Alternative diagenetic models for cretaceous talus deposits, Deep Sea Drilling Project Site 536, Gulf of Mexico
Robert B. Halley, B. J. Pierson, Wolfgang Schlager
1984, Book chapter, Initial reports of the Deep Sea Drilling Project
Talus deposits recovered from Site 536 show evidence of aragonite dissolution, secondary porosity development, and calcite cementation. Although freshwater diagenesis could account for the petrographic features of the altered talus deposits, it does not uniquely account for isotopic or trace-element characteristics. Also, the hydrologic setting required for freshwater alteration is not easily...
VERTICAL MOVEMENT OF GROUND WATER UNDER A LANDFILL, ANCHORAGE, ALASKA.
Gordon L. Nelson
1984, Conference Paper
A thorough review of existing ground-water information may, in some cases, be adequate to estimate rates of migration of pollutants. Analysis of data from well-performance tests and from hydrologic-data stations near a landfill in Anchorage, Alaska, indicates that pollutants migrating downward toward a confined aquifer that supplies water to three...
Aquifer reclamation design: The use of contaminant transport simulation combined with nonlinear programing
Steven M. Gorelick, Clifford I. Voss, Philip E. Gill, Walter Murray, Michael A. Saunders, Margaret H. Wright
1984, Water Resources Research (20) 415-427
A simulation-management methodology is demonstrated for the rehabilitation of aquifers that have been subjected to chemical contamination. Finite element groundwater flow and contaminant transport simulation are combined with nonlinear optimization. The model is capable of determining well locations plus pumping and injection rates for groundwater quality control. Examples demonstrate linear...
Origin and distribution of carbon dioxide in the unsaturated zone of the southern High Plains of Texas
Warren W. Wood, Michael J. Petraitis
1984, Water Resources Research (20) 1193-1208
Partial pressures of CO2, O2, N2, and Ar were monitored at two locations in the Ogallala aquifer system on the Southern High Plains of Texas. Samples were collected monthly during parts of 1980–1981 from nine depths ranging from 0.6 to 36 meters below land surface. PCO2 was observed to be greater at...
Comparison of sediments and organisms in identifying sources of biologically available trace metal contamination
E.A. Thomson, Samuel N. Luoma, C.E. Johansson, D.J. Cain
1984, Water Research (18) 755-765
Sediments and an indicator organism (Macoma balthica, a deposit-feeding bivalve) were used to assess the relative importance of secondary sewage, urban runoff, a landfill containing metal-enriched ash wastes and a yacht harbor in contributing to Ag, Cu and Zn enrichment in South San Francisco Bay. Spatial gradients in sediments and...
Subsurface injection of treated sewage into a saline-water aquifer at St. Petersburg, Florida - Aquifer pressure buildup
J.J. Hickey
1984, Ground Water (22) 48-55
The city of St. Petersburg has been testing subsurface injection of treated sewage into the Floridan aquifer as a means of eliminating discharge of sewage to surface waters and as a means of storing treated sewage for future nonpotable reuse. Treated sweage that had a mean chloride concentration of 170...
RAINFALL-RUNOFF MECHANICS FOR DEVELOPED URBAN BASINS, SOUTH FLORIDA.
Robert A. Miller
1984, Conference Paper, University of Kentucky, Office of Engineering Services, (Bulletin) UKY BU
Rainfall-runoff data, collected by the US Geological Survey as part of an urban hydrology study in south Florida, were analyzed to find relations between depths of rainfall and basin runoff. Data were collected for about 300 runoff events on four different urban land-use basins - commercial, highway, single-family residential, and...
Stable isotope geochemistry of acid mine drainage: Experimental oxidation of pyrite
B.E. Taylor, M.C. Wheeler, D. Kirk Nordstrom
1984, Geochimica et Cosmochimica Acta (48) 2669-2678
Sulfate and water from experiments in which pyrite was oxidized at a pH of 2.0 were analyzed for sulfur and oxygen stable isotopes. Experiments were conducted under both aerobic and anaerobic sterile conditions, as well as under aerobic conditions in the presence of Thiobacillus ferrooxidans, to elucidate the pathways of...
A column technique for determining sorption of organic solutes on the lithological structure of aquifers
D.F. Goerlitz
1984, Bulletin of Environmental Contamination and Toxicology (32) 37-44
No abstract available....
The impact of uncertainties in hydrologic measurement on phosphorus budgets and empirical models for two Colorado reservoirs.
James W. LaBaugh, T. C. Winter
1984, Limnology and Oceanography (29) 322-339
Water budgets and related chemical budgets of aquatic ecosystems commonly are interpreted without reference to uncertainties resulting from errors of measurement. The importance of such uncertainties in the use and interpretation of the phosphorus budgets of two Colorado reservoirs was determined....
Simulation of ground-water flow in a mined watershed in eastern Ohio
J. S. Weiss, A. C. Razem
1984, Groundwater (22) 549-560
A 43-acre watershed in Muskingum County, Ohio, was studied to determine the hydrologic consequences of strip mining for coal. A quantitative description of the effects on the ground-water flow components of the hydrologic system has been obtained using digital models.The premining watershed was characterized by...
Effect of organic contamination upon microbial distributions and heterotrophic uptake in a Cape Cod, Massachusetts, aquifer
R.W. Harvey, R. L. Smith, L. George
1984, Applied and Environmental Microbiology (48) 1197-1202
No abstract available....
The ecological effect of acid conditions and precipitation of hydrous metal oxides in a Rocky Mountain stream
Diane M. McKnight, G. L. Feder
1984, Hydrobiologia (119) 129-138
Periphyton and benthic invertebrates assemblages were studied at the confluence of two Rocky Mountain streams, Deer Creek and the Snake River near Montezuma, Colorado. Upstream from the confluence the Snake River is acidic and enriched in dissolved trace metals, while Deer Creek is a typical Rocky Mountain stream. In the...
Changes in flood response of the Red River of the North basin, North Dakota-Minnesota
Jeffrey E. Miller, Dale L. Frink
1984, Water Supply Paper 2243
The magnitude and frequency of large floods that have occurred in recent years in the basin of the Red River of the North have caused concern that land-use changes and manmade drainage have increased flooding. This study was undertaken to determine whether any changes in flood response of the basin...
Hydrology of area 56, Northern Great Plains, and Rocky Mountain Coal Provinces, Utah
Gregory C. Lines
1984, Open-File Report 83-38
No abstract available....
Hydrologic analysis of the High Plains aquifer system in Box Butte County, Nebraska
R. A. Pettijohn, Hsiu-Hsiung Chen
1984, Water-Resources Investigations Report 84-4046
During the past 40 years, pumpage of ground water for irrigation from the High Plains aquifer system underlying Box Butte County, Nebraska, has resulted in a steady decline of water levels. Consequently, a digital model of the aquifer system was constructed to evaluate various water-management alternatives. The hydraulic conductivity of...
Statistical summaries of streamflow data in Oregon; Volume 1, eastern Oregon
John Friday, S. J. Miller
1984, Open-File Report 84-454
Statistical summaries of streamflow data at 335 streamgaging sites are presented in this two volume report to aid in appraising the hydrology of river basins in Oregon. Records for 31 gaging stations were compiled into separate periods owing to changes in regulation during the period of data collection. The periods...
Pore volume determination in activated carbon and coal
P.J. Reucroft, K.B. Patel, C. T. Chiou
1984, Carbon (22) 100-102
No abstract available....
Volatilization of ketones
R. E. Rathbun, D. Y. Tai
1984, Chemosphere (13) 1009-1023
Volatilization fluxes of seven ketones were measured over a range of temperatures. Gas-film coefficients were calculated from these volatilization fluxes and related to the gas-film coefficient for the evaporation of water. These relations, when combined with an equation for estimating the gas-film coefficient for evaporation of water from a canal,...
Comparison of nonlinear least squares and log transformation procedures for calculating volatilization coefficients
R. E. Rathbun, D. Y. Tai
1984, Chemosphere (13) 715-730
A nonlinear least squares procedure and a log transformation procedure for calculating first-order rate coefficients from experimental concentration-versus-time data were compared using laboratory measurements of the volatilization from water of 1,1,1-trichloroethane and 1,2-dichloroethane and the absorption of oxygen by water. Ratios of the nonlinear least squares to log transformation volatilization...
Heating rates in furnace atomic absorption using the L'vov platform
S. R. Koirtyohann, R.C. Giddings, Howard E. Taylor
1984, Spectrochimica Acta Part B: Atomic Spectroscopy (39) 407-413
Heating rate profiles for the furnace tube wall, the furnace atmosphere, and a L'vov platform were established for a range of conditions in a cyclically heated graphite atomizer. The tube wall profile was made by direct observation with a recording optical pyrometer. The...
Adsorption of goethite onto quartz and kaolinite
M. C. Goldberg, Eugene R. Weiner, P. M. Boymel
1984, Journal of the Chemical Society, Faraday Transactions 1: Physical Chemistry in Condensed Phases (80) 1491-1498
The adsorption of colloidal goethite onto quartz and kaolinite substrates has been studied as a function of pH and NaCl concentration. Goethite adsorption was measured quantitatively by Fourier-transform infrared spectroscopy. The results indicate that adsorption onto both substrates is due primarily to coulombic forces; however, the pH dependence of adsorption...
Paleohydrologic regimes in the southwestern Great Basin, 0-3.2 my ago, compared with other long records of "gobal" climate
G.I. Smith
1984, Quaternary Research (22) 1-17
Nine distinct paleohydrologic regimes in the southwestern Great Basin over the last 3.2 my are recorded by the lacustrine deposits in KM-3, a 930-m core from Searles Lake, California. These are characterized as being "wet," "intermediate," or "dry" (like today). Excepting the present incomplete regime, each lasted 0.12 to 0.76...
Copper transport along a Sierra Nevada stream
James S. Kuwabara, H.V. Leland, Kenneth E. Bencala
1984, Journal of Environmental Engineering (110) 646-655
No abstract available....
Glacier mass balance and runoff research in the U.S.A.
L.R. Mayo
1984, Geografiska Annaler, Series A (66 A) 215-227
Research on glacier mass balance began in the U.S.A. about 50 years ago. More complete studies of climate, snow and ice balance, and the hydrology of glaciers were initiated for the IGY in 1957 and the IHD in 1966. Investigations included the magnitude and geographic distribution of normal...