss of target organic chemicals from environmental water samples between the time of sample collection and isolation is important to the integrity of an investigation. During this sample holding time, there is a potential for analyte loss through volatilization from the water to the headspace, sorption to the...
Oxidation of dimethylselenide by δMnO2: oxidation product and factors affecting oxidation rate
Bronwen Wang, Richard G. Burau
1995, Environmental Science & Technology (29) 1504-1510
Volatile dimethylselenide (DMSe) was transformed to a nonvolatile Se compound in a ??-MnO2 suspension. The nonvolatile product was a single compound identified as dimethylselenoxide based on its mass spectra pattern. After 24 h, 100% of the DMSe added to a ??-MnO2 suspension was converted to nonpurgable Se as opposed to...
Determination of nanogram per liter concentrations of volatile organic compounds in water by capillary gas chromatography and selected ion monitoring mass spectrometry and its use to define groundwater flow directions in Edwards Aquifer, Texas
P.M. Buszka, D.L. Rose, G. B. Ozuna, G.E. Groschen
1995, Analytical Chemistry (67) 3659-3667
A method has been developed to measure nanogram per liter amounts of selected volatile organic compounds (VOCs) including dichlorodifluoromethane, trichlorofluoromethane, cis-1,2-dichloroethene, trichloroethene, tetrachloroethene, and the isomers of dichlorobenzene in water. The method uses purge-and-trap techniques on a 100 mL sample, gas chromatography with a megabore capillary column, and electron impact,...
Techniques of contributing-area delineation for analysis of nonpoint-source contamination of Long Island, New York
P. Misut
1995, Models for assessing and monitoring groundwater quality. Proc. symposium, Boulder, 1995 (227) 31-37
Ninety shallow monitoring wells on Long Island, N.Y., were used to test the hypothesis that the correlation between the detection of volatile organic compounds (VOC's) at a well and explanatory variables representing land use, population density, and hydrogeologic conditions around the well is affected by the size and shape of...
Cooling, degassing and compaction of rhyolitic ash flow tuffs: A computational model
J.R. Riehle, T.F. Miller, R. A. Bailey
1995, Bulletin of Volcanology (57) 319-336
Previous models of degassing, cooling and compaction of rhyolitic ash flow deposits are combined in a single computational model that runs on a personal computer. The model applies to a broader range of initial and boundary conditions than Riehle's earlier model, which did not integrate heat and mass flux with...
Mantle helium in ground waters of eastern North America: Time and space constraints on sources
T. Torgersen, S. Drenkard, M. Stute, P. Schlosser, A. Shapiro
1995, Geology (23) 675-678
Mantle helium in continental environments is generally considered to be the result of active volcanism and/or active extension. The latest episodes of volcanism in northeastern North America are the track of the New England hotspot (95–190 Ma) and the closure of the Iapetus sea (before 300 Ma). Thus, the identification...
Occurrence of active and inactive herbicide ingredients at selected sites in Iowa
W. Wang, M. Liszewski, R. Buchmiller, K. Cherryholmes
1995, Water, Air, & Soil Pollution (83) 21-35
The objective of this study was to investigate the occurrence of herbicide active and inactive ingredients (primarily volatile organic compounds) at four selected sites in Iowa representing drain tiles, observation wells, or lysimeters. Water samples were collected monthly and bi-monthly before and after herbicide applications in 1991, respectively. They...
Aerodynamic measurements of methyl bromide volatilization from tarped and nontarped fields
M.S. Majewski, M.M. McChesney, J.E. Woodrow, J.H. Prueger, J.N. Seiber
1995, Journal of Environmental Quality (24) 742-752
Methyl bromide (MeBr) is used extensively in agriculture as a soil fumigant and there is growing concern over the role it may play in the depletion of stratospheric ozone. Methyl bromide is applied using various techniques and very little is known about how much of the...
Denver's urban ground-water quality: Nutrients, pesticides, and volatile organic compounds
Breton W. Bruce
1995, Fact Sheet 106-95
A recent study by the U.S. Geological Survey (USGS) under the National Water-Quality Assessment (NAWQA) program characterized the ground-water quality in a part of the Denver, Colorado, metropolitan area. The study provides an assessment of water-quality conditions in an alluvial aquifer that drains into the South Platte River. Thirty wells...
Infiltration and quality of water for two arroyo channels, Albuquerque, New Mexico, 1988-92
Carole L. Thomas
1995, Water-Resources Investigations Report 95-4070
Selected reaches of Grant Line Arroyo and Tijeras Arroyo in Albuquerque, New Mexico, were studied to collect information about the amount and quality of infiltration through arroyo channels. Infiltration rate was calculated for selected reaches of Grant Line Arroyo and Tijeras Arroyo based on instantaneous streamflow-loss volumes, wetted channel area, and instantaneous...
Toxicity of metal-contaminated sediments from the upper Clark Fork River, Montana, to aquatic invertebrates and fish in laboratory exposures
Nile E. Kemble, William G. Brumbaugh, Eric L. Brunson, F. James Dwyer, Christopher G. Ingersoll, Dave P. Monda, Daniel F. Woodward
1994, Environmental Toxicology and Chemistry (13) 1985-1997
Sediments of the upper Clark Fork River, from the Butte and Anaconda area to Milltown Reservoir (230 km downstream), are contaminated with As, Cd, Cu, Pb, Mn, and Zn primarily from mining activities. The toxicity of pore water from these sediments was determined using Daphnia magna (48-h exposure), rainbow trout (96-h...
Hydrogeology and ground-water quality of northern Bucks County, Pennsylvania
Ronald A. Sloto, Curtis L. Schreffler
1994, Water-Resources Investigations Report 94-4109
The 187-square mile study area is in the Triassic-Jurassic Newark Basin. Most of the area is underlain by sedimentary rocks of Upper Triassic age (74 percent) and intrusive diabase of Jurassic age (12 percent) and includes two southwest-northeast trending valleys underlain by carbonate and crystalline rock. Ground water in the sedimentary...