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Phase relations in the system CuMoS
H. Dawei, L.L.Y. Chang, C.R. Knowles
1990, Journal of the Less-Common Metals (163) 281-286
Phase relations in the system CuMoS were studied in the temperature range 500-1000 ??C by using the conventional sealed, evacuated glass capsule technique. Reflected-light microscopy, X-ray powder diffraction and electron microprobe analysis were used for phase characterization. The chevrel-type phase, CuxMo3S4, is stable above 600??C, and forms equilibrium assemblages with...
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...
Hydrogeochemistry and stable isotopes of ground and surface waters from two adjacent closed basins, Atacama Desert, northern Chile
Charles N. Alpers, Donald O. Whittemore
1990, Applied Geochemistry (5) 719-734
The geochemistry and stable isotopes of groundwaters, surface waters, and precipitation indicate different sources of some dissolved constituents, but a common source of recharge and other constituents in two adjacent closed basins in the Atacama Desert region of northern Chile (24°15′–24°45′S). Waters from artesian wells, trenches, and ephemeral streams in...
Genetic implications of regional and temporal trends in ore fluid geochemistry of Mississippi Valley-type deposits in the Ozark region
J.G. Viets, D. L. Leach
1990, Economic Geology (85) 842-861
Fluids extracted from aqueous fluid inclusions in epigenetic gangue and ore minerals record the migration of huge volumes of highly saline fluids throughout the stratigraphic section of the Ozark region. The extracted fluids share many similarities regionally, but there are significant temporal differences which define two geochemically distinct end-member ore-forming...
Effects of ozonated-water reuse on salinity tolerance of Atlantic salmon
H. A. Poston, R.C. Williams
1990, Progressive Fish-Culturist (52) 36-40
We conducted several seasonal aquarium experiments to determine survival and body chemistry changes of Atlantic salmon (Salmo salar) after 24‐h exposures to salinities of 0, 16.5, 33, and 40‰ at 10°C. Fish transferred directly to test aquaria from an ozonated, 100‰ closed water‐reuse system at 18°C were compared with fish...
National contaminant biomonitoring program: concentrations of arsenic, cadmium, copper, lead, mercury, selenium, and zinc in U.S. Freshwater Fish, 1976–1984
Christopher J. Schmitt, William G. Brumbaugh
1990, Archives of Environmental Contamination and Toxicology (19) 731-747
From late 1984 to early 1985, the U.S. Fish and Wildlife Service collected a total of 315 composite samples of whole fish from 109 stations nationwide, which were analyzed for arsenic, cadmium, copper, lead, mercury, selenium, and zinc. Geometric mean, maximum, and 85th percentile concentrations (μg/g wet weight) for 1984...
Spark ablation-inductively coupled plasma spectrometry for analysis of geologic materials
D. W. Golightly, A. Montaser, B.L. Smith, A. F. Dorrzapf Jr.
1989, Talanta (36) 299-303
Spark ablation—inductively coupled plasma (SA-ICP) spectrometry is applied to the measurement of hafnium—zirconium ratios in zircons and to the determination of cerium, cobalt, iron, lead, nickel and phosphorus in ferromanganese nodules. Six operating parameters used for the high-voltage spark and argon-ICP combination are established by sequential simplex optimization of both...
Lithologic, geophysical, and well-construction data for observation wells in the Melton Valley area, Oak Ridge Reservation, Tennessee
Patrick Tucci, D. W. Hanchar
1989, Water-Resources Investigations Report 88-4197
Nineteen wells were installed at nine sites in the Melton Valley area. The wells are intended to provide information on water levels in both regolith and bedrock, aquifer characteristics, and subsurface lithology. Well depths range from 24 to 86 ft for shallow wells, and from 126 to 301 ft for...
Assessment of processes affecting low-flow water quality of Cedar Creek, west-central Illinois
Arthur R. Schmidt, W.O. Freeman, R.D. McFarlane
1989, Water-Resources Investigations Report 88-4141
Water quality and the processes that affect dissolved oxygen, nutrient (nitrogen and phosphorus species), and algal concentrations were evaluated for a 23.8-mile reach of Cedar Creek near Galesburg, west-central Illinois, during periods of warm-weather, low-flow conditions. Water quality samples were collected and stream conditions were measured over a diel (24...
The vertical distribution of selected trace metals and organic compounds in bottom materials of the proposed lower Columbia River export channel, Oregon, 1984
Gregory J. Fuhrer, Arthur J. Horowitz
1989, Water-Resources Investigations Report 88-4099
A proposal to deepen the lower Columbia River navigation channel in Oregon prompted a study of the vertical distribution of selected trace metals and organic compounds in bottom sediments. These data are needed to evaluate the effects of dredging and disposal operations. Elutriation testing of bottom material indicated chemical concentrations...
Quality of bottom material and elutriates in the lower Willamette River, Portland Harbor, Oregon
Gregory J. Fuhrer
1989, Water-Resources Investigations Report 89-4005
In October 1983 the U.S. Geological Survey, in cooperation with the U.S. Army Corp of Engineers, collected bottom-material and water samples from Portland Harbor, Oregon to determine concentrations of trace metals and organic compounds in elutriate-test filtrate and bottom material. Of the trace metals examined in bottom material, concentrations of...
Water quality in Reedy Fork and Buffalo Creek basins in the Greensboro area, North Carolina, 1986-87
M.S. Davenport
1989, Water-Resources Investigations Report 88-4210
Water and bottom-sediment samples were collected from April 1986 through September 1987 at 19 sites in Guilford County and the City of Greensboro, North Carolina. Sampling locations included 13 stream sites, two lakes that supply the City of Greensboro with drinking water, two City of Greensboro finished drinking-water filtration plants,...
Mineral resources of the Mount Tipton Wilderness Study Area, Mohave County, Arizona
Robert C. Greene, Robert L. Turner, Robert C. Jachens, William A. Lawson, Carl L. Almquist
1989, Bulletin 1737-B
The Mount Tipton Wilderness Study Area (AZ-020-012/ 042) comprises 33,950 acres in Mohave County, Ariz. At the request of the U.S. Bureau of Land Management, this area was evaluated for identified mineral resources (known) and mineral resource potential (undiscovered). This work was carried out by the U.S. Bureau of Mines...
The United States Geological Survey: 1879-1989
Mary C. Rabbitt
1989, Circular 1050
The United States Geological Survey was established on March 3, 1879, just a few hours before the mandatory close of the final session of the 45th Congress, when President Rutherford B. Hayes signed the bill appropriating money for sundry civil expenses of the Federal Government for the fiscal year beginning...
Bedrock geology of the Bristol quadrangle, Hartford, Litchfield, and New Haven Counties, Connecticut
Howard E. Simpson
1989, Bulletin 1573
Metamorphosed strata of sedimentary origin underlie the upland surface of western Connecticut, and nonmetamorphosed sedimentary strata underlie the adjacent lowland surface of central Connecticut. The metamorphic rocks consist chiefly of micaceous schists and gneisses, with minor amounts of pegmatite, amphibolite, and metaquartzite. These rocks represent three formations. They are, in...
Studies of contaminant and water quality effects on striped bass prolarvae and yearlings in the Potomac River and upper Chesapeake Bay in 1988
L. W. Hall Jr., M.C. Ziegenfuss, S. J. Bushong, M.A. Unger, R. L. Herman
1989, Transactions of the American Fisheries Society (118) 619-629
Simultaneous on‐site and in situ studies of survival of prolarval and yearling striped bass Morone saxatilis were conducted in the Potomac River during the 1988 spawning season. Various water quality and contaminant conditions were monitored during these experiments. In situ experiments on yearlings and monitoring of water quality and contaminants were also...
Copper deficiency in Tule Elk at Point Reyes, California
Peter J.P. Gogan, David A. Jessup, Mark Akeson
1989, Journal of Range Management (42) 233-238
Tule elk (Cervus elaphus nannodes) reintroduced to Point Reyes, Calif., in 1978 exhibited gross signs of copper deficiency by June 1979. Copper levels in liver (x=5.9 ppm) and serum (0.42 ppm) of elk in Point Reyes were below levels in adult tule elk from other locations in California (liver,...
Suggestions for prospecting
Water Resources Division, U.S. Geological Survey
1989, Report
Prospectors have contributed much to the development of this Nation's mineral resources. Since the time of the earliest settlement, the need for iron for tools and guns, lead for bullets, and copper for utensils has prompted a search for sources of these metals. The lure of gold and silver provided...
Effects of land use on the water quality and biota of three streams in the Piedmont province of North Carolina
J. K. Crawford, D. R. Lenat
1989, Water-Resources Investigations Report 89-4007
Three small streams in North Carolina 's northern Piedmont were studied to compare the effects of land use in their watersheds on water quality characteristics and aquatic biota. Devil 's Cradle Creek (agricultural watershed) had more than two times the sediment yield of Smith Creek (forested watershed) (0.34 tons/acre compared...
Statistical and simulation analysis of hydraulic-conductivity data for Bear Creek and Melton Valleys, Oak Ridge Reservation, Tennessee
J. F. Connell, Z. C. Bailey
1989, Water-Resources Investigations Report 89-4062
A total of 338 single-well aquifer tests from Bear Creek and Melton Valley, Tennessee were statistically grouped to estimate hydraulic conductivities for the geologic formations in the valleys. A cross-sectional simulation model linked to a regression model was used to further refine the statistical estimates for each of the formations...