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Hydrogeology and preliminary assessment of the potential for contamination of the Memphis aquifer in the Memphis area, Tennessee
W. S. Parks
1990, Water-Resources Investigations Report 90-4092
Detailed maps of the thickness of the Jackson-upper Claibome confining unit and the altitude of the water table in the alluvium andfluvial deposits provide much new information concerning areas where downward leakage is or may be occurringfrom the water-table aquifers to theMemphrj aqutyer in the Memphis area. A detailed map of the altitude of the potentiometric surface...
Geohydrology and water quality of Kalamazoo County, Michigan, 1986-88
S. J. Rheaume
1990, Water-Resources Investigations Report 90-4028
Thick, glacial sand and gravel deposits provide most ground-water supplies in Kalamazoo County. These deposits range in thickness from 50 to about 600 feet in areas that overlie buried bedrock valleys. Most domestic wells completed at depths of less than 75 feet in the sands and gravels yield adequate water...
Preliminary delineation of contaminated water-bearing fractures intersected by open-hole bedrock wells
John Williams, Randall W. Conger
1990, Groundwater Monitoring & Remediation (10) 118-126
Contaminated water‐bearing fractures intersected by open‐hole bedrock wells were preliminarily delineated through a combination of geophysical logging, vertical‐flow measurements, and downhole water sampling as part of remedial site investigations in southeastern New York. The wells investigated range from 100 to 450 feet in depth, have only shallow surface casing, and...
Geochemistry of highly fractionated I- and S-type granites from the tin-tungsten province of western Tasmania
Wayne N. Sawka, M.T. Heizler, R. W. Kistler, B. W. Chappell
Holly J. Stein, Judith L. Hannah, editor(s)
1990, Book chapter, Ore-bearing granite systems; petrogenesis and mineralizing processes
The Devonian batholiths of western Tasmania represent a diverse assemblage of highly fractionated intrusions (70 to 77 percent SiO2) that are the products of different source materials. The Housetop batholith exhibits compositional affinities to a fluorine-rich I-type magma. The Meredith batholith also has characteristics indicative of I-type source materials. The...
Prediction of stream volatilization coefficients
Ronald E. Rathbun
1990, Journal of Environmental Engineering (116) 615-631
Equations are developed for predicting the liquid-film and gas-film reference-substance parameters for quantifying volatilization of organic solutes from streams. Molecular weight and molecular-diffusion coefficients of the solute are used as correlating parameters. Equations for predicting molecular-diffusion coefficients of organic solutes in water and air are developed, with molecular weight and...
Organic contamination of ground water at Gas Works Park, Seattle, Washington
G. L. Turney, D.F. Goerlitz
1990, Groundwater Monitoring & Remediation (10) 187-198
Gas Works Park, in Seattle, Washington, is located on the site of a coal and oil gasification plant that ceased operation in 1956. During operation, many types of wastes, including coal, tar, and oil, accumulated on-site. The park soil is currently (1986) contaminated with compounds such as polynuclear aromatic...
Combustion and leaching behavior of elements in the argonne premium coal samples
R. B. Finkelman, C.A. Palmer, M.R. Krasnow, P. J. Aruscavage, G.A. Sellers, F.T. Dulong
1990, Energy & Fuels (4) 755-766
Eight Argonne Premium Coal samples and two other coal samples were used to observe the effects of combustion and leaching on 30 elements. The results were used to infer the modes of occurrence of these elements. Instrumental neutron activation analysis indicates that the effects of combustion and leaching on many...
Mineralogy and geochemistry of altered rocks associated with Lemitar carbonatites, central New Mexico, U.S.A.
V. T. McLemore, P.J. Modreski
1990, LITHOS (26) 99-113
The intrusion of more than 100 Cambrian-Ordovician carbonatite dikes caused minor alteration of Proterozoic granitic and mafic rocks in the Lemitar Mountains, although hematization, carbonatization and fenitization caused extensive alteration locally. Ampibolites within 15-20 m of the carbonatite dike contacts were highly altered by carbonatization. Locally the Lemitar diorite/gabbro adjacent...
Temperature, size, and depth of the magma reservoir for the Taylor Creek Rhyolite, New Mexico
W. A. Duffield, du Bray
1990, American Mineralogist (75) 1059-1070
The 55 km3 mid-Tertiary Taylor Creek Rhyolite in southwestern New Mexico consists of 20 lava domes and flows. This rhyolite is metaluminous to weakly peraluminous. Compositional zonation in feldspar phenocrysts is very minor and nonsystematic. The compositions of each feldspar species vary little throughout the suite of analyzed samples. This...
Volcanism in the Sumisu Rift, I. Major element, volatile, and stable isotope geochemistry
A.G. Hochstaedter, J.B. Gill, M. Kusakabe, S. Newman, M. Pringle, B. Taylor, P. Fryer
1990, Earth and Planetary Science Letters (100) 179-194
A bimodal volcanic suite with KAr ages of 0.05–1.40 Ma was collected from the Sumisu Rift using alvin. These rocks are contemporaneous with island arc tholeiite lavas of the Izu-Ogasawara arc 20 km to the east, and provide a present day example of volcanism associated with...
High-density volatiles in the system C-O-H-N for the calibration of a laser Raman microprobe
I.-M. Chou, J. D. Pasteris, J. C. Seitz
1990, Geochimica et Cosmochimica Acta (54) 535-543
Three methods have been used to produce high-density volatiles in the system C-O-H-N for the calibration of a laser Raman microprobe (LRM): synthetic fluid-inclusion, sealed fused-quartz-tube, and high-pressure-cell methods. Because quantitative interpretation of a Raman spectrum of mixed-volatile fluid inclusions requires accurate knowledge of pressure- and composition-sensitive Raman scattering efficiencies...
Comment on "The surface of lo: A new model" by Bruce Hapke
A. S. McEwen, J. I. Lunine
1990, Icarus (84) 268-274
Hapke (1989, Icarus 79, 56–74) proposed that the surface of Io is dominantly basaltic with thin coatings of polysulfur oxide, S2O, ad SO,2. However, observations and models of the active volcanism indicate that volatiles such as sulfur and SO2 must be more abundant than envisioned by Hapke....
The Taylor Creek Rhyolite of New Mexico: a rapidly emplaced field of lava domes and flows
W. A. Duffield, G. B. Dalrymple
1990, Bulletin of Volcanology (52) 475-487
The Tertiary Taylor Creek Rhyolite of southwest New Mexico comprises at least 20 lava domes and flows. Each of the lavas was erupted from its own vent, and the vents are distributed throughout a 20 km by 50 km area. The volume of the rhyolite and genetically associated pyroclastic deposits...
Production of sulfur gases and carbon dioxide by synthetic weathering of crushed drill cores from the Santa Cruz porphyry copper deposit near Casa Grande, Pinal County, Arizona
M. E. Hinkle, J. L. Ryder, S. J. Sutley, T. Botinelly
1990, Journal of Geochemical Exploration (38) 43-67
Samples of ground drill cores from the southern part of the Santa Cruz porphyry copper deposit, Casa Grande, Arizona, were oxidized in simulated weathering experiments. The samples were also separated into various mineral fractions and analyzed for contents of metals and...
Evaluation of gases, condensates, and SO2 emissions from Augustine volcano, Alaska: the degassing of a Cl-rich volcanic system
R.B. Symonds, William I. Rose Jr., T.M. Gerlach, Paul H. Briggs, R.S. Harmon
1990, Bulletin of Volcanology (52) 355-374
After the March-April 1986 explosive eruption a comprehensive gas study at Augustine was undertaken in the summers of 1986 and 1987. Airborne COSPEC measurements indicate that passive SO2 emission rates declined exponentially during this period from 380??45 metric tons/day (T/D) on 7/24/86 to 27??6 T/D on 8/24/87. These data are...
Recent crustal subsidence at Yellowstone Caldera, Wyoming
D. Dzurisin, J.C. Savage, R.O. Fournier
1990, Bulletin of Volcanology (52) 247-270
Following a period of net uplift at an average rate of 15??1 mm/year from 1923 to 1984, the east-central floor of Yellowstone Caldera stopped rising during 1984-1985 and then subsided 25??7 mm during 1985-1986 and an additional 35??7 mm during 1986-1987. The average horizontal strain rates in the northeast part...
Water-quality data for the Potomac-Raritan-Magothy aquifer system in the northern coast plain of New Jersey, 1923-86
Douglas A. Harriman, Daryll A. Pope, Alison D. Gordon
1989, Report
Ground-water-quality data for the upper and middle aquifers of the Potomac-Raritan-Magothy aquifer system in Middlesex and Monmouth Counties are compiled for the period 1923-86. A total of 330 wells were sampled: 192 wells in the upper aquifer and 138 wells in the middle aquifer. Most of the complete water-quality analyses...
Hydrogeology of Wood County, Wisconsin
W. G. Batten
1989, Wisconsin Geological & Natural History Survey Information Circular 60
The presence of low-permeability Precambrian rocks near land surface limits ground-water availability in the northern two-thirds of Wood County. Sand and gravel deposits provide large amounts of water (more than 500 gallons per minute) to some wells in the southeastern part of the county. Fine-grained unconsolidated deposits generally are less...
Gas transport in unsaturated porous media: The adequacy of Fick's law
D.C. Thorstenson, D.W. Pollock
1989, Reviews of Geophysics (27) 61-78
The increasing use of natural unsaturated zones as repositories for landfills and disposal sites for hazardous wastes (chemical and radioactive) requires a greater understanding of transport processes in the unsaturated zone. For volatile constituents an important potential transport mechanism is gaseous diffusion. Diffusion, however, cannot be treated as an independent...
Dikes, joints, and faults in the upper mantle
H. G. Wilshire, S. H. Kirby
1989, Tectonophysics (161) 23-31
Three different types of macroscopic fractures are recognized in upper-mantle and lower-crustal xenoliths in volcanic rocks from around the world: 1. (1) joints that are tensile fractures not occupied by crystallized magma products 2. (2) dikes that are tensile fractures occupied by mafic magmas crystallized to pyroxenites, gabbros or hydrous-mineral-rich...
Appraisal of ground-water quality in the Bunker Hill Basin of San Bernardino Valley, California
L. F. Duell Jr., R. A. Schroeder
1989, Water-Resources Investigations Report 88-4203
Water samples were collected from 47 wells and analyzed for concentration of major inorganic ions, nitrogen species, and volatile (purgeable) organic priority pollutants to assess groundwater quality in the Bunker Hill basin, California. Data were supplemented with additional analysis of nitrate, tetrachloroethylene, and trichloroethylene made by other agencies. The organic...
Biannual water-resources review, White Sands Missile Range, New Mexico, 1986 and 1987
Robert G. Myers, Steven C. Sharp
1989, Open-File Report 89-49
Hydrologic data were collected at White Sands Missile Range, New Mexico in 1986 and 1987. The total groundwater withdrawal in 1986 was 565,462,500 gal and in 1987 it was 620,492,000 gal. The total groundwater withdrawal was 110,971,300 gal less in 1986 than in 1985, but 55,029,500 gal more in 1987...
Inorganic and organic ground-water chemistry in the Canal Creek area of Aberdeen Proving Ground, Maryland
M.M. Lorah, D.A. Vroblesky
1989, Water-Resources Investigations Report 89-4022
Groundwater chemical data were collected from November 1986 through April 1987 in the first phase of a 5-year study to assess the possibility of groundwater contamination in the Canal Creek area of Aberdeen Proving Ground, Maryland. Water samples were collected from 87 observation wells screened in Coastal Plain sediments; 59...