Big Chemical Encyclopedia

Chemical substances, components, reactions, process design ...

Articles Figures Tables About

Manganese isotope

TEA chloride See tetraethylammonium chloride., te,e a klorjd ) technetium chem A transition element, symbol Tc, atomic number 43 derived from uranium and plutonium fission products chemically similar to rhenium and manganese isotope Tc has a half-life of 200,000 years used to absorb slow neutrons in reactor technology. tek ne-she-om ... [Pg.368]

Rosell, R. A. and K. L. Babcock (1968). Precipitated manganese isotopically exchanged with Mn and chelated by soil organic matter. In "Isotopes and Radiation in Soil Organic Matter Studies," pp. 453-469. International Atomic Energy Agency, Vienna, Austria. [Pg.151]

After irradiation and cooling, samples are dissolved in acid and carrier added. Separation of manganese can be made by precipitation as tetraphenylarsonium permanganate (Cotzias et al.. 1966) or manganese dioxide (Miyata et al., 1983) by extraction at pH 8 into chloroform with 8-hydroxyquinoline (Versieck et al.. 1973) or with diethylammonium diethyidithiocarbamate (Damsgaard et al., 1973) by separation with anion exchange resin (Miyata et al., 1973) and after removal of alkali metal salts on a hydrated antimony pentoxide (HAP) column (Miyata et al., 1973). Addition of another manganese isotope ( Mn) can be used to check recoveries of separation procedures. [Pg.391]

Manganese [7439-96-5] atomic number 25, atomic weight 54.94, belongs to Group 7 (VII) ia the Periodic Table. Its isotopes are Mn, Mn, Mn,... [Pg.486]

Manganese, atomic no. 25, belongs to the first transition series and is the principal member of Group 7 (VIIA). It has nine isotopes (1,2) (Table 1). Table 1. Isotopes of Manganese... [Pg.501]

All isotopes of technetium (Z = 43) are unstable, so the element is not found an Avhere in the Earth s crust. Its absence left a gap in the periodic table below manganese. The search for this missing element occupied researchers for many years. It was not until 1937 that the first samples of technetium were prepared in a nuclear reactor. In fact, technetium was the first element to be made artificially in the laboratory. To date, 21 radioactive isotopes of technetium have been identified, some of them requiring millions of years to decompose. [Pg.93]

C22-0036. Manganese has only one stable isotope. Calculate the A/ Z ratio for each of the following four... [Pg.1614]

Krishnaswami S, Lai D, Somayajulu BLK (1976) Large-volume in-situ filtration of deep Pacific waters Mineralogical and radioisotope studies. Earth Planet Sci Lett 32 420-429 Krishnaswami S, Mangini A, Thomas JH, Sharma P, Cochran JK, Turekian KK, Parker PD (1982) °Be and Th isotopes in manganese nodules and adjacent sediments nodule growth histories and nuclide behavior. Earth Planet Sci Lett 59 217-234... [Pg.526]

Kn TL, Omnra A, Chen PS (1979) Be ° and U-series isotopes in manganese nodules from the central north Pacific. In Marine geology and oceanography of the Pacific manganese nodule province (ed. J. L. Bishoff and Z. Piper), pp. 791-804. Plenum... [Pg.526]

Tin hold the record with 10 stable isotopes. There are 19 so-called "pure elements" of which there is only one isotope. These anisotopic elements are beryllium, fluorine, sodium, aluminum, phosphorus, scandium, manganese, cobalt, arsenic, yttrium, niobium, rhodium, iodine, cesium, praseodymium, terbium, holmium, thulium, gold, and bismuth. [Pg.96]

Mercury was determined after suitable digestion by the cold vapour atomic absorption method [40]. Lead was determined after digestion by a stable isotope dilution technique [41-43]. Copper, lead, cadmium, nickel, and cobalt were determined by differential pulse polarography following concentration by Chelex 100 ion-exchange resin [44,45], and also by the Freon TF extraction technique [46]. Manganese was determined by flameless atomic absorption spectrometry (FAA). [Pg.34]

Livingston and Cochran [50] collected large seawater samples by using a cable-supported electrical pumping system for subsequent determination of thorium, americium, and plutonium isotopes. Particles were removed by filtration and actinides were collected by absorption on manganese dioxide-coated filters. The samples were then analysed by standard radiochemical and a spec-trometric techniques. [Pg.351]

Chromium iron manganese brown spinel, formula and DCMA number, 7 348t Chromium iron nickel black spinel, formula and DCMA number, 7 348t Chromium isotopes, 6 476 Chromium magnesium oxide, 5 583 Chromium manganese zinc brown spinel, formula and DCMA number, 7 348t Chromium-nickel alloys, 77 100-101 Chromium-nickel-iron alloys, 17 102-103 Chromium-nickel stainless steels, 15 563 Chromium niobium titanium buff rutile, formula and DCMA number, 7 347t Chromium(III) nitrate, 6 533 Chromium nitride, 4 668... [Pg.184]

Barling J, Anbar AD (2004) Molybdenum isotope fractionation during adsorption by manganese oxides. Earth Planet Sci Lett 217 315-329... [Pg.22]

Birck JL, Allegre CJ (1988) Manganese chromium isotope systematics and development of the early solar system. Nature 331 579-584... [Pg.56]

Virag A, Zinner E, Lewis RS, Tang M (1989) Isotopic compositions of H, C, and N in C8 diamonds from the Allende and Murray carbonaceous chondrites. Lunar Planet Sci XX 1158-1159 Volkening J, Papanastassiou DA (1989) Iron isotope anomalies. Astrophys J 347 L43-L46 Volkening J, Papanastassiou DA (1990) Zinc isotope anomalies. Astrophys J 358 L29-L32 Wadhwa M, Zinner EK, Crozaz G (1997) Manganese-chromium systematics in sulfides of unequilibrated enstatite chondrites. Meteorit Planet Sci 32 281-292... [Pg.63]

Beaudoin G, Taylor BE, Rumble III D, Thiemens M (1994) Variations in the sulfur isotope composition of troilite from the Canon Diablo iron meteorite. Geochim Cosmochim Acta 58 4253-4255 Birck JL, Allegre CJ (1988) Manganese-chromium isotope systematics and the development of the early solar system. Nature 331(6157) 579-584... [Pg.314]

Aveston J, Anacker EW, Johnson JS (1964) Hydrolysis of molybdenum (VI). Ultracentrifugation, acidity measurements, and Raman spectra of polymolybdates. Inorg Chem 3 735-746 Baes Jr. CF, Mesmer RE (1986) The Hydrolysis of Cations. Krieger Publishing Company, Melbourne, EL Barling J, Anbar AD (2004) Molybdenum isotope fractionation during adsorption by manganese oxides. Earth Planet Sci Lett, in press... [Pg.451]


See other pages where Manganese isotope is mentioned: [Pg.150]    [Pg.214]    [Pg.157]    [Pg.922]    [Pg.1653]    [Pg.150]    [Pg.214]    [Pg.157]    [Pg.922]    [Pg.1653]    [Pg.442]    [Pg.151]    [Pg.93]    [Pg.94]    [Pg.464]    [Pg.527]    [Pg.527]    [Pg.598]    [Pg.141]    [Pg.153]    [Pg.259]    [Pg.263]    [Pg.263]    [Pg.347]    [Pg.349]    [Pg.820]    [Pg.498]    [Pg.839]    [Pg.185]    [Pg.130]    [Pg.106]    [Pg.34]    [Pg.63]    [Pg.407]    [Pg.419]   
See also in sourсe #XX -- [ Pg.1012 ]

See also in sourсe #XX -- [ Pg.1124 ]




SEARCH



Manganese isotopes and their properties

© 2024 chempedia.info