Origin of the lethal gas burst from Lake Monoun, Cameroun
Haraldur Sigurdsson, J.D. Devine, F.M. Tchua, F.M. Presser, M.K.W. Pringle, William C. Evans
1987, Journal of Volcanology and Geothermal Research (31) 1-16
On 15 August, 1984, a lethal gas burst issued from a submerged 96-m-deep crater in Lake Monoun in Cameroun, western Africa, killing 37 people. The event was associated with a landslide from the eastern crater rim, which slumped into deep water. Waters below 50 m are anoxic, dominated by high...
Direct comparison of kinetic and local equilibrium formulations for solute transport affected by surface reactions
Jean M. Bahr, Jacob Rubin
1987, Water Resources Research (23) 438-452
Modeling transport of reacting solutes in porous media often requires a choice between models based on the local equilibrium assumption (LEA) and models involving reaction kinetics. Direct comparison of the mathematical formulations for these two types of transport models can aid in this choice. For cases of transport affected by...
Evidence for Late-Paleozoic brine migration in Cambrian carbonate rocks of the central and southern Appalachians: Implications for Mississippi Valley-type sulfide mineralization
P.P. Hearn Jr., J. F. Sutter, H. E. Belkin
1987, Geochimica et Cosmochimica Acta (51) 1323-1334
Many Lower Paleozoic limestones and dolostones in the Valley and Ridge province of the central and southern Appalachians contain 10 to 25 weight percent authigenic potassium feldspar. This was considered to be a product of early diagenesis, however, 40Ar39Ar">40Ar39Ar analyses of overgrowths on detrital K-feldspar in...
Benthic foraminifera of the Panamanian Province: distribution and origins.
R.W. Crouch, C. W. Poag
1987, Journal of Foraminiferal Research (17) 153-176
Two hundred twenty-nine species of benthic foraminifera have been identified from 96 stations representing 33 localities on the eastern Pacific inner continental shelf, ranging from southern Peru to northern Baja California. Their distributions mark nearshore provincial boundaries that are nearly identical with those previously documented from the distribution of ostracodes...
Processes and kinetics of Cd2+ sorption by a calcareous aquifer sand
C. C. Fuller, J.A. Davis
1987, Geochimica et Cosmochimica Acta (51) 1491-1502
The rate of Cd2+ sorption by a calcareous aquifer sand was characterized by two reaction steps, with the first step reaching completion in 24 hours. The second step proceeded at a slow and nearly constant rate for at least seven days. The first step includes a fast adsorption reaction which...
Analyzing numerical errors in domain heat transport models using the CVBEM
T. V. Hromadka II
1987, Journal of Offshore Mechanics and Arctic Engineering (109) 163-169
Besides providing an exact solution for steady-state heat conduction processes (Laplace-Poisson equations), the CVBEM (complex variable boundary element method) can be used for the numerical error analysis of domain model solutions. For problems where soil-water phase change latent heat effects dominate the thermal regime, heat transport can be approximately modeled...
NEW APPLICATIONS IN THE INVERSION OF ACOUSTIC FULL WAVEFORM LOGS - RELATING MODE EXCITATION TO LITHOLOGY.
Frederick L. Paillet, C.H. Cheng, J.A. Meredith
1987, Log Analyst (28) 307-320
Existing techniques for the quantitative interpretation of waveform data have been based on one of two fundamental approaches: (1) simultaneous identification of compressional and shear velocities; and (2) least-squares minimization of the difference between experimental waveforms and synthetic seismograms. Techniques based on the first approach do not always work, and...
Changes in the H O Ar isotope composition of clays during retrograde alteration
M.R. Wilson, T.K. Kyser, H. H. Mehnert, J. Hoeve
1987, Geochimica et Cosmochimica Acta (51) 869-878
K-Ar ages of illite alteration associated with Middle Proterozoic Athabasca unconformity-type U deposits in Saskatchewan range from 414 to 1493 Ma. The K-Ar ages correlate with water contents and δD values such that illites with young K-Ar ages have δD values as low as −169 and water contents as high...
A model for trace metal sorption processes at the calcite surface: Adsorption of Cd2+ and subsequent solid solution formation
J.A. Davis, C. C. Fuller, A.D. Cook
1987, Geochimica et Cosmochimica Acta (51) 1477-1490
The rate of Cd2+ sorption by calcite was determined as a function of pH and Mg2+ in aqueous solutions saturated with respect to calcite but undersaturated with respect to CdCO3. The sorption is characterized by two reaction steps, with the first reaching completion within 24 hours. The second step proceeded...
Solute transport with equilibrium aqueous complexation and either sorption or ion exchange: Simulation methodology and applications
F.M. Lewis, Clifford I. Voss, J. Rubin
1987, Journal of Hydrology (90) 81-115
Methodologies that account for specific types of chemical reactions in the simulation of solute transport can be developed so they are compatible with solution algorithms employed in existing transport codes. This enables the simulation of reactive transport in complex multidimensional flow regimes, and provides a means for existing codes to...
Computation of unsteady flows in the Alabama River
Hillary H. Jeffcoat, Marshall E. Jennings
1987, Water Resources Bulletin (23) 313-315
An application is described of the branch-network flow model, BRANCH, to the upper Alabama River system in central Alabama. The model is used to simulate one-dimensional unsteady flows and water surface elevations in approximately 60 river miles of the Alabama River system. Preliminary calibration was made using 72 hours of...
Large-scale volcano-ground ice interactions on Mars
S. W. Squyres, D.E. Wilhelms, A.C. Moosman
1987, Icarus (70) 385-408
The process of volcano-ground ice interaction on Mars is investigated by thermodynamic calculations and observations of Viking Orbiter images. We develop a numerical model of volcano-ground ice interaction that includes heat transport by conduction, radiation from the surface, heat transfer to the...
Biogeochemical cycling in an organic-rich coastal marine basin. 8. A sulfur isotopic budget balanced by differential diffusion across the sediment-water interface
J. P. Chanton, C.S. Martens, M. B. Goldhaber
1987, Geochimica et Cosmochimica Acta (51) 1201-1208
The sulfur isotopic composition of the sulfur fluxes occurring in the anoxic marine sediments of Cape Lookout Bight, N.C., U.S.A., was determined, and the result of isotopic mass balance was obtained via the differential diffusion model. Seasonal pore water sulfate δ34S measurements yielded a calculated sulfate input of 0.6%.. Sulfate transported into the sediments via diffusion...
Thermodynamics of aragonite-strontianite solid solutions: Results from stoichiometric solubility at 25 and 76°C
Niel Plummer, E. Busenberg
1987, Geochimica et Cosmochimica Acta (51) 1393-1411
Dissolution of synthetic strontianite-aragonite solid solutions was followed analytically to stoichiometric saturation using large solid to solution ratios in CO2-H2O solution at 25 and 76°C. The compositional dependence of the equilibrium constant was calculated from the composition of saturated (stoichiometric) solutions and used to calculate the activities and activity...
Presence and potential significance of aromatic-ketone groups in aquatic humic substances
J.A. Leenheer, M. A. Wilson, Ronald L. Malcolm
1987, Organic Geochemistry (11) 273-280
Aquatic humic- and fulvic-acid standards of the International Humic Substances Society were characterized, with emphasis on carbonyl-group nature and content, by carbon-13 nuclear-magnetic-resonance spectroscopy, proton nuclear-magnetic-resonance spectroscopy, and infrared spectroscopy. After comparing spectral results of underivatized humic and fulvic acids with spectral results of chemically modified derivatives, that allow improved...
A Pennsylvanian-age terrestrial storm deposit: using plant fossils to characterize the history and process of sediment accumulation
C. Wnuk, H.W. Pfefferkorn
1987, Journal of Sedimentary Petrology (57) 212-221
A thin black shale overlying the B-coal underclay (in the Middle Pennsylvanian post-Pottsville strata of the Bernice Basin) contains a compression flora composed of large, prostrate, unidirectionally oriented lycopod trunks and randomly oriented pteridosperm stems. Analyses of modern log accumulations indicate that unidirectional...
Pure shear and simple shear calcite textures. Comparison of experimental, theoretical and natural data
H.-R. Wenk, T. Takeshita, E. Bechler, B.G. Erskine, S. Matthies
1987, Journal of Structural Geology (9) 731-745
The pattern of lattice preferred orientation (texture) in deformed rocks is an expression of the strain path and the acting deformation mechanisms. A first indication about the strain path is given by the symmetry of pole figures: coaxial deformation produces orthorhombic pole figures, while non-coaxial deformation yields monoclinic or triclinic...
Examples of transient sounding from groundwater exploration in sedimentary aquifers
D.V. Fitterman
1987, Groundwater (25) 685-692
Examples of the use of transient electromagnetic soundings for three ground-water exploration problems in sedimentary aquifers are given. The examples include: (1) estimating depths to water table and bedrock in an alluvium-filled basin, (2) mapping a confined fresh-water aquifer in bedrock sediments, and (3) locating...
Playa-lake basins on the Southern High Plains of Texas and New Mexico: Part II. A hydrologic model and mass-balance arguments for their development.
W.W. Wood, W. R. Osterkamp
1987, Geological Society of America Bulletin (99) 224-230
Hydrologic, geologic, geomorphic, and mass-balance data suggest that most of the ∼30,000 playa lake basins on the Southern High Plains have developed by a combination of dissolution of caliche and piping of surface material into the unsaturated zone rather than by eolian processes as has generally been stated. A conceptual...
Hydrogeological concepts in the United States: a historical perspective.
J.E. Moore, B.B. Hanshaw
1987, Episodes (10) 315-321
Reviews the development of hydrogeological concepts in the USA from 1879 to 1987, from early qualitative reconnaissance investigations to modern qualitative and multi-disciplinary studies involving predictive analytical techniques and a consideration of management practices. The authors present a sampling of historical milestone papers in US hydrology in the form of...
Detection of a locked zone at depth on the Parkfield, California, segment of the San Andreas fault
R.A. Harris, P. Segall
1987, Journal of Geophysical Research Solid Earth (92) 7945-7962
The Parkfield, California, segment of the San Andreas fault is transitional in character between the creeping segment of the fault to the northwest and the locked Carrizo Plain segment to the southeast. The rate of shallow fault slip decreases from 25–30 mm/yr northwest of the epicenter of the 1966 Parkfield...
Analysis of steady-state salt-water upconing with application at Truro well field, Cape Cod, Massachusetts
T. E. Reilly, M. H. Frimpter, D.R. LeBlanc, A.S. Goodman
1987, Groundwater (25) 194-206
Salt-water upconing describes the phenomenon where salt water is transported vertically upward under a well in response to pumpage in a fresh-water aquifer underlain by salt water. Sharp interface methods have been used successfully to describe the physics of upconing. A finite-element model is developed...
Introduction to the Special Issue on remote sensing
K. Watson
1987, Geophysics (52) 839-840
In 1977, the first Special Issue on remote sensing published by Geophysics contained papers selected from two special sessions at the 45th Annual International SEG Meeting, October 12–16, 1975, in Denver, Colorado. That first Special Issue consisted of eight papers: four are primarily tutorial (image processing, spectral signatures in the...
Infragravity waves over a natural barred profile
A. H. Sallenger Jr., R.A. Holman
1987, Journal of Geophysical Research Solid Earth (92) 9531-9540
Measurements of cross-shore flow were made across the surf zone during a storm as a nearshore bar became better developed and migrated offshore. Measured infragravity band spectra were compared to synthetic spectra calculated numerically over the natural barred profile assuming a white run-up spectrum of leaky mode or high-mode edge...
Role of geophysics in identifying and characterizing sites for high-level nuclear waste repositories.
J. C. Wynn, E.H. Roseboom
1987, Journal of Geophysical Research (92) 7787-7796
Evaluation of potential high-level nuclear waste repository sites is an area where geophysical capabilities and limitations may significantly impact a major governmental program. Since there is concern that extensive exploratory drilling might degrade most potential disposal sites, geophysical methods become crucial as the only nondestructive means to examine large volumes...