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Page 5266, results 131626 - 131650

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Thymocyte plasma membrane of the rainbow trout, Salmo gairdneri: Associated immunoglobulin and heteroantigens
G.W. Warr, D. DeLuca, D. P. Anderson
1983, Comparative Biochemistry and Physiology, Part B: Comparative Biochemistry (76) 515-521
1. Thymic lymphocytes of the rainbow trout, S. gairdneri were disrupted and a plasma membrane containing fraction isolated by differential and buoyant density centrifugation.2. Radioiodine introduced into the membrane by the lactoperoxidase catalyzed reaction and immunoglobulin (identified by radioimmunoassay with monoclonal antibody) both copurified in the plasma membrane fraction.3. Rabbit...
Influence of the eyes and pineal gland on locomotor activity patterns of channel catfish, Ictalurus punctatus
C. A. Goudie, K. B. Davis, B.A. Simco
1983, Ecological and Evolutionary Physiology (56) 10-17
The influence of the eyes and pineal gland on locomotor activity rhythms of channel catfish, Ictalurus punctatus, and the extent to which varying light intensity altered these activity rhythms were evaluated. Locomotor activity was measured in normal, blinded, pinealectomized, and pinealectomized-blinded channel catfish exposed to a 12:12 light/dark photoperiod of decreasing light intensities (7,500, 175, and 0.7...
A review of distributed parameter groundwater management modeling methods
Steven M. Gorelick
1983, Water Resources Research (19) 305-319
Models which solve the governing groundwater flow or solute transport equations in conjunction with optimization techniques, such as linear and quadratic programing, are powerful aquifer management tools. Groundwater management models fall in two general categories: hydraulics or policy evaluation and water allocation. Groundwater hydraulic management models enable the determination of...
Remote detection of metal anomalies on Pilot Mountain, Randolph County, North Carolina
N.M. Milton, W. Collins, Sheng-Huei Chang, R. G. Schmidt
1983, Economic Geology (78) 605-617
Pilot Mountain, a hydrothermally altered monadnock within the Carolina slate belt, contains areas of anomalously high amounts of Cu, Mo, and Sn in the soils. Leaves of canopy trees in the mineralized zone also contain more copper than trees in a nearby control area. Spectral data were processed using a...
DIGITAL GEOLOGIC MAP OF THE UNITED STATES.
Patricia Fulton
1983, Conference Paper, Technical Papers of the American Congress of Surveying and Mapping
The geologic map of the United States was published in 1974 by the U. S. Geological Survey. This major publication contains an enormous amount of information on the surficial geology of the United States. Many geologists have used this map as a research tool. Most have needed information from only...
Birdseyes, fenestrae, shrinkage pores, and loferites: a reevaluation
E.A. Shinn
1983, Journal of Sedimentary Petrology (53) 619-628
Birdseyes, birdseye limestone, fenestrae, fenestral fabric, shrinkage pores, and loferites are considered similar or synonymous when occurring in lime mudstone or syndepositional dolomite, especially in association with mudcracks and stromatolites. Compaction experiments indicate, however, that without early cementation, these vugs can be obliterated,...
Geophysical Logging in Carbonate Aquifers
L.M. MacCary
1983, Groundwater (21) 334-342
Some logging methods are inherently superior to others for the analysis of limestone and dolomite aquifers. Three such systems are the density, neutron, and acousticvelocity logs.Relative percentages of limestone and dolomite, average matrix (grain) densities of the rock mixtures, and porosity of the rock mass...
Hafnium isotope results from mid-ocean ridges and Kerguelen.
P. J. Patchett
1983, LITHOS (16) 47-51
176Hf/177Hf ratios are presented for oceanic volcanic rocks representing both extremes of the range of mantle Hf-Nd-Sr isotopic variation. Hf from critical mid-ocean ridge basalts shows that 176Hf/177Hf does indeed have a greater variability than 143Nd/144Nd and 87Sr/86Sr in the depleted mantle. This extra variation is essentially of a random...
Simulation of solute transport in a mountain pool-and-riffle stream with a kinetic mass transfer model for sorption
Kenneth E. Bencala
1983, Water Resources Research (19) 732-738
In natural channels there are often long periods of low flow during which solutes have repeated opportunity for contact with relatively immobile bed materials. Such conditions can exist in very small pool-and-riffle mountain streams. If a solute can sorb onto bed materials, then both hydrodynamic and chemical processes control solute...
The 1979 Homestead Valley earthquake sequence, California: Control of aftershocks and postseismic deformation
R.S. Stein, M. Lisowski
1983, Journal of Geophysical Research Solid Earth (88) 6477-6490
The coseismic slip and geometry of the March 15, 1979, Homestead Valley, California, earthquake sequence are well constrained by precise horizontal and vertical geodetic observations and by data from a dense local seismic network. These observations indicate 0.52±0.10 m of right-lateral slip and 0.17±0.04 m of reverse slip on a...
A description of the external and internal quiet daily variation currents at North American locations for a quiet-Sun year.
W.H. Campbell
1983, Geophysical Journal of the Royal Astronomical Society (73) 51-64
An order 4, degree 12 spherical harmonic analysis of the smoothed quiet geomagnetic daily variations was used to separate the external and internal geomagnetic Sq field at North American locations for the quiet-Sun year, 1965. These fields were represented by a month-by-month display of equivalent current vortex systems with dominant,...
SIMPLE METHOD FOR DETECTING ANOMALOUS FLUID MOTIONS IN BOREHOLES FROM CONTINUOUS TEMPERATURE LOGS.
William H. Diment, Thomas C. Urban
1983, Conference Paper, Transactions - Geothermal Resources Council
Above a critical Rayleigh number, the fluid in a borehole convects. The aspect ratio of the convective motions is commonly between four and ten as determined by temperature-time recordings at fixed depths in cased holes. Aspect ratios greatly in excess of this range indicate anomalous fluid-flow in the hole such...