Sulfur geochemistry of hydrothermal waters in Yellowstone National Park: I. The origin of thiosulfate in hot spring waters
Y. Xu, M.A.A. Schoonen, D. Kirk Nordstrom, K.M. Cunningham, J.W. Ball
1998, Geochimica et Cosmochimica Acta (62) 3729-3743
Thiosulfate (S2O32−), polythionate (SxO62−), dissolved sulfide (H2S), and sulfate (SO42−) concentrations in thirty-nine alkaline and acidic springs in Yellowstone National Park (YNP) were determined. The analyses were conducted on site, using ion chromatography for thiosulfate, polythionate, and sulfate, and using colorimetry for dissolved sulfide. Thiosulfate was detected at concentrations typically...
Singularity and Nonnormality in the Classification of Compositional Data
Geoffrey C. Bohling, J.C. Davis, Ricardo A. Olea, Jan Harff
1998, Mathematical Geology (30) 5-20
Geologists may want to classify compositional data and express the classification as a map. Regionalized classification is a tool that can be used for this purpose, but it incorporates discriminant analysis, which requires the computation and inversion of a covariance matrix. Covariance matrices of compositional data always will be singular...
Observations on basaltic lava streams in tubes from Kilauea Volcano, island of Hawai'i
J. Kauahikaua, K. V. Cashman, T. N. Mattox, C. Christina Heliker, K.A. Hon, M. T. Mangan, C.R. Thornber
1998, Journal of Geophysical Research B: Solid Earth (103) 27303-27323
From 1986 to 1997, the Pu'u 'O'o-Kupaianaha eruption of Kilauea produced a vast pahoehoe flow field fed by lava tubes that extended 10–12 km from vents on the volcano's east rift zone to the ocean. Within a kilometer of the vent, tubes were as much as 20 m high and...
An evaluation of in-situ measurements of water temperature, specific conductance, and pH in low ionic strength streams
A.J. Ranalli
1998, Water, Air, & Soil Pollution (104) 423-441
Survey for continuous measurement of water temperature, specific conductance, and pH in four low ionic strength streams in the Catskill Mountains of New York was evaluated through a calculation of their bias, precision, and accuracy and by comparison with laboratory measurements of specific conductance and pH on samples collected concurrently....
The interplinian activity at Somma-Vesuvius in the last 3500 years
G. Rolandi, P. Petrosino, Geehin J. Mc
1998, Journal of Volcanology and Geothermal Research (82) 19-52
Between 1884 B.C. and A.D. 472, eruptive activity at Somma-Vesuvius was dominated by the three plinian eruptions of Avellino (3550 yr B.P.), Pompei (A.D. 79) and A.D. 472 and, as a result, little attention has been given to the intervening interplinian activity. The interplinian events are here reconstructed using new...
Chlorine-36 and the initial value problem
S.N. Davis, D. Cecil, M. Zreda, Prakash Sharma
1998, Hydrogeology Journal (6) 104-114
Chlorine-36 is a radionuclide with a half-life of 3.01×105a. Most 36Cl in the hydrosphere originates from cosmic radiation interacting with atmospheric gases. Large amounts were also produced by testing thermonuclear devices during 1952–58. Because the monovalent anion, chloride, is the most common form of chlorine found in...
Using stable isotopes of water and strontium to investigate the hydrology of a natural and a constructed wetland
R. J. Hunt, T.D. Bullen, D. P. Krabbenhoft, C. Kendall
1998, Ground Water (36) 434-443
Wetlands cannot exist without water, but wetland hydrology is difficult to characterize. As a result, compensatory wetland mitigation often only assumes the proper hydrology has been created. In this study, water sources and mass transfer processes in a natural and constructed wetland complex were investigated using...
Chitin: 'Forgotten' source of nitrogen: From modern chitin to thermally mature kerogen: Lessons from nitrogen isotope ratios
A. Schimmelmann, R. P. Wintsch, M. D. Lewan, M. J. DeNiro
1998, ACS Symposium Series (707) 226-242
Chitinous biomass represents a major pool of organic nitrogen in living biota and is likely to have contributed some of the fossil organic nitrogen in kerogen. We review the nitrogen isotope biogeochemistry of chitin and present preliminary results suggesting interaction between kerogen and ammonium during thermal maturation. Modern arthropod chitin...
Quantitative measure of the variation in fault rheology due to fluid-rock interactions
M.L. Blanpied, C.J. Marone, D.A. Lockner, J.D. Byerlee, D.P. King
1998, Journal of Geophysical Research B: Solid Earth (103) 9691-9712
We analyze friction data from two published suites of laboratory tests on granite in order to explore and quantify the effects of temperature (T) and pore water pressure (Pp) on the sliding behavior of faults. Rate-stepping sliding tests were performed on laboratory faults in granite containing “gouge” (granite powder), both...
Landscape modeling for Everglades ecosystem restoration
D.L. DeAngelis, L.J. Gross, M.A. Huston, W.F. Wolff, D. M. Fleming, E.J. Comiskey, S.M. Sylvester
1998, Ecosystems (1) 64-75
A major environmental restoration effort is under way that will affect the Everglades and its neighboring ecosystems in southern Florida. Ecosystem and population-level modeling is being used to help in the planning and evaluation of this restoration. The specific objective of one of these modeling approaches, the Across Trophic Level...
Holocene geologic and climatic history around the Gulf of Alaska
D.H. Mann, A.L. Crowell, T. D. Hamilton, B. P. Finney
1998, Arctic Anthropology (35) 112-131
Though not as dramatic as during the last Ice Age, pronounced climatic changes occurred in the northeastern Pacific over the last 10,000 years. Summers warmer and drier than today's accompanied a Hypsithermal interval between 9 and 6 ka. Subsequent Neoglaciation was marked by glacier expansion after 5-6 ka and the...
Solute changes during aquifer storage recovery testing in a limestone/clastic aquifer
J. E. Mirecki, B. G. Campbell, K.J. Conlon, M.D. Petkewich
1998, Groundwater (36) 394-403
Aquifer storage recovery (ASR) was tested in the Santee Limestone/Black Mingo Aquifer near Charleston, South Carolina, to assess the feasibility for subsurface storage of treated drinking water. Water quality data obtained during two representative ASR tests were interpreted to show three things: (1) recovery efficiency...
Degradation of chloroacetanilide herbicides: The prevalence of sulfonic and oxanilic acid metabolites in Iowa groundwaters and surface waters
Stephen J. Kalkhoff, Dana W. Kolpin, E.M. Thurman, I. Ferrer, D. Barcelo
1998, Environmental Science & Technology (32) 1738-1740
Water samples were collected from 88 municipal wells throughout Iowa during the summer and were collected monthly at 12 stream sites in eastern Iowa from March to December 1996 to study the occurrence of the sulfonic and oxanilic metabolites of acetochlor, alachlor, and metolachlor. The sulfonic and oxanilic metabolites were...
Late Cretaceous to early Tertiary transtension and strain partitioning in the Chugach Accretionary Complex, SE Alaska
J.S. Davis, Sarah M. Roeske, Susan M. Karl
1998, Journal of Structural Geology (20) 639-654
Shear zones in the Late Cretaceous Sitka Graywacke of the Chugach accretionary complex in southeast Alaska record constrictional finite strains, with maximum principal s tretches plunging shallowly subparallel to strike of the shear zones. Macrostructural analysis indicates the finite strain formed during one deformation event. Microstructural analysis of the shear...
Airborne pesticide residues along the Mississippi River
M.S. Majewski, W.T. Foreman, D.A. Goolsbys, N. Nakagaki
1998, Environmental Science & Technology (32) 3689-3698
The occurrence, concentration, and geographical distribution of agricultural pesticides were determined in air over the Mississippi River from New Orleans, LA, to St. Paul, MN, during the first 10 days of June 1994. Air samples were collected from a research vessel by pulling air through polyurethane foam plugs at about...
Bacterial oxidation of dibromomethane and methyl bromide in natural waters and enrichment cultures
K.D. Goodwin, J.K. Schaefer, R.S. Oremland
1998, Applied and Environmental Microbiology (64) 4629-4636
Bacterial oxidation of14CH2Br2 and14CH3Br was measured in freshwater, estuarine, seawater, and hypersaline-alkaline samples. In general, bacteria from the various sites oxidized similar amounts of14CH2Br2 and comparatively less 14CH3Br. Bacterial oxidation of14CH3Br was rapid in freshwater samples compared to bacterial oxidation of 14CH3Br in more saline waters. Freshwater was also the only site in which...
Time functions of deep earthquakes from broadband and short-period stacks
H. Houston, H.M. Benz, J.E. Vidale
1998, Journal of Geophysical Research B: Solid Earth (103) 29895-29913
To constrain dynamic source properties of deep earthquakes, we have systematically constructed broadband time functions of deep earthquakes by stacking and scaling teleseismic P waves from U.S. National Seismic Network, TERRAscope, and Berkeley Digital Seismic Network broadband stations. We examined 42 earthquakes with depths from 100 to 660 km that...
The Fremont complex: A behavioral perspective
D.B. Madsen, S.R. Simms
1998, Journal of World Prehistory (12) 255-336
The Fremont complex is composed of farmers and foragers who occupied the Colorado Plateau and Great Basin region of western North America from about 2100 to 500 years ago. These people included both immigrants and indigenes who shared some material culture and symbolic attributes, but also varied in ways not...
Spatial and temporal study of nitrate concentration in groundwater by means of coregionalization
V. D’Agostino, E.A. Greene, G. Passarella, M. Vurro
1998, Environmental Geology (36) 285-295
Spatial and temporal behavior of hydrochemical parameters in groundwater can be studied using tools provided by geostatistics. The cross-variogram can be used to measure the spatial increments between observations at two given times as a function of distance (spatial structure). Taking into account the existence of such a spatial structure,...
The geochemical record in rock glaciers
E.J. Steig, J. J. Fitzpatrick, N. Potter Jr., D.H. Clark
1998, Geografiska Annaler, Series A: Physical Geography (80) 277-286
A 9.5 m ice core was extracted from beneath the surficial debris cover of a rock glacier at Galena Creek, northwestern Wyoming. The core contains clean, bubble-rich ice with silty debris layers spaced at roughly 20 cm intervals. The debris layers are similar in appearance...
Frequency of effective wave activity and the recession of coastal bluffs: Calvert Cliffs, Maryland
P.R. Wilcock, D. S. Miller, R.H. Shea, R.T. Kerkin
1998, Journal of Coastal Research (14) 256-268
The Calvert Cliffs, Chesapeake Bay, Maryland, USA, erode by direct wave undercutting or by freeze/thaw erosion accompanied by wave removal of slope debris. Directly undercut slopes recede more rapidly, with long-term rates exceeding 1.0 m/yr; freeze/thaw slopes recede at rates approaching 0.5 m/yr. The frequency of wave height and water...
Development of migratory behavior in northern white-tailed deer
M.E. Nelson
1998, Canadian Journal of Zoology (76) 426-432
I examined the development of migratory behavior in northern white-tailed deer (Odocoileus virginianus) from 1975 to 1996 by radio-tracking adult females and their fawns. Of 40 migratory fawns with radio-collared mothers, all returned from winter ranges to their mothers' summer ranges, as did 36 fawns with unknown mothers. Of 1.5-...
A history of early geologic research in the Deep River Triassic Basin, North Carolina
T. W. Clark
1998, Southeastern Geology (38) 65-76
The Deep River Triassic basin has one of the longest recorded histories of geologic research in North Carolina. A quick perusal of nineteenth century geologic literature in North Carolina reveals the Deep River basin has received a tremendous amount of attention, second only, perhaps, to the gold deposits of the...
Abnormally high formation pressures, Potwar Plateau, Pakistan
B. E. Law, S.H.A. Shah, M.A. Malik
1998, AAPG Memoir 247-258
Abnormally high formation pressures in the Potwar Plateau of north-central Pakistan are major obstacles to oil and gas exploration. Severe drilling problems associated with high pressures have, in some cases, prevented adequate evaluation of reservoirs and significantly increased drilling costs. Previous investigations of abnormal pressure in the Potwar Plateau have...
Three-dimensional seismic structure and moment tensors of non-double-couple earthquakes at the Hengill-Grensdalur volcanic complex, Iceland
A.D. Miller, B.R. Julian, G.R. Foulger
1998, Geophysical Journal International (133) 309-325
The volcanic and geothermal areas of Iceland are rich sources of non-double-couple (non-DC) earthquakes. A state-of-the-art digital seismometer network deployed at the Hengill–Grensdalur volcanic complex in 1991 recorded 4000 small earthquakes. We used the best recorded of these to determine 3-D VP and VP /VS structure tomographically and accurate earthquake moment...