Retention of lead during oxidative ashing of selected naturally occurring carbonaceous substances
F. Cuttitta, J.J. Warr Jr.
1958, Geochimica et Cosmochimica Acta (13) 256-259
The amount of lead retained in the ash of lead-bearing carbonaceous material is essentially independent of the method of ashing. Samples containing lead in the range of 0.00X to 0.X per cent were ashed by ignition in a high-oxygen atmosphere and were also wet-ashed. The lead in the ash was...
The water, deuterium, gas and uranium content of tektites
I. Friedman
1958, Geochimica et Cosmochimica Acta (14) 316-324
The water content, deuterium concentration of the water, total gas and uranium contents were determined on tektite samples and other glass samples from Texas, Australia, Philippine Islands, Java, French Indo-China, Czechoslovakia, Libyan Desert, Billiton Island, Thailand, French West Africa, Peru, and New Mexico. The water content ranges from 0.24 per...
Role of clay minerals in the transportation of iron
D. Carroll
1958, Geochimica et Cosmochimica Acta (14) 1-28
The clay minerals have iron associated with them in several ways:1.(1) as an essential constituent2.(2) as a minor constituent within the crystal lattice where it is in isomorphous substitution and3.(3) as iron oxide on the surface of the mineral platelets. Nontronite, “hydromica,” some...
Biogeochemistry of the rare-earth elements with particular reference to hickory trees
W. O. Robinson, H. Bastron, K. J. Murata
1958, Geochimica et Cosmochimica Acta (14) 55-67
Hickory trees concentrate the rare-earth elements in their leaves to a phenomenal degree and may contain as much as 2300 p.p.m. of total rare earths based on the dry weight of the leaves. The average proportions of the individual elements (atomic percent of the total rare-earth elements) in the leaves...
A combined deamination and nitro reduction method for nitroanilines
G. C. Finger, R.H. White
1958, Journal of Organic Chemistry (23) 1612-1613
The hypophosphorous acid-cuprous oxide deamination method on nitroanilines has been modified so that the nitro compounds which are formed are reduced in turn by cuprous oxide to the corresponding amines. Over-all yields of 55-65% are reported for three halogenated nitroanilines....
Determination of thorium in the parts per million range in rocks
H. Levine, F. S. Grimaldi
1958, Geochimica et Cosmochimica Acta (14) 93-97
A procedure is presented for the determination of thorium in the concentration range of 0·2 to 10 parts per million ThO2 in felsic or mafic rocks. Thorium is extracted by mesityl oxide and purified by iodate precipitation from nitric acid medium containing tartaric acid and hydrogen peroxide. The thorium is determined...
Information needed with analytical data
W.B. Hamilton
1958, Geochimica et Cosmochimica Acta (14) 253-255
No abstract available....
Uranium in carbonaceous rocks in the Townsend and Helena Valleys, Montana
George Earle Becraft
1958, Bulletin 1046-G
No abstract available....
Ground-water resources of the San Luis Valley, Colorado, with a section on an inflow-outflow study of the area
William J. Powell, Philip B. Mutz
1958, Water Supply Paper 1379
No abstract available....
Isolation and identification of an ester from a crude oil
H.F. Phillips, Irving A. Breger
1958, Geochimica et Cosmochimica Acta (15) 51-56
A dioctylphthalate has been isolated from a crude oil by means of adsorption column chromatography. The ester was identified by means of elemental analysis, refractive index, and its infra-red absorption spectrum. Saponification of the isolate and examination of the resultant alcohol by means of infrared absorption spectra led to the...
Use of ion exchange resins in the analysis of rocks and minerals: Separation of sodium and potassium
L.E. Reichen
1958, Analytical Chemistry (30) 1948-1950
This procedure was developed primarily for analyses in which limited amounts of sample are available. Sodium and potassium can be separated from the other constituents of silicate rocks by cation exchange resin (Amberlite IR-120). The sample is decomposed with hydrofluoric and sulfuric acids and passed through the resin bed after...
Fishery management problems and possibilities on large southeastern reservoirs
John W. Parsons
1958, Transactions of the American Fisheries Society (87) 333-355
Principal problems concerning the fisheries of large reservoirs in the Southeast are: inefficient and highly selective exploitation of fish stocks, and protection and reclamation of damaged or threatened fisheries in tailwaters and tributary streams. Seven mainstream reservoirs on which data are available support an average angling pressure of 4.9 trips...
Resistance to furunculosis and ulcer disease in Eastern brook trout, Salvelinus fontinalis
S. F. Snieszko, C. E. Dunbar, G. L. Bullock
1958, Conference Paper, Bacteriological Proceedings
No abstract available at this time...
Structure and ore deposits of the Darwin quadrangle, Inyo County, California
Wayne E. Hall
1958, Open-File Report 58-42
No abstract available....
Columnaris disease of fishes
S. F. Snieszko
1958, Fishery Leaflet 461
Fin rot and peduncle disease of salmonid fishes
S. F. Snieszko
1958, Fishery Leaflet 462
Fish furunculosis,
S. F. Snieszko
1958, Fishery Leaflet 467
Bacterial gill disease of freshwater fishes
S. F. Snieszko
1958, Fishery Leaflet 464
Suggestions for reduction of natural mortality in fish populations
S. F. Snieszko
1958, Transactions of the American Fisheries Society (87) 380-385
Illness, in fish as well as in other animals, when caused by an infectious disease, is often not the result of infection with pathogens alone. In many cases the pathogens and hosts can exist side by side without development of disease symptoms. Such symptoms, with resulting illness or death,...
Some natural variations in the relative abundance of copper isotopes
E. C. Walker, F. Cuttitta, F. E. Senftle
1958, Geochimica et Cosmochimica Acta (15) 183-194
The relative isotopic abundance of copper has been measured in a number of minerals and a few plant materials. Suites of samples from Michigan and the Colorado Plateau have been examined in more detail to determine if local variations due to isotopic exchange or diffusion could be found. The relative...
Determination of the oxidation state of uranium in apatite and phosphorite deposits
R. S. Clarke Jr., Z. S. Altschuler
1958, Geochimica et Cosmochimica Acta (13) 127-142
Geological and mineralogical evidence indicate that the uranium present in apatite may proxy for calcium in the mineral structure as U(IV). An experimental investigation was conducted and chemical evidence was obtained that establishes the presence of U(IV) in apatite.The following analytical procedure was developed for the determination of U(IV). Carbonatefluorapatite...
Equilibrium distribution of dissolved sulphur species in water at 25°C and 1 atm total pressure
R.M. Garrels, C.R. Naeser
1958, Geochimica et Cosmochimica Acta (15) 113-130
The Eh-pH diagrams for the equilibrium concentrations in aqueous solution at 25°C of native sulphur and all the various sulphur-containing ions and acids from which the ions are produced have been constructed for systems having a total sulphur concentration of 0.1 molar. The composite of these diagrams indicates that elemental sulphur,...
A laboratory aid to speed up filtration
H.I. Feinstein
1958, Journal of Chemical Education (35) 509
[No abstract available]...
Potassium bromide method of infrared sampling
R.G. Milkey
1958, Analytical Chemistry (30) 1931-1933
In the preparation of potassium bromide pressed windows for use in the infrared analysis of solids, severe grinding of the potassium bromide powder may produce strong absorption bands that could interfere seriously with the spectra of the sample. These absorption bands appear to be due to some crystal alteration of...
Quartz helix magnetic susceptibility balance using the Curie-Cheneveau principle
F. E. Senftle, M. D. Lee, A. A. Monkewicz, J. W. Mayo, T. Pankey
1958, Review of Scientific Instruments (29) 429-432
A quartz spring balance is described which can be used to measure the magnetic susceptibility of submilligram amounts of sample. The magnetic field is supplied by a moving permanent magnet, and the susceptibility is determined by the deflection of the spring observed in a measuring microscope. The apparatus is calibrated by a comparison standard (platinum) and results are shown for platinum, nickel aluminate, lead, manganese, and sucrose. A precision of better...