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Page 1670, results 41726 - 41750

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Hydrochemistry of the Mahomet Bedrock Valley Aquifer, East-Central Illinois: Indicators of recharge and ground-water flow
S.V. Panno, Keith C. Hackley, K. Cartwright, Chao-Li Liu
1994, Groundwater (32) 591-604
A conceptual model of the ground-water flow and recharge to the Mahomet Bedrock Valley Aquifer (MVA), east-central Illinois, was developed using major ion chemistry and isotope geochemistry. The MVA is a “basal” fill in the east-west trending buried bedrock valley composed of clean, permeable...
Water resources data, Massachusetts and Rhode Island, water year 1993
R.S. Gadoury, R.S. Socolow, G.G. Girouard, L.R. Ramsbey
1994, Water Data Report MA-RI-93-1
Water resources data for the 1993 water year for Massachusetts and Rhode Island consists of records of stage, discharge, and water quality of streams; contents of lakes and reservoirs; and ground-water levels. This report contains discharge records for 77 gaging stations, month end contents of five lakes and reservoirs, water...
Geochemistry of tectonically expelled fluids from the northern Coast ranges, Rumsey Hills, California, USA
M.L. Davisson, T. S. Presser, R.E. Criss
1994, Geochimica et Cosmochimica Acta (58) 1687-1699
Tectonic compression has created abnormally high pressure on deep basinal fluids causing their expulsion from areally exposed Upper Cretaceous rock along the eastern margin of the California Coast ranges. The fluids emerge as near-neutral, perennial sodium chloride springs at high elevations with flow rates as high as 10 L per...
Comparison of humic substances isolated from peatbog water by sorption on DEAE-cellulose and amberlite XAD-2
J. Hejzlar, B. Szpakowska, R.L. Wershaw
1994, Water Research (28) 1961-1970
Aquatic humic substances (AHS) were isolated from peatbog water by adsorption (1) on diethylaminoethyl cellulose (DEAE-C) and (2) on Amberlite XAD-2 (XAD) to compare yields of the methods and the composition of the isolated AHS. To provide a detailed comparison, the isolates were fractionated using size-exclusion and hydrophobic-interaction chromatography on...
Water Resources Data, California, Water Year 1993. Volume 3. Southern Central Valley Basins and the Great Basin from Walker River to Truckee River
J.R. Mullen, S.W. Anderson, P.D. Hayes
1994, Water Data Report CA-93-3
Water resources data for the 1993 water year for California consist of records of stage, discharge, and water quality of streams; stage and contents in lakes and reservoirs; and water levels and water quality in wells. Volume 3 contains discharge records for 175 streamflow-gaging stations, 3 crest-stage partial-record streamflow stations...
Isotopic Approach to Soil Carbonate Dynamics and Implications for Paleoclimatic Interpretations
E. G. Pendall, J.W. Harden, S.E. Trumbore, O.A. Chadwick
1994, Quaternary Research (42) 60-71
The radiocarbon content and stable isotope composition of soil carbonate are best described by a dynamic system in which isotopic reequilibration occurs as a result of recurrent dissolution and reprecipitation. Depth of water penetration into the soil profile, as well as soil age, determines the degree of carbonate isotope reequilibration....
Water resources data, Virginia, water year 1993; Volume 1: Surface-water discharge and surface-water quality records
Byron J. Prugh Jr., P.E. Herman, Donna L. Belval
1994, Water Data Report VA-93-1
The Water Resources Division of the U.S. Geological Survey, in cooperation with State agencies, obtains a large amount of data pertaining to the water resources of Virginia each water year. These data, accumulated during many water years, constitute a valuable data base for developing an improved understanding of the water...
Water resources data, Wyoming, water year 1993
S. A. Druse, W. R. Glass, G.F. Ritz, M.L. Smalley
1994, Water Data Report WY-93-1
Water resources data for the 1993 water year for Wyoming consists of records of stage, discharge and water quality of streams; stage and contents of lakes and reservoirs, and water levels and water quality of ground water. This report contains discharge records for 190 gaging stations; stage and contents for...
The role of magmas in the formation of hydrothermal ore deposits
Jeffrey W. Hedenquist, Jacob B. Lowenstern
1994, Nature (370) 519-527
Magmatic fluids, both vapour and hypersaline liquid, are a primary source of many components in hydrothermal ore deposits formed in volcanic arcs. These components, including metals and their ligands, become concentrated in magmas in various ways from various sources, including subducted oceanic crust. Leaching of rocks also contributes components...
Ground-water resources of Okeechobee County, Florida
L. A. Bradner
1994, Water-Resources Investigations Report 92-4166
Rapid population growth in Okeechobee County, Florida will increase future demand for potable water. Much of the ground water within the county is vulnerable to saltwater upconing or recharge water of poor-quality from the land surface. The surficial aquifer system within the county is a major source of domestic and...
Development of saline seeps in Southwestern United States
Kenneth S. Johnson
Anon, editor(s)
1994, Conference Paper, National Conference Publication - Institution of Engineers, Australia
Saline seeps are an increasingly serious problem in semi-arid regions of the southwestern United States. They result when excessive recharge of the shallow ground water in soils raises the water table locally to within one meter of the land surface, and the salinity of the shallow water is increased through...
Precursory swarms of long-period events at Redoubt Volcano (1989-1990), Alaska: Their origin and use as a forecasting tool
B. A. Chouet, R.A. Page, C.D. Stephens, J.C. Lahr, J.A. Power
1994, Journal of Volcanology and Geothermal Research (62) 95-135
During the eruption of Redoubt Volcano from December 1989 through April 1990, the Alaska Volcano Observatory issued advance warnings of several tephra eruptions based on changes in seismic activity related to the occurrence of precursory swarms of long-period (LP) seismic events (dominant period of about 0.5 s). The initial eruption...
Testing an automated method to estimate ground-water recharge from streamflow records
A. T. Rutledge, C.C. Daniel
1994, Groundwater (32) 180-189
The computer program, RORA, allows automated analysis of streamflow hydrographs to estimate ground-water recharge. Output from the program, which is based on the recession-curve-displacement method (often referred to as the Rorabaugh method, for whom the program is named), was compared to estimates of recharge obtained...
Evaluation of the effects of an oxygen injection system on the growth, hematology, and immunity of lake trout
W. F. Krise, J. W. Meade, J.R. McClain
1994, Progressive Fish-Culturist (56) 207-210
Fingerling lake trout (Salvelinus namaycush) were reared for 64 d at three pressures of dissolved gases, expressed in relation to saturation values (▵P)–untreated (control) water, ▵P = 10 mm Hg; water treated by column degassing with air, ▵P = 9 mm Hg; and water treated with an oxygen injection system,...
Proceedings Abstracts: American Water Resources Association's Symposium on the National Water-Quality Assessment (NAWQA) Program--November 7-9, 1994, Chicago, Illinois
Stephen K. Sorenson, editor(s)
1994, Open-File Report 94-397
Approximately 418,000 pounds of triazine herbicides are applied annually to control weeds in crops grown in the Albemarle-Pamilico Sound drainage basin, located in North Carolina and Virginia. An enzyme-linked immunosorbent assay was used to detect concentrations of total triazine herbicides in streams draining into Albemarle-Pamlico Sound. Water samples were collected...
Holocene paleoecology of an estuary on Santa Rosa Island, California
K.L. Cole, Gaisheng Liu
1994, Quaternary Research (41) 326-335
The middle to late Holocene history and early Anglo-European settlement impacts on Santa Rosa Island, California, were studied through the analysis of sediments in a small estuarine marsh. A 5.4-m-long sediment core produced a stratigraphic and pollen record spanning the last 5200 yr. Three major zones are distinguishable in the...
Water-quality data for the South Umpqua River Basin, Oregon, 1990-92
Chauncey W. Anderson, Dwight Q. Tanner, Douglas B. Lee
1994, Open-File Report 94-40
Data are presented from a study of algal and nutrient dynamics in the South Umpqua River Basin in southwestern Oregon during summer, low-flow periods from September 1990 to October 1992. The study was done to assist local and state regulatory agencies in determining total maximum daily loads of nutrients for...
Distribution and variability of nitrogen and phosphorus in the alluvial, High Plains, Rush Springs, and Blaine aquifers in western Oklahoma
C.J. Becker
1994, Open-File Report 94-41
Aquifers are the primary source of water for drinking and agricultural purposes in western Oklahoma. Health concerns about consuming nitrogen and an increased reliance on ground water for drinking necessitate a better understanding of the cause and effect of contamination from nutrients. The purpose of this project was to compile...
Sensitivity of northern Sierra Nevada streamflow to climate change
L.F.W. Duell
1994, Water Resources Bulletin (30) 841-859
The sensitivity of streamflow to climate change was investigated in the American, Carson, and Truckee River Basins, California and Nevada. Nine gaging stations were used to represent streamflow in the basins. Annual models were developed by regressing 1961-1991 streamflow data on temperature and precipitation. Climate-change scenarios were used as inputs...
Geochemistry and solid-phase association of chromium in sediment from the Calcasieu River and estuary, Louisiana, U.S.A.
N.S. Simon, C. Demas, W. d'Angelo
1994, Chemical Geology (116) 123-135
Sediment samples were collected from the lower Calcasieu River and estuary, Louisiana, in a study of the release of metals from sediments to the overlying water column. Whole samples were characterized by analyses that included: (1) determination of total sediment ammonium concentrations; (2) determination of total sediment Cr, Mn and...
Disruption of Drift glacier and origin of floods during the 1989-1990 eruptions of Redoubt Volcano, Alaska
D.C. Trabant, R. B. Waitt, J. J. Major
1994, Journal of Volcanology and Geothermal Research (62) 369-385
Melting of snow and glacier ice during the 1989–1990 eruption of Redoubt Volcano caused winter flooding of the Drift River. Drift glacier was beheaded when 113 to 121 × 106 m3 of perennial snow and ice were mechanically entrained in hot-rock avalanches and pyroclastic flows initiated by the four largest eruptions between...
Flow and chloride transport in the tidal Hudson River, NY
Lawrence A. Weiss, Raymond W. Schaffranek, M. Peter de Vries
1994, Conference Paper, Proceedings - National Conference on Hydraulic Engineering
A one-dimensional dynamic-flow model and a one-dimensional solute-transport model were used to evaluate the effects of hypothetical public-supply water withdrawals on saltwater intrusion in a 133-mile reach of the tidal Hudson River between Green Island dam, near Troy, N.Y., and Hastings-on-Hudson, N.Y. Regression techniques were used in analyses of current...
Two- and three-dimensional pathline analysis of contributing areas to public-supply wells of Cape Cod, Massachusetts
Paul M. Barlow
1994, Groundwater (32) 399-410
Steady-state two- and three-dimensional ground-water-flow models coupled with particle tracking (fluid-particle pathline analysis) have been evaluated to determine their relative effectiveness in delineating contributing areas and particle traveltimes to public-supply wells in two contrasting stratified-drift aquifers of Cape Cod, Massachusetts. Several contributing areas delineated by the three-dimensional pathline analysis do...
Permeability-porosity relationships in sedimentary rocks
Philip H. Nelson
1994, Log Analyst (35) 38-62
In many consolidated sandstone and carbonate formations, plots of core data show that the logarithm of permeability (k) is often linearly proportional to porosity (??). The slope, intercept, and degree of scatter of these log(k)-?? trends vary from formation to formation, and these variations are attributed to differences in initial...