Instrumentation for a dry-pond detention study
L. M. Pope, M.E. Jennings, K.G. Thibodeaux
1988, Conference Paper
A 12.3-acre, fully urbanized, residential land-use catchment was instrumented by the U. S. Geological Survey in Topeka, Kansas. Hydraulic instrumentation for flow measurement includes two types of flumes, a pipe-insert flume and a culvert-inlet (manhole) flume. Samples of rainfall and runoff for water-quality analyses were collected by automatic, 3-liter, 24-sample...
Kleptoparasitism by bald eagles wintering in south-central Nebraska
Dennis G. Jorde, G.R. Lingle
1988, Journal of Field Ornithology (59) 183-188
Kleptoparasitism on other raptors was one means by which Bald Eagles (Haliaeetus leucocephalus) secured food along the North Platte and Platte rivers during the winters of 1978-1980. Species kelptoparasitized were Ferruginous Hawk (Buteo regalis), Red-tailed Hawk (B. jamaicensis), Rough-legged Hawk (B. lagopus), Golden Eagle (Aquila chrysaetos), and Bald Eagle. Stealing...
Icebergs rework shelf sediments to 500 m off Antarctica
P. W. Barnes, R. Lien
1988, Geology (16) 1130-1133
Icebergs and sea ice rework the sediments of high-latitude shelves, producing modern diamicts (ice-keel turbates) unrelated to glacial proximity. Off Antarctica, sidescan sonar data indicate the presence of ice-gouge features formed by the physical interaction between ice keels and the sea bed. These...
Use of aerial photography to inventory aquatic vegetation
Donald W. Schloesser, Charles L. Brown, Bruce A. Manny
1988, Journal of Aerospace Engineering (1) 142-150
This study demonstrates the feasibility of using low-altitude aerial photography to inventory submersed macrophytes in the connecting channels of the Great Lakes. For this purpose, we obtained aerial color transparencies and collateral ground truth information about submersed vegetation at 160 stations within four study sites in the St. Clair and...
MAGMIX: a basic program to calculate viscosities of interacting magmas of differing composition, temperature, and water content
T. P. Frost, J.R. Lindsay
1988, Computers & Geosciences (14) 213-228
MAGMIX is a BASIC program designed to predict viscosities at thermal equilibrium of interacting magmas of differing compositions, initial temperatures, crystallinities, crystal sizes, and water content for any mixing proportion between end members. From the viscosities of the end members at thermal equilibrium, it is possible to predict the styles...
Contrasting serpentinization processes in the eastern Central Alps
D.J.M. Burkhard, J. R. O’Neil
1988, Contributions to Mineralogy and Petrology (99) 498-506
Stable isotope compositions have been determined for serpentinites from between Davos (Arosa-Platta nappe, Switzerland) and the Valmalenco (Italy). ??D and ??18O values (-120 to -60 and 6-10???, respectively) in the Arosa-Platta nappe indicate that serpentinization took place on the continent at relatively low temperatures in the presence of limited amounts...
Comparative biology of the sculpins of Lake Superior
James H. Selgeby
1988, Journal of Great Lakes Research (14) 44-51
The slimy sculpin (Cottus cognatus), spoonhead sculpin (Cottus ricei), and deepwater sculpin (Myoxocephalus thompsoni) are abundant fishes in Lake Superior. Slimy and spoonhead sculpins occupy a zone from near shore to depths of 210 m but are generally most abundant in waters 50 to 90 m deep. Deepwater sculpins are...
Sorption characteristics of organic compounds on hexadecyltrimethylammonium-smectite
Stephen A. Boyd, Max M. Mortland, Cary T. Chiou
1988, Soil Science Society of America Journal (52) 652-657
When hexadedyltrimethylammonium (HDTMA) ion is exchanged for metal cations like calcium in smectite, the sorptive properties of the clay are greatly modified. The resultant HDTMA-smectite complex behaves as a dual sorbent, in the sorption of organic compounds, in which the mineral fraction functions as a solid adsorbent and the organic...
A statistical evaluation of formation disturbance produced by well- casing installation methods
R. H. Morin, Denis R. LeBlanc, W.E. Teasdale
1988, Ground Water (26) 207-217
Water-resources investigations concerned with contaminant transport through aquifers comprised of very loose, unconsolidated sediments have shown that small-scale variations in aquifer characteristics can significantly affect solute transport and dispersion. Commonly, measurement accuracy and resolution have been limited by a borehole environment consisting of an annulus of disturbed sediments produced by...
Effects of highway runoff on streamflow and water quality in the Sevenmile Creek basin, a rural area in the Piedmont Province of North Carolina, July 1981 to July 1982
Douglas Harned
1988, Water Supply Paper 2329
An evaluation of water-quality data from streams that receive stormwater runoff from a segment of Interstate Highway 85 in North Carolina indicated increased levels of many constituents compared to levels in nearby undeveloped basins. Additional data collected from a network of dry and wet atmospheric deposition collectors, lysimeter samples, soil...
FORTRAN 77 programs for conductive cooling of dikes with temperature-dependent thermal properties and heat of crystallization
P.T. Delaney
1988, Computers & Geosciences (14) 181-212
Temperature histories obtained from transient heat-conduction theory are applicable to most dikes despite potential complicating effects related to magma flow during emplacement, groundwater circulation, and metamorphic reaction during cooling. Here. machine-independent FORTRAN 77 programs are presented to calculate temperatures in and around dikes as they cool conductively. Analytical solutions can...
Partition of nonionic organic compounds in aquatic systems
James A. Smith, Patrick J. Witkowski, Cary T. Chiou
1988, Reviews of Environmental Contamination and Toxicology (103) 127-151
In aqueous systems, the distribution of many nonionic organic solutes in soil-sediment, aquatic organisms, and dissolved organic matter can be explained in terms of a partition model. The nonionic organic solute is distributed between water and different organic phases that behave as bulk solvents. Factors such as polarity, composition, and...
The aqueous geochemistry of uranium in a drainage containing uraniferous organic-rich sediments, Lake Tahoe area, Nevada, USA
R. A. Zielinski, J. K. Otton, R. B. Wanty, C. T. Pierson
1988, Uranium (4) 281-305
Anomalously uraniferous waters occur in a small (4.2 km2) drainage in the west-central Carson Range, Nevada, on the eastern side of Lake Tahoe. The waters transport uranium from local U-rich soils and bedrock to organic-rich valley-fill sediments where it is concentrated, but weakly bound. The dissolved U and the U...
Concentration of gold in natural waters
J. B. McHugh
1988, Journal of Geochemical Exploration (30) 85-94
The purpose of this paper is to investigate the amount of gold present in natural waters. One hundred and thirty-two natural water samples were collected from various sources and analyzed for gold by the latest techniques. Background values for gold in...
Hydrogen concentrations as an indicator of the predominant terminal electron-accepting reactions in aquatic sediments
Derek R. Lovley, S. Goodwin
1988, Geochimica et Cosmochimica Acta (52) 2993-3003
Factors controlling the concentration of dissolved hydrogen gas in anaerobic sedimentary environments were investigated. Results, presented here or previously, demonstrated that, in sediments, only microorganisms catalyze the oxidation of H2 coupled to the reduction of nitrate, Mn(IV), Fe(III), sulfate, or carbon dioxide. Theoretical considerations suggested that, at steady-state conditions, H2...
Ferromanganese deposits from the Gulf of Alaska Seamount Province: Mineralogy, chemistry, and origin
R.A. Koski
1988, Canadian Journal of Earth Sciences (25) 116-133
Ferromanganese-oxide deposits dredged from four seamounts (Welker, Miller, Murray, and Patton) in the Gulf of Alaska Seamount Province include poorly crystallized microlaminated crusts on basalt substrate, well-crystallized Mn-oxide veins in epiclastic sedimentary rocks, and crystalline Mn-oxide layers and micronodules in phosphorite. The principal rock types dredged are alkali-basalt pillow fragments...
Source-rock evaluation of outcrop samples from Vanuatu (Malakula, Espiritu Santo, Maewo, and Pentecost)
Binyamin Buchbinder, Robert B. Halley
1988, Book chapter, Geology and offshore resources of Pacific Island Arcs: Vanuatu Region
Thirty-nine outcrop samples of mudstones, siltstones, and limestones were collected for source-rock evaluation of the sedimentary column in Vanuatu. Twenty-nine samples showing the least evidence of oxidation were selected for total organic analysis from the Miocene Matanui Group and Port Sandwich Formation in Malakula, and from the Miocene Ilava, Peteao,...
Carbonate to siliciclastic periplatform sediments: southwest Florida
Charles W. Holmes
1988, Developments in Sedimentology (42) 271-287
Three distinct carbonate deposits have been identified on the slope and adjacent sea floor of the southwestern Florida Platform: (1) reef talus, recognized by shape and location, found on the upper slope of the Yucatan Channel and also east of the Marquesas Keys; (2) hemipelagic sediments, with complex sigmoid-oblique...
Fate of acetone in an outdoor model stream in southern Mississippi, U.S.A.
R. E. Rathbun, D. W. Stephens, D.J. Shultz, D. Y. Tai
1988, Journal of Hydrology (104) 181-209
The fate of acetone in water was investigated in an outdoor model stream located in southern Mississippi, U.S.A. Acetone was injected continuously for 32 days resulting in small milligram-perliter concentrations in the stream. Rhodamine-WT dye was injected at the beginning and at the end of the study to determine the...
Louisiana hydrologic atlas map no. 3: Altitude of the base of freshwater in Louisiana
Charles W. Smoot
1988, Water-Resources Investigations Report 86-4314
No abstract available....
Methane cycling in the sediments of Lake Washington
K.M. Kuivila, J.W. Murray, A.H. Devol, M.E. Lidstrom, C.E. Reimers
1988, Limnology and Oceanography (33) 571-581
About half of the methane flux from depth is oxidized to CO2 in the upper 0.7 cm of the sediments and the remainder escapes into the water column. In terms of the total carbon budget of the lake, the upward flux of methane is insignificant with only about 2% of...
Conductive heat flux in VC-1 and the thermal regime of Valles caldera, Jemez Mountains, New Mexico
J.H. Sass, P. Morgan
1988, Journal of Geophysical Research Solid Earth (93) 6027-6039
Over 5% of heat in the western United States is lost through Quaternary silicic volcanic centers, including the Valles caldera in north central New Mexico. These centers are the sites of major hydrothermal activity and upper crustal metamorphism, metasomatism, and mineralization, producing associated geothermal resources. We present new heat flow...
Estimation of descriptive statistics for multiply censored water quality data
Dennis R. Helsel, Timothy A. Cohn
1988, Water Resources Research (24) 1997-2004
This paper extends the work of Gilliom and Helsel (1986) on procedures for estimating descriptive statistics of water quality data that contain “less than” observations. Previously, procedures were evaluated when only one detection limit was present. Here we investigate the performance of estimators for data that have multiple detection limits....
Identification, movement, growth, mortality, and exploitation of walleye stocks in Lake St. Clair and the western basin of Lake Erie
Robert C. Haas, Mary C. Fabrizio, Thomas N. Todd
1988, Fisheries Research Report 1954
The harvest of walleye by sport and commercial fisheries in lakes St. Clair and Erie is under a cooperative management program involving several states and two countries. In this report we present the results of a long-term tag-recapture study as well as corroborative evidence of stock discreteness fromstudies of...
Stable isotope geochemistry of sphalerite and other mineral matter in coal beds of the Illinois and Forest City basins
J. F. Whelan, J.C. Cobb, R. O. Rye
1988, Economic Geology (83) 990-1007
Cleat and clastic dikes of Middle Pennsylvanian-age coal beds of the Illinois and Forest City basins of Illinois, Iowa, Missouri, and Kansas locally contain appreciable amounts of sphalerite within a kaolinite-pyrite-sphalerite (+ or - pyrite)-calcite paragenetic sequence. The sphalerite and associated minerals are of interest as a partial record of...