Loss of volatile hydrocarbons from an LNAPL oil source
Mary Jo Baedecker, Robert P. Eganhouse, Barbara A. Bekins, Geoffrey N. Delin
2011, Journal of Contaminant Hydrology (126) 140-152
The light nonaqueous phase liquid (LNAPL) oil pool in an aquifer that resulted from a pipeline spill near Bemidji, Minnesota, was analyzed for volatile hydrocarbons (VHCs) to determine if the composition of the oil remains constant over time. Oil samples were obtained from wells at five locations in the oil...
Heterogeneous pumice populations in the 2.08-Ma Cerro Galán Ignimbrite: Implications for magma recharge and ascent preceding a large-volume silicic eruption
Heather M. Wright, Christopher B. Folkes, Ray A.F. Cas, Katharine V. Cashman
2011, Bulletin of Volcanology (73) 1513-1533
Triggering mechanisms of large silicic eruptions remain a critical unsolved problem. We address this question for the ~2.08-Ma caldera-forming eruption of Cerro Galán volcano, Argentina, which produced distinct pumice populations of two colors: grey (5%) and white (95%) that we believe may hold clues to the onset of eruptive activity....
Magma at depth: A retrospective analysis of the 1975 unrest at Mount Baker, Washington, USA
Juliet G. Crider, David Frank, Stephen D. Malone, Michael P. Poland, Cynthia Werner, Jacqueline Caplan-Auerbach
2011, Bulletin of Volcanology (73) 175-189
Mount Baker volcano displayed a short interval of seismically-quiescent thermal unrest in 1975, with high emissions of magmatic gas that slowly waned during the following three decades. The area of snow-free ground in the active crater has not returned to pre-unrest levels, and fumarole gas geochemistry shows a decreasing magmatic...
Origin of a rhyolite that intruded a geothermal well while drilling at the Krafla volcano, Iceland
W.A. Elders, G.O. Fridleifsson, R.A. Zierenberg, E.C. Pope, A.K. Mortensen, A. Gudmundsson, Jacob B. Lowenstern, N.E. Marks, L. Owens, D.K. Bird, M. Reed, N.J. Olsen, Peter Schiffmant
2011, Geology (39) 231-234
Magma flowed into an exploratory geothermal well at 2.1 km depth being drilled in the Krafla central volcano in Iceland, creating a unique opportunity to study rhyolite magma in situ in a basaltic environment. The quenched magma is a partly vesicular, sparsely phyric, glass containing ∼1.8% of dissolved volatiles. Based...
Derivation of S and Pb in phanerozoic intrusion-related metal deposits from neoproterozoic sedimentary pyrite, Great Basin, United States
Peter G. Vikre, S.R. Poulson, Alan E. Koenig
2011, Economic Geology (106) 883-912
The thick (≤8 km), regionally extensive section of Neoproterozoic siliciclastic strata (terrigenous detrital succession, TDS) in the central and eastern Great Basin contains sedimentary pyrite characterized by mostly high δ34S values (−11.6 to 40.8‰, >70% exceed 10‰; 51 analyses) derived from reduction of seawater sulfate, and by markedly radiogenic Pb isotopes...
Volatile abundances and oxygen isotopes in basaltic to dacitic lavas on mid-ocean ridges: The role of assimilation at spreading centers
V.D. Wanless, M.R. Perfit, W.I. Ridley, P.J. Wallace, Craig B. Grimes, E.M. Klein
2011, Chemical Geology (287) 54-65
Most geochemical variability in MOR basalts is consistent with low- to moderate-pressure fractional crystallization of various mantle-derived parental melts. However, our geochemical data from MOR high-silica glasses, including new volatile and oxygen isotope data, suggest that assimilation of altered crustal material plays a significant role in the petrogenesis of dacites...
Pigeonholing pyroclasts: Insights from the 19 March 2008 explosive eruption of Kīlauea volcano
Bruce F. Houghton, Don Swanson, R.J. Carey, J. Rausch, Andrew Sutton
2011, Geology (39) 263-266
We think, conventionally, of volcanic explosive eruptions as being triggered in one of two ways: by release and expansion of volatiles dissolved in the ejected magma (magmatic explosions) or by transfer of heat from magma into an external source of water (phreatic or phreatomagmatic explosions). We document here an event...
Waste isolation and contaminant migration - Tools and techniques for monitoring the saturated zone-unsaturated zone-plant-atmosphere continuum
Brian J. Andraski, David A. Stonestrom
T.J. Nicholson, H.D. Arlt, editor(s)
2011, Conference Paper, Proceedings of the workshop on engineered barrier performance related to low-level radioactive waste, decommissioning, and uranium mill tailings facilities (NUREG/CP-0195)
In 1976 the U.S. Geological Survey (USGS) began studies of unsaturated zone hydrology next to the Nation’s first commercial disposal facility for low-level radioactive waste (LLRW) near Beatty, NV. Recognizing the need for long-term data collection, the USGS in 1983 established research management areas in the vicinity of the waste-burial...
Mercury capture by selected Bulgarian fly ashes: Influence of coal rank and fly ash carbon pore structure on capture efficiency
I.J. Kostova, J.C. Hower, Maria Mastalerz, S.V. Vassilev
2011, Applied Geochemistry (26) 18-27
Mercury capture by fly ash C was investigated at five lignite- and subbituminous-coal-burning Bulgarian power plants (Republika, Bobov Dol, Maritza East 2, Maritza East 3, and Sliven). Although the C content of the ashes is low, never exceeding 1.6%, the Hg capture on a unit C basis demonstrates that the...
Secondary chaotic terrain formation in the higher outflow channels of southern circum-Chryse, Mars
J.A.P. Rodriguez, J.S. Kargel, K. L. Tanaka, D.A. Crown, D.C. Berman, A.G. Fairen, V.R. Baker, R. Furfaro, P. Candelaria, S. Sasaki
2011, Icarus (213) 150-194
Higher outflow channel dissection in the martian region of southern circum-Chryse appears to have extended from the Late Hesperian to the Middle Amazonian Epoch. These outflow channels were excavated within the upper 1. km of the cryolithosphere, where no liquid water is expected to have existed during these geologic epochs....
Effects of nitrogen deposition and empirical nitrogen critical loads for ecoregions of the United States
L.H. Pardo, M.E. Fenn, C.L. Goodale, L.H. Geiser, C. T. Driscoll, E.B. Allen, Jill Baron, R. Bobbink, W.D. Bowman, C.M. Clark, B. Emmett, F.S. Gilliam, T.L. Greaver, S.J. Hall, E.A. Lilleskov, L. Liu, J.A. Lynch, K.J. Nadelhoffer, S.S. Perakis, M. J. Robin-Abbott, J.L. Stoddard, K.C. Weathers, R.L. Dennis
2011, Ecological Applications (21) 3049-3082
Human activity in the last century has led to a significant increase in nitrogen (N) emissions and atmospheric deposition. This N deposition has reached a level that has caused or is likely to cause alterations to the structure and function of many ecosystems across the United States. One approach for...
Gas emissions from failed and actual eruptions from Cook Inlet Volcanoes, Alaska, 1989-2006
C.A. Werner, M.P. Doukas, P.J. Kelly
2011, Bulletin of Volcanology (73) 155-173
Cook Inlet volcanoes that experienced an eruption between 1989 and 2006 had mean gas emission rates that were roughly an order of magnitude higher than at volcanoes where unrest stalled. For the six events studied, mean emission rates for eruptions were ~13,000 t/d CO2 and 5200 t/d SO2, but only...
Ammonium in thermal waters of Yellowstone National Park: Processes affecting speciation and isotope fractionation
J.M. Holloway, D. Kirk Nordstrom, J.K. Böhlke, R. Blaine McCleskey, J.W. Ball
2011, Geochimica et Cosmochimica Acta (75) 4611-4636
Dissolved inorganic nitrogen, largely in reduced form (NH4(T)≈NH4(aq)++NH3(aq)o), has been documented in thermal waters throughout Yellowstone National Park, with concentrations ranging from a few micromolar along the Firehole River to millimolar concentrations at Washburn Hot Springs. Indirect evidence from rock nitrogen analyses and previous work on organic compounds associated with...
210Po in Nevada groundwater and its relation to gross alpha radioactivity
R. L. Seiler
2011, Ground Water (49) 160-171
Polonium-210 (210Po) is a highly toxic alpha emitter that is rarely found in groundwater at activities exceeding 1 pCi/L. 210Po activities in 63 domestic and public-supply wells in Lahontan Valley in Churchill County in northern Nevada, United States, ranged from 0.01 ± 0.005 to 178 ± 16 pCi/L with a...
Segregating gas from melt: an experimental study of the Ostwald ripening of vapor bubbles in magmas
Nicole C. Lautze, Thomas W. Sisson, Margaret T. Mangan, Timothy L. Grove
2011, Contributions to Mineralogy and Petrology (161) 331-347
Diffusive coarsening (Ostwald ripening) of H2O and H2O-CO2 bubbles in rhyolite and basaltic andesite melts was studied with elevated temperature–pressure experiments to investigate the rates and time spans over which vapor bubbles may enlarge and attain sufficient buoyancy to segregate in magmatic systems. Bubble growth and segregation are also considered...
Columnar jointing in vapor-phase-altered, non-welded Cerro Galán Ignimbrite, Paycuqui, Argentina
Heather M. Wright, Chiara Lesti, Ray A.F. Cas, Massimiliano Porreca, Jose G. Viramonte, Christopher B. Folkes, Guido Giordano
2011, Bulletin of Volcanology (73) 1567-1582
Columnar jointing is thought to occur primarily in lavas and welded pyroclastic flow deposits. However, the non-welded Cerro Galán Ignimbrite at Paycuqui, Argentina, contains well-developed columnar joints that are instead due to high-temperature vapor-phase alteration of the deposit, where devitrification and vapor-phase crystallization have increased the density and cohesion of...
'Forensic' geochemical approaches to constrain the source of Au-Ag in low-sulfidation epithermal ores
James A. Saunders, G. D. Kamenov, Albert H. Hofstra, D. L. Unger, R. A. Creaser, F. Barra
Roger Steininger, Bill Pennell, editor(s)
2011, Conference Paper, Great Basin evolution and metallogeny: 2010 symposium proceedings
In order to better constrain genetic processes involved in forming mineral deposits (and ultimately exploration models), it helps to know from where the metals of interest are derived. How the metals arrived at their point of deposition, and why they were deposited there, are separate issues. We are using three...
Occurrence and distribution of organic chemicals and nutrients and comparison of water-quality data from public drinking-water supplies in the Columbia aquifer in Delaware, 2000-08
Betzaida Reyes
2010, Scientific Investigations Report 2010-5206
The U.S. Geological Survey, in cooperation with the Delaware Department of Natural Resources and Environmental Control and the Delaware Geological Survey, conducted a groundwater-quality investigation to (a) describe the occurrence and distribution of selected contaminants, and (b) document any changes in groundwater quality in the Columbia aquifer public water-supply wells...
Contamination movement around a permeable reactive barrier at Solid Waste Management Unit 12, Naval Weapons Station Charleston, North Charleston, South Carolina, 2009
Don A. Vroblesky, Matthew D. Petkewich, Kevin J. Conlon
2010, Scientific Investigations Report 2010-5086
The U.S. Geological Survey and the Naval Facilities Engineering Command Southeast investigated natural and engineered remediation of chlorinated volatile organic compound groundwater contamination at Solid Waste Management Unit 12 at the Naval Weapons Station Charleston, North Charleston, South Carolina, beginning in 2000. In early 2004, groundwater contaminants began moving around...
Hydrostratigraphy, soil/sediment chemistry, and water quality, Potomac-Raritan-Magothy aquifer system, Puchack Well Field Superfund site and vicinity, Pennsauken Township, Camden County, New Jersey, 1997-2001
Julia L. Barringer, Richard L. Walker, Eric Jacobsen, Pamela Jankowski
2010, Scientific Investigations Report 2009-5179
Drinking-water supplies from the Potomac-Raritan-Magothy aquifer system at the Puchack well field in Pennsauken Township, Camden County, New Jersey, have been contaminated by hexavalent chromium-the most toxic and mobile form-at concentrations exceeding the New Jersey maximum contaminant level of 100 micrograms per liter. Also, scattered but widespread instances of volatile...
Augustine Volcano - The influence of volatile components in magmas erupted A.D. 2006 to 2,100 years before present: Chapter 16 in The 2006 eruption of Augustine Volcano, Alaska
James D. Webster, Charlie Mandeville, Beth Goldoff, Michelle L. Coombs, Christine Tappen
John A. Power, Michelle L. Coombs, Jeffrey T. Freymueller, editor(s)
2010, Professional Paper 1769-16
The petrology and geochemistry of 2006 eruptive products of Augustine Volcano, Alaska, have been investigated through analyses of whole-rock samples, phenocrysts, silicate melt inclusions, and matrix glasses to constrain processes of magma evolution, eruption, and degassing. Particular attention was directed toward the concentrations and geochemical relationships involving the magmatic volatile...
Seismic observations of Augustine Volcano, 1970-2007
John A. Power, Douglas J. Lalla
Michelle L. Coombs, Jeffrey T. Freymueller, editor(s)
2010, Professional Paper 1769-1
Seismicity at Augustine Volcano in south-central Alaska was monitored continuously between 1970 and 2007. Seismic instrumentation on the volcano has varied from one to two short-period instruments in the early 1970s to a complex network comprising 8 to 10 short-period, 6 broadband, and 1 strong-motion instrument in 2006. Since seismic...
The role of water in generating the calc-alkaline trend: New volatile data for aleutian magmas and a new tholeiitic index
Mindy M. Zimmer, Terry Plank, Erik H. Hauri, Gene Yogodzinski, Peter L. Stelling, Jessica Larsen, Brad Singer, Brian R. Jicha, Charlie Mandeville, Christopher J. Nye
2010, Journal of Petrology (51) 2411-2444
The origin of tholeiitic (TH) versus calc-alkaline (CA) magmatic trends has long been debated. Part of the problem stems from the lack of a quantitative measure for the way in which a magma evolves. Recognizing that the salient feature in many TH–CA discrimination diagrams is enrichment in Fe during magma...
Surface-water quantity and quality, aquatic biology, stream geomorphology, and groundwater-flow simulation for National Guard Training Center at Fort Indiantown Gap, Pennsylvania, 2002-05
Michael J. Langland, Peter J. Cinotto, Douglas C. Chichester, Michael D. Bilger, Robin A. Brightbill
2010, Scientific Investigations Report 2010-5155
Base-line and long-term monitoring of water resources of the National Guard Training Center at Fort Indiantown Gap in south-central Pennsylvania began in 2002. Results of continuous monitoring of streamflow and turbidity and monthly and stormflow water-quality samples from two continuous-record long-term stream sites, periodic collection of water-quality samples from five...
Applying GORE-TEX technology for rapid contaminant assessments at Fort Gordon, Georgia
Fred W. Falls, Larry G. Harrelson, W. Hagan Ratliff, John B. Wellborn, James Landmeyer
2010, Conference Paper, Proceedings of the 2010 South Carolina Water Resources Conference
The U.S. Geological Survey, in cooperation with the U.S. Department of the Army at Fort Gordon, Georgia, deployed GORE1 adsorbent samplers along creeks and floodplains to rapidly assess potential contamination at abandoned facilities and in adjacent surface water. The samplers provide screening-level data to determine the presence or absence of...