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Publication Extents

Not all publications have extents, not all extents are completely accurate
How fast does water flow in an unsaturated macropore? Evidence from field and lab experiments
John R. Nimmo
2003, Book chapter, Estudios de la zona no saturada del suelo, v. VI
A wide range of available field and lab evidence can lead to useful generalizations about the speed of macropore flow, which often dominates the transport of water and contaminants. In 36 published field tests, the values of maximum transport speed in macropores and other preferential channels vary surprisingly little. The...
Microbial degradation of atmospheric halocarbons
Ronald S. Oremland
2003, Book chapter, Microbiology of atmospheric trace gases
Halocarbons are present in the atmosphere at parts-per-trillion (ppt) mixing ratios and are represented by such substances as chlorofluorocarbons (CFCs), hydrochlolofluorocarbons (HCFCs), hydrofluorocarbons (HFCs), and methyl halides like methyl bromide (MeBr) and their further substituted halomethane analogues (e. g., dibromomethane, bromoform). Many Halocarbons have only an anthropogenic origin (e.g., CFCs,...
Geothermal arsenic
John G. Webster, D. Kirk Nordstrom
A. H. Welch, Kenneth G. Stollenwerk, editor(s)
2003, Book chapter, Arsenic in ground water: Geochemistry and occurrence
No abstract available. ...
Geochemical processes controlling transport of arsenic in groundwater: A review of adsorption
Kenneth G. Stollenwerk
A. H. Welch, Kenneth G. Stollenwerk, editor(s)
2003, Book chapter, Arsenic in Ground Water
Adsorption is the predominate mechanism controlling transport of arsenic in many ground water systems. Hydrous oxides of iron, aluminum, and manganese, and clay minerals are commonly associated with aquifer solids and have been shown to be significant adsorbents of arsenic. The extent of arsenic adsorption is influenced by the chemistry...
Climate science issues and needs of the CALFED Bay-Delta Program
M. D. Dettinger, W.A. Bennett, D.R. Cayan, J. Florsheim, M. Hughes, B.L. Ingram, A.D. Jassby, N. Knowles, F. Malamud, D. H. Peterson, K. Redmond, L. Smith
2003, Conference Paper, American Meteorological Society, 83rd Annual Meeting, Impacts of Water Availability Symposium
No abstract available....
Formation and evolution of valley-bottom and channel features, Lower Deschutes River, Oregon
Janet H. Curran, Jim E. O’Conner
Jim E. O’Conner, Gordon E. Grant, editor(s)
2003, AGU Water Science and Application Series 7-5
Primary geologic and geomorphic processes that formed valley-bottom and channel features downstream from the Pelton-Round Butte dam complex are inferred from a canyon-long analysis of feature morphology, composition, location, and spatial distribution. Major controls on valley-bottom morphology are regional tectonics, large landslides, and outsized floods (floods with return periods greater...
Meteorology and hydrology in Yosemite National Park: A sensor network application
J.D. Lundquist, D.R. Cayan, M. D. Dettinger
2003, Lecture Notes in Computer Science (including subseries Lecture Notes in Artificial Intelligence and Lecture Notes in Bioinformatics) (2634) 518-528
Over half of California's water supply comes from high elevations in the snowmelt-dominated Sierra Nevada. Natural climate fluctuations, global warming, and the growing needs of water consumers demand intelligent management of this water resource. This requires a comprehensive monitoring system across and within the Sierra Nevada. Unfortunately, because of severe...
Interactions between dissolved organic matter and mercury in the Florida Everglades
G. Aiken, M. Haitzer, J. N. Ryan, K. Nagy, George Aiken
Boutron C.Ferrari C., editor(s)
2003, Journal De Physique. IV : JP (107) 29-32
Experiments were conducted using organic matter isolated from various surface waters in the Florida Everglades to study the interactions between dissolved organic matter (DOM) and Hg (II). Conditional distribution coefficients ( ), obtained using an equilibriurn dialysis ligand exchange method, were strongly affected by...
Assessing toxicant effects in a complex estuary--A case study of effects of silver on reproduction in the bivalve, Potamocurbula amurensis, in San Francisco Bay
Cynthia L. Brown, Francis Parchaso, Janet K. Thompson, Samuel N. Luoma
2003, Human and Ecological Risk Assessment (9) 95-119
Contaminant exposures in natural systems can be highly variable. This variability is superimposed upon cyclic variability in biological processes. Together, these factors can confound determination of contaminant effects. Long term, multidisciplined studies with high frequency sampling can be effective in overcoming such obstacles. While studying trace metal contamination in the...
Temperature-profile methods for estimating percolation rates in arid environments
Jim Constantz, Scott W. Tyler, Edward Kwicklis
2003, Vadose Zone Journal (2) 12-24
Percolation rates are estimated using vertical temperature profiles from sequentially deeper vadose environments, progressing from sediments beneath stream channels, to expansive basin-fill materials, and finally to deep fractured bedrock underlying mountainous terrain. Beneath stream channels, vertical temperature profiles vary over time in response to downward heat transport, which is generally...
Two new organic reference materials for δ13C and δ15N measurements and a new value for the δ13C of NBS 22 oil
Haiping Qi, Tyler B. Coplen, Heike Geilmann, Willi A. Brand, J.K. Böhlke
2003, Rapid Communications in Mass Spectrometry (17) 2483-2487
Analytical grade L-glutamic acid is chemically stable and has a C/N mole ratio of 5, which is close to that of many of natural biological materials, such as blood and animal tissue. Two L-glutamic acid reference materials with substantially different 13C and 15N abundances have been prepared for use as...
The ecology of arsenic
Ronald S. Oremland, John F. Stolz
2003, Science (300) 939-944
Arsenic is a metalloid whose name conjures up images of murder. Nonetheless, certain prokaryotes use arsenic oxyanions for energy generation, either by oxidizing arsenite or by respiring arsenate. These microbes are phylogenetically diverse and occur in a wide range of habitats. Arsenic cycling may take place in the absence of...
Spatial variability of groundwater recharge and its effect on shallow groundwater quality in southern New Jersey
Bernard T. Nolan, Arthur L. Baehr, Leon J. Kauffman
2003, Vadose Zone Journal (2) 677-691
Point estimates of groundwater recharge at 48 sediment-coring locations vary substantially (−18.5–1840 cm yr−1) in a 930-km2 area of southern New Jersey. Darcian estimates of steady, long-term recharge made at depth in the unsaturated zone were estimated using pedotransfer functions of soil texture and interpolated (mapped) with nonparametric methods to...
Peer reviewed: Characterizing aquatic dissolved organic matter
Jerry A. Leenheer, Jean-Philippe Croue
2003, Environmental Science & Technology (37) 18A-26A
Whether it causes aesthetic concerns such as color, taste, and odor; leads to the binding and transport of organic and inorganic contaminants; produces undesirable disinfection byproducts; provides sources and sinks for carbon; or mediates photochemical processes, the nature and properties of dissolved organic matter (DOM) in water are topics of...
Immobilization of cobalt by sulfate-reducing bacteria in subsurface sediments
Lee R. Krumholz, Dwayne A. Elias, Joseph M. Suflita
2003, Geomicrobiology Journal (20) 61-72
We investigated the impact of sulfate-reduction on immobilization of metals in subsurface aquifers. Co 2+ was used as a model for heavy metals. Factors limiting sulfate-reduction dependent Co 2+ immobilization were tested on pure cultures of sulfate-reducing bacteria, and in sediment columns from a landfill leachate contaminated aquifer. In the...
The geochemical evolution of riparian ground water in a forested piedmont catchment
Douglas A. Burns, Niel Plummer, Jeffrey J. McDonnell, Eurybiades Busenberg, Gerolamo C. Casile, Carol Kendall, Richard P. Hooper, James E. Freer, Norman E. Peters, Keith Beven, Peter Schlosser
2003, Groundwater (41) 913-925
The principal weathering reactions and their rates in riparian ground water were determined at the Panola Mountain Research Watershed (PMRW) near Atlanta, Georgia. Concentrations of major solutes were measured in ground water samples from 19 shallow wells completed in the riparian (saprolite) aquifer and in one borehole completed in granite,...
Changes in the chemistry of lakes and precipitation in high-elevation national parks in the western United States, 1985–1999
David W. Clow, James O. Sickman, Robert G. Striegl, David P. Krabbenhoft, John G. Elliott, Mark M. Dornblaser, David A. Roth, Donald H. Campbell
2003, Water Resources Research (39)
High-elevation lakes in the western United States are sensitive to atmospheric deposition of sulfur and nitrogen due to fast hydrologic flushing rates, short growing seasons, an abundance of exposed bedrock, and a lack of well-developed soils. This sensitivity is reflected in the dilute chemistry of the lakes, which was documented...
Comment on “Isotopic fractionation between Fe(III) and Fe(II) in aqueous solutions” by Clark Johnson et al., [Earth Planet. Sci. Lett. 195 (2002) 141–153]
Thomas D. Bullen, Arthur F. White, Cyril W. Childs
2003, Earth and Planetary Science Letters (206) 229-232
In a recent contribution [1], Johnson et al. reported the equilibrium isotope fractionation factor between dissolved Fe(II) and Fe(III) in aqueous solutions at pH=2.5 and 5.5. They suggest that because the iron isotope fractionation observed in their experiments spans virtually the entire range observed in...
Determining temperature and thermal properties for heat-based studies of surface-water ground-water interactions: Appendix A of Heat as a tool for studying the movement of ground water near streams (Cir1260)
David A. Stonestrom, Kyle W. Blasch
David A. Stonestrom, Jim Constantz, editor(s)
2003, Report, Heat as a tool for studying the movement of ground water near streams (Cir1260)
Advances in electronics leading to improved sensor technologies, large-scale circuit integration, and attendant miniaturization have created new opportunities to use heat as a tracer of subsurface flow. Because nature provides abundant thermal forcing at the land surface, heat is particularly useful in studying stream-groundwater interactions. This appendix describes methods for...