Use of stable isotopes, tritium, soluble salts, and redox-sensitive elements to distinguish ground water from irrigation water in the Salton Sea basin
Roy A. Schroeder, James G. Setmire, Jill N. Densmore
1991, Conference Paper
Evaporative concentration of irrigation water diverted from the Colorado River to the Salton Sea basin for several decades has produced an overlying system (that includes drainwater and surface waters) whose composition is highly variable and differs from that of the shallow regional ground water beneath it. The role of hydrologic...
Observation of suspended sediments in Mobile Bay, Alabama from satellite
Richard P. Stumpf
1991, Conference Paper, Coastal Sediments '91
As part of a comprehensive geologic study of coastal Alabama and Mississippi, the U.S. Geological Survey is investigating coastal sediment transport in Mobile Bay and the adjacent shelf. Satellite imagery from the NOAA AVHRR is being used to provide data on the variability of spatial patterns in the near-surface suspended...
Debris flows as geomorphic agents in the Huachuca Mountains of southeastern Arizona
E.E. Wohl, P.P. Pearthree
1991, Geomorphology (4) 273-292
Numerous debris flows occurred in the Huachuca Mountains of southeastern Arizona during the summer rainy season of 1988 in areas that were burned by a forest fire earlier in the summer. Debris flows occurred following a major forest fire in 1977 as...
National Water-Quality Assessment (NAWQA) program. A basis for water-resource policy development
P. Patrick Leahy, William G. Wilber
1991, Conference Paper
The concepts that are the basis for the U.S. Geological Survey's National Water-Quality Assessment (NAWQA) program began forming in the early 1980's. By 1986, a pilot phase was initiated to test and refine assessment concepts and in 1991, the NAWQA program began a multi-year transition to a fully operational program....
Geochemistry and exploration criteria for epithermal cinnabar and stibnite vein deposits in the Kuskokwim River region, southwestern Alaska
J. E. Gray, R.J. Goldfarb, D.E. Detra, K. E. Slaughter
1991, Journal of Geochemical Exploration (41) 363-386
Cinnabar- and stibnite-bearing epithermal vein deposits are found throughout the Kuskokwim River region of southwestern Alaska. A geochemical orientation survey was carried out around several of these epithermal lodes to obtain information for planning regional geochemical surveys and to develop procedures which maximize the anomaly: threshold contrast of the deposits....
Geochemical mass-balance in a small forested watershed in southwestern Pennsylvania
Emitt C. Witt III, Michael Bikerman
1991, Conference Paper
An intensive hydrologic investigation of the North Fork Bens Creek Watershed on Laurel Hill in southwestern Pennsylvania was made during 1984-85. Precipitation was sampled weekly, and stream water was sampled monthly and during selected storms for discharge and chemical composition. The watershed is underlain by sandstone and sandy shale consisting...
Genesis and continuity of quaternary sand and gravel in glacigenic sediment at a proposed low-level radioactive waste disposal site in east-central Illinois
K. G. Troost, B. Brandon Curry
1991, Environmental Geology and Water Sciences (18) 159-170
The Illinois Department of Nuclear Safety has characterized the Martinsville Alternative Site (MAS) for a proposed low-level radioactive waste disposal facility. The MAS is located in east-central Illinois approximately 1.6 km (1 mi) north of the city of Martinsville. Geologic investigation of the 5.5-km2 (1380-acre) site revealed a sequence of...
A statistical approach to the interpretation of aliphatic hydrocarbon distributions in marine sediments
J. B. Rapp
1991, Chemical Geology (93) 163-177
Q-mode factor analysis was used to quantitate the distribution of the major aliphatic hydrocarbon (n-alkanes, pristane, phytane) systems in sediments from a variety of marine environments. The compositions of the pure end members of the systems were obtained from factor scores and the distribution of the systems within each sample...
Hydrologic and geochemical approaches for determining ground-water flow components
H. W. Hjalmarson, F. N. Robertson
1991, Conference Paper
Lyman Lake is an irrigation-storage reservoir on the Little Colorado River near St. Johns, Arizona. The main sources of water for the lake are streamflow in the Little Colorado River and ground-water inflow from the underlying Coconino aquifer. Two approaches, a hydrologic analysis and a geochemical analysis, were used to...
Chemical equilibrium and mass balance relationships associated with the Long Valley hydrothermal system, California, U.S.A.
A. F. White, M. L. Peterson
1991, Journal of Volcanology and Geothermal Research (48) 283-302
Recent drilling and sampling of hydrothermal fluids from Long Valley permit an accurate characterization of chemical concentrations and equilibrium conditions in the hydrothermal reservoir. Hydrothermal fluids are thermodynamically saturated with secondary quartz, calcite, and pyrite but are in disequilibrium with respect to aqueous sulfide-sulfate speciation. Hydrothermal fluids are enriched in...
Chloride cycling in two forested lake watersheds in the west-central Adirondack Mountains, New York, U.S.A.
N.E. Peters
1991, Water, Air, & Soil Pollution (59) 201-215
The chemistry of precipitation, throughfall, soil water, ground water, and surface water was evaluated in two forested lake-watersheds over a 4-yr period to assess factors controlling C1- cycling. Results indicate that C1- cycling in these watersheds is more complex than the generally held view of the rapid transport of atmospherically...
Relation between the national handbook of recommended methods for water data acquisition and ASTM standards
G. Douglas Glysson, John V. Skinner
1991, Conference Paper, ASTM Special Technical Publication
In the late 1950's, intense demands for water and growing concerns about declines in the quality of water generated the need for more water-resources data. About thirty Federal agencies, hundreds of State, county and local agencies, and many private organizations had been collecting water data. However, because of differences in...
An analytical method for hydrogeochemical surveys: Inductively coupled plasma-atomic emission spectrometry after using enrichment coprecipitation with cobalt and ammonium pyrrolidine dithiocarbamate
D.M. Hopkins
1991, Journal of Geochemical Exploration (41) 349-361
Trace metals that are commonly associated with mineralization were concentrated and separated from natural water by coprecipitation with ammonium pyrollidine dithiocarbamate (APDC) and cobalt and determined by inductively coupled plasma-atomic emission spectroscopy (ICP-AES). The method is useful in hydrogeochemical surveys because it permits preconcentration near the sample sites, and selected...
Tritium concentrations in the active Pu'u O'o crater, Kilauea volcano, Hawaii: implications for cold fusion in the Earth's interior
J. E. Quick, T. K. Hinkley, G.M. Reimer, C. E. Hedge
1991, Physics of the Earth and Planetary Interiors (69) 132-137
The assertion that deuterium-deuterium fusion may occur at low temperature suggests a potential new source of geothermal heat. If a cold-fusion-like process occurs within the Earth, then a test for its existence would be a search for anomalous tritium in volcanic emissions. The Pu'u O'o crater is the first point...
Importance of hydrologic data for interpreting wetland maps and assessing wetland loss and mitigation
V. Carter
1991, Biological Report - US Fish & Wildlife Service (90) 79-85
The US Geological Survey collects and disseminates, in written and digital formats, groundwater and surface-water information related to the tidal and nontidal wetlands of the United States. This information includes quantity, quality, and availability of groundwater and surface water; groundwater and surface-water interactions (recharge-discharge); groundwater flow; and the basic surface-water...
The interaction between biology and the management of aquatic macrophytes
S. A. Nichols
1991, Aquatic Botany (41) 225-252
‘Management’ refers to controlling nuisance aquatic species and to restoring or restructing aquatic plant communities. Producing stable, diverse, aquatic plant communities containing a high percentage of desirable species is a primary management goal.There are a variety of techniques including harvesting, herbicides, water-level fluctuation, sediment alteration, nutrient limitation, light alteration, and...
Geochemistry of dissolved inorganic carbon in a Coastal Plain aquifer. 2. Modeling carbon sources, sinks, and δ13C evolution
Peter B. McMahon, Francis H. Chapelle
1991, Journal of Hydrology (127) 109-135
Stable isotope data for dissolved inorganic carbon (DIC), carbonate shell material and cements, and microbial CO2 were combined with organic and inorganic chemical data from aquifer and confining-bed pore waters to construct geochemical reaction models along a flowpath in the Black Creek aquifer of South Carolina. Carbon-isotope fractionation between DIC and...
Radon-222 and its parent radionuclides in groundwater from two study areas in New Jersey and Maryland, U.S.A.
R. B. Wanty, S. L. Johnson, Paul H. Briggs
1991, Applied Geochemistry (6) 305-318
A study of groundwater chemistry and radionuclide mobility in New Jersey and Maryland was conducted to investigate natural processes that control the mobility of radionuclides in the water-rock system. Groundwater was sampled from two geological units in New Jersey and from six in Maryland. The water sampled was from aquifiers...
Field and modelling studies of immiscible fluid flow above a contaminated water-table aquifer
W.N. Herkelrath, H.I. Essaid, K.M. Hess
1991, Conference Paper, National Conference Publication - Institution of Engineers, Australia
A method was developed for measuring the spatial distribution of immiscible liquid contaminants in the subsurface. Fluid saturation distributions measured at a crude-oil spill site were used to test a numerical multiphase flow model....
Valencia gorge: Possible Messinian refill channel for the western Mediterranean Sea
M.E. Field, J.V. Gardner
1991, Geology (19) 1129-1132
A deeply incised gorge is buried nearly 800 m beneath the floor of the Valencia Trough in the western Mediterranean Sea. The gorge is steeply cut more than 200m into Messinian evaporite deposits and has been mapped for more than 40 km. Published...
Late Neogene marine Ostracoda from Tjornes, Iceland
T. M. Cronin
1991, Journal of Paleontology (65) 767-794
On the western side of the Tjörnes Peninsula in northern Iceland exposures of fossiliferous marine sediments, basalts, and glacial tills record the climatic history of this region of the North Atlantic Ocean. Seventy-five marine ostracode species were recovered from the Pliocene Tjörnes sediments and Quaternary sediments known...
The neutral oil in commercial linear alkylbenzenesulfonate and its effect on organic solute solubility in water
C. T. Chiou, D. E. Kile, D.W. Rutherford
1991, Environmental Science & Technology (25) 660-665
No abstract available....
Mesh-size effects on drift sample composition as determined with a triple net sampler
K. V. Slack, L. J. Tilley, S.S. Kennelly
1991, Hydrobiologia (209) 215-226
Nested nets of three different mesh apertures were used to study mesh-size effects on drift collected in a small mountain stream. The innermost, middle, and outermost nets had, respectively, 425 ??m, 209 ??m and 106 ??m openings, a design that reduced clogging while partitioning collections into three size groups. The...
Effects of drainage on water, sediment and biota
Richard A. Engberg, Marc A. Sylvester, Herman R. Feltz
1991, Conference Paper
The U.S. Department of the Interior started a program in 1985 to identify effects of irrigation-induced trace constituents in water, bottom sediment and biota. The program was developed in response to concerns that contamination similar to that found in 1983 at Kesterson Reservoir in California might exist elsewhere. Studies are...
Degassing and differentiation in subglacial volcanoes, Iceland
J.G. Moore, L. C. Calk
1991, Journal of Volcanology and Geothermal Research (46) 157-180
Within the neovolcanic zones of Iceland many volcanoes grew upward through icecaps that have subsequently melted. These steep-walled and flat-topped basaltic subglacial volcanoes, called tuyas, are composed of a lower sequence of subaqueously erupted, pillowed lavas overlain by breccias and hyaloclastites produced by phreatomagmatic explosions in shallow water, capped by...