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Flow to a well in a water-table aquifer: An improved laplace transform solution
A.F. Moench
1996, Ground Water (34) 593-604
An alternative Laplace transform solution for the problem, originally solved by Neuman, of constant discharge from a partially penetrating well in a water-table aquifer was obtained. The solution differs from existing solutions in that it is simpler in form and can be numerically inverted without the need for time-consuming numerical...
A catastrophic flood caused by drainage of a caldera lake at Aniakchak Volcano, Alaska, and implications for volcanic hazards assessment
C. F. Waythomas, J. S. Walder, R. G. McGimsey, C.A. Neal
1996, Geological Society of America Bulletin (108) 861-871
Aniakchak caldera, located on the Alaska Peninsula of southwest Alaska, formerly contained a large lake (estimated volume 3.7 × 109 m3) that rapidly drained as a result of failure of the caldera rim sometime after ca. 3400 yr B.P. The peak discharge of the resulting flood was estimated using three methods:...
Effects of glacial meltwater inflows and moat freezing on mixing in an ice-covered antarctic lake as interpreted from stable isotope and tritium distributions
L.G. Miller, G. R. Aiken
1996, Limnology and Oceanography (41) 966-976
Perennially ice-covered lakes in the McMurdo Dry Valleys have risen several meters over the past two decades due to climatic warming and increased glacial meltwater inflow. To elucidate the hydrologic responses to changing climate and the effects on lake mixing processes we measured the stable isotope (??18O and ??D) and...
The influence of landscape position on lake chemical responses to drought in northern Wisconsin
K.E. Webster, T.K. Kratz, C.J. Bowser, J.J. Magnuson, W. J. Rose
1996, Limnology and Oceanography (41) 977-984
Climatic shifts to drier conditions during drought alter the hydrologic pathways of water and solute flow to aquatic ecosystems. We examined differences in drought-induced trends in the semiconservative cations, Ca+Mg, in seven northern Wisconsin lakes. These spanned the range of hydrologic settings in the region, including hydraulically mounded, groundwater flowthrough,...
Hydrologic impact of Great Flood of 1993 in south-central Kansas
M. Sophocleous, A.J. Stern, S.P. Perkins
1996, Journal of Irrigation and Drainage Engineering (122) 203-210
The writers analyze the hydrologic budget and quantify the ground-water recharge impact of the Great Flood of 1993 on the Great Bend Prairie aquifer of south-central Kansas. During the summer of 1993, rainfall totals exceeded normal levels by 200% in the northern portion of the study area, while air temperature...
Occurrence and accumulation of pesticides and organic contaminants in river sediment, water and clam tissues from the San Joaquin River and tributaries, California
W. E. Pereira, Joseph L. Domagalski, F. D. Hostettler, L. R. Brown, J. B. Rapp
1996, Environmental Toxicology and Chemistry (15) 172-180
A study was conducted in 1992 to assess the effects of anthropogenic activities and land use on the water quality of the San Joaquin River and its major tributaries. This study focused on pesticides and organic contaminants, looking at distributions of contaminants in water, bed and suspended sediment, and the...
Controls on surface water chemistry in the upper Merced River basin, Yosemite National Park, California
D. W. Clow, M.A. Mast, K. Campbell
1996, Hydrological Processes (10) 727-746
Surface water draining granitic bedrock in Yosemite National Park exhibits considerable variability in chemical composition, despite the relative homogeneity of bedrock chemistry. Other geological factors, including the jointing and distribution of glacial till, appear to exert strong controls on water composition. Chemical data from...
Reactive solute transport in acidic streams
R. E. Broshears
1996, Water, Air, & Soil Pollution (90) 195-204
Spatial and temporal profiles of Ph and concentrations of toxic metals in streams affected by acid mine drainage are the result of the interplay of physical and biogeochemical processes. This paper describes a reactive solute transport model that provides a physically and thermodynamically quantitative interpretation of these profiles. The model...
Climate change and northern prairie wetlands: Simulations of long-term dynamics
Karen A. Poiani, W. Carter Johnson, George A. Swanson, Thomas C. Winter
1996, Limnology and Oceanography (41) 871-881
A mathematical model (WETSIM 2.0) was used to simulate wetland hydrology and vegetation dynamics over a 32-yr period (1961–1992) in a North Dakota prairie wetland. A hydrology component of the model calculated changes in water storage based on precipitation, evapotranspiration, snowpack, surface runoff, and subsurface inflow. A spatially explicit vegetation...
Infiltration and solute transport experiments in unsaturated sand and gravel, Cape Cod, Massachusetts: Experimental design and overview of results
David L. Rudolph, R. Gary Kachanoski, Michael A. Celia, Denis R. LeBlanc, Jonathon H. Stevens
1996, Water Resources Research (32) 519-532
A series of infiltration and tracer experiments was conducted in unsaturated sand and gravel deposits on Cape Cod, Massachusetts. A network of 112 porous cup lysimeters and 168 time domain reflectometry (TDR) probes was deployed at depths from 0.25 to 2.0 m below ground surface along the centerline of a...
Shallow subsurface geology of part of the Savannah River alluvial valley in the upper Coastal Plain of Georgia and South Carolina
D.C. Leeth, D.D. Nagle
1996, Southeastern Geology (36) 1-14
The depth to which Coastal Plain rivers incise underlying formations is an important control on local and regional hydrologic flow systems. In order to clarify these stream/aquifer relations, a better understanding of the shallow subsurface geology of the Savannah River was necessary. To accomplish this, three drillhole transects were completed...
Effects of winter atmospheric circulation on temporal and spatial variability in annual streamflow in the western United States
G. J. McCabe Jr.
1996, Hydrological Sciences Journal (41) 873-887
Winter mean 700-hectoPascal (hPa) height anomalies, representing the average atmospheric circulation during the snow season, are compared with annual streamflow measured at 140 streamgauges in the western United States. Correlation and anomaly pattern analyses are used to identify relationships between winter mean atmospheric circulation and temporal and spatial variability in...
Integrating a geographic information system, a scientific visualization system and an orographic precipitation model
L. Hay, L. Knapp
1996, IAHS-AISH Publication 123-131
Investigating natural, potential, and man-induced impacts on hydrological systems commonly requires complex modelling with overlapping data requirements, and massive amounts of one- to four-dimensional data at multiple scales and formats. Given the complexity of most hydrological studies, the requisite software infrastructure must incorporate many components including simulation modelling, spatial analysis...
A top specified boundary layer (TSBL) approximation approach for the simulation of groundwater contamination processes
H. Rubin, R. W. Buddemeier
1996, Journal of Contaminant Hydrology (22) 123-144
This paper presents improvements in the 'classical boundary layer' (CBL) approximation method to obtain simple but robust initial characterization of aquifer contamination processes. Contaminants are considered to penetrate into the groundwater through the free surface of the aquifer. The improved method developed in this study is termed the 'top specified...
Hydrologic landscapes on the Delmarva Peninsula - Part 2: Estimates of base-flow nitrogen load to Chesapeake Bay
Bachman L. Joseph, P. J. Phillips
1996, Journal of the American Water Resources Association (32) 779-791
ABSTRACT: The relation between landscape characteristics and water chemistry on the Delmarva Peninsula can be determined through a principal-component analysis of basin characteristics. Two basin types were defined by factor scores: (1) well-drained basins, characterized by combinations of a low percentage of forest cover, a low...
Herbicide metabolites in surface water and groundwater: Introduction and overview
E.M. Thurman, M. T. Meyer
1996, ACS Symposium Series (630)
Several future research topics for herbicide metabolites in surface and ground water are outlined in this chapter. They are herbicide usage, chemical analysis of metabolites, and fate and transport of metabolites in surface and ground water. These three ideas follow the themes in this book, which are the summary of...
Wide angle X-ray scattering (WAXS) study of "two-line" ferrihydrite structure: Effect of arsenate sorption and counterion variation and comparison with EXAFS results
G.A. Waychunas, C. C. Fuller, B.A. Rea, J.A. Davis
1996, Geochimica et Cosmochimica Acta (60) 1765-1781
Wide angle X-ray scattering (WAXS) measurements have been made on a suite of “two-line” ferrihydrite (FHY2) samples containing varying amounts of coprecipitated arsenate. Samples prepared at pH 8 with counter ions chloride, nitrate, and a mixture of both also were examined. The raw WAXS scattering functions show that “two-line” ferrihydrite...
Experimental investigation and modeling of uranium (VI) transport under variable chemical conditions
M. Kohler, G.P. Curtis, D.B. Kent, J.A. Davis
1996, Water Resources Research (32) 3539-3551
The transport of adsorbing and complexing metal ions in porous media was investigated with a series of batch and column experiments and with reactive solute transport modeling. Pulses of solutions containing U(VI) were pumped through columns filled with quartz grains, and the breakthrough of U(VI) was studied as a function...
Kinetic and mineralogic controls on the evolution of groundwater chemistry and 87Sr/86Sr in a sandy silicate aquifer, northern Wisconsin, USA
T.D. Bullen, D. P. Krabbenhoft, C. Kendall
1996, Geochimica et Cosmochimica Acta (60) 1807-1821
Substantial flowpath-related variability of 87Sr/86Sr is observed in groundwaters collected from the Trout Lake watershed of northern Wisconsin. In the extensive shallow aquifer composed of sandy glacial outwash, groundwater is recharged either by seepage from lakes or by precipitation that infiltrates the inter-lake uplands. 87Sr/86Sr of groundwater derived mainly as...
The long-term salinity field in San Francisco Bay
R.J. Uncles, D. H. Peterson
1996, Continental Shelf Research (16) 2005-2039
Data are presented on long-term salinity behaviour in San Francisco Bay, California. A two-level, width averaged model of the tidally averaged salinity and circulation has been written in order to interpret the long-term (days to decades) salinity variability. The model has been used to simulate daily averaged salinity in the...
Use of 13C NMR and ftir for elucidation of degradation pathways during natural litter decomposition and composting I. early stage leaf degradation
R.L. Wershaw, J.A. Leenheer, K. R. Kennedy, T.I. Noyes
1996, Soil Science (161) 667-679
Oxidative degradation of plant tissue leads to the formation of natural dissolved organic carbon (DOC) and humus. Infrared (IR) and 13C nuclear magnetic resonance (NMR) spectrometry have been used to elucidate the chemical reactions of the early stages of degradation that give rise to DOC derived from litter and compost....
Reactive solute transport in streams: 1. Development of an equilibrium- based model
Robert L. Runkel, Kenneth E. Bencala, Robert E. Broshears, Steven C. Chapra
1996, Water Resources Research (32) 409-418
An equilibrium-based solute transport model is developed for the simulation of trace metal fate and transport in streams. The model is formed by coupling a solute transport model with a chemical equilibrium submodel based on MINTEQ. The solute transport model considers the physical processes of advection, dispersion, lateral inflow, and...
Comparison of denitrification activity measurements in groundwater using cores and natural-gradient tracer tests
R. L. Smith, S. P. Garabedian, M. H. Brooks
1996, Environmental Science & Technology (30) 3448-3456
The transport of many solutes in groundwater is dependent upon the relative rates of physical flow and microbial metabolism. Quantifying rates of microbial processes under subsurface conditions is difficult and is most commonly approximated using laboratory studies with aquifer materials. In...