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Sulfur isotopic

In addition to the 4 stable isotopes sulfur has at least 9 radioactive isotopes, the one with the longest half-life being which decays by activity (Kmax 0.167 MeV, 87.5 d). can be prepared by Cl(n,p), S(n,> ) or S(d,p) and is commercially available as SeicmcQt H2S, SOCb and KSCN. The radiation has a similar energy to that of C ( mav 0.155 MeV) and similar counting techniques can be used (p. 276). The maximum range is 300 min in air and 0.28 mm in water, and effective shielding is provided by a perspex screen 3-10 mm thick. The preparation of many - S-containii compounds has been... [Pg.661]

To study the biosynthesis of thiophenes in Tagetes, S-labeled thiophene derivatives have been prepared by in vitro culture of Tagetes sp. 3. Different sources of isotopic sulfur were tested and the best results were achieved with Na2 S04- The resulting bithiophenes such as alkyne 12 are derived from triceapentaynene obtained from oleic acid <1995MI807, 1996JRN455, 1997MI175>. [Pg.933]

Strontium isotopes Osmium isotopes Sulfur isotopes Carbon isotopes Oxygen isotopes... [Pg.3831]

In addition to the 4 stable isotopes sulfur has at least 9 radioactive isotopes, the one with the longest half-life being which decays by activity ( max 0.167 MeV, 87.5 d), can be... [Pg.661]

Isotopic. Sulfur-35 emits j8-particles of 0.167 M.e.v. maximum energy and has a half-life of 87.1 days. It is readily assayed as a solid with a thin-mica-end-window Geiger counter. [Pg.119]

Eleven isotopes of sulfur exist. None of the four isotopes that in nature are radioactive. A finely divided form of sulfur, known as flowers of sulfur, is obtained by sublimation. [Pg.39]

Naturally selenium contains six stable isotopes. Fifteen other isotopes have been characterized. The element is a member of the sulfur family and resembles sulfur both in its various forms and in its compounds. [Pg.97]

We also developed a number of other useful new fluorinating reagents. They ineluded a convenient in situ form of sulfur tetrafluoride in pyridinium polyhydrogen fluoride, selenium tetrafluoride, and ey-anurie fluoride. We introdueed uranium hexafluoride (UFg), depleted from the U-235 isotope, which is an abundant by-product of enrichment plants, as an effective fluorinating agent. [Pg.104]

Interpreting the mass spectra of sulfur compounds is aided by the observation of an M+2 peak because of the presence of the mass 34 isotope of sulfur The major cleav age pathway of thiols is analogous to that of alcohols... [Pg.653]

Compounds that contain chlorine, bromine, sulfur, or silicon are usually apparent from prominent peaks at masses 2, 4, 6, and so on, units larger than the nominal mass of the parent or fragment ion. Eor example, when one chlorine atom is present, the P + 2 mass peak will be about one-third the intensity of the parent peak. When one bromine atom is present, the P + 2 mass peak will be about the same intensity as the parent peak. The abundance of heavy isotopes is treated in terms of the binomial expansion (a -I- h) , where a is the relative abundance of the light isotope, b is the relative abundance of the heavy isotope, and m is the number of atoms of the particular element present in the molecule. If two bromine atoms are present, the binomial expansion is... [Pg.812]

CDT. canyon diabolo troilite (a standard for sulfur isotopes see VCDT)... [Pg.445]

V. a term used to describe a voltage difference between one electrode and another VCDT. Vienna canyon diabolo troilite (actually silver sulfide used as a replacement standard for CDT [sulfur isotopes])... [Pg.447]

Laser isotope separation techniques have been demonstrated for many elements, including hydrogen, boron, carbon, nitrogen, oxygen, sHicon, sulfur, chlorine, titanium, selenium, bromine, molybdenum, barium, osmium, mercury, and some of the rare-earth elements. The most significant separation involves uranium, separating uranium-235 [15117-96-1], from uranium-238 [7440-61-1], (see Uranium and uranium compounds). The... [Pg.19]

Any radioactive nucUde or isotope of an element can be used as a radioactive tracer, eg, chromium-51 [14392-02-0] cobalt-60 [10198-40-0] tin-110 [15700-33-1] and mercury-203 [13982-78-0],hut the preponderance ofuse has been for carbon-14 [14762-75-5],hydj ogen-3 [10028-17-8] (tritium), sulfur-35 [15117-53-0], phosphoms-32, and iodine-125 [14158-31 -7]. More recendy phosphoms-33 has become available and is used to replace sulfur-35 and phosphoms-32 in many appUcations. By far the greater number of radioactive tracers produced are based on carbon-14 and hydrogen-3 because carbon and hydrogen exist in a large majority of the known natural and synthetic chemical compounds. [Pg.437]

The radioactive isotopes available for use as precursors for radioactive tracer manufacturing include barium [ C]-carbonate [1882-53-7], tritium gas, p2p] phosphoric acid or pP]-phosphoric acid [15364-02-0], p S]-sulfuric acid [13770-01 -9], and sodium [ I]-iodide [24359-64-6]. It is from these chemical forms that the corresponding radioactive tracer chemicals are synthesized. [ C]-Carbon dioxide, [ C]-benzene, and [ C]-methyl iodide require vacuum-line handling in weU-ventilated fume hoods. Tritium gas, pH]-methyl iodide, sodium borotritide, and [ I]-iodine, which are the most difficult forms of these isotopes to contain, must be handled in specialized closed systems. Sodium p S]-sulfate and sodium [ I]-iodide must be handled similarly in closed systems to avoid the Uberation of volatile p S]-sulfur oxides and [ I]-iodine. Adequate shielding must be provided when handling P P]-phosphoric acid to minimize exposure to external radiation. [Pg.437]

There are four stable isotopes of sulfur and S, which have relative abundances of 95.1, 0.74, 4.2, and 0.016%, respectively. The relative... [Pg.117]

The only sulfur isotope with a nuclear spin is which is quadrupolar (/ = 3/2) and of low natural abundance (0.76%). In view of these inherent difficulties and the low symmetry around the sulfur nuclei in most S-N compounds, S NMR spectroscopy has found very limited application in S-N chemistry. However, it is likely that reasonably narrow resonances could be obtained for sulfur in a tetrahedral environment, e.g. [S(N Bu)4], cf. [S04] . On the other hand both selenium and tellurium have isotopes with I = Vi with significant natural abundances ( Se, 7.6% and Te, 7.0%). Consequently, NMR studies using these nuclei can provide useful information for Se-N and Te-N systems. [Pg.35]

R. W. FairbriiXjE, Encyclopedia of Geochemistry and Environmental Sciences, Van Nostrand, New York, 1972.. See sections on Geochemical Classification of the Elements Sulfates Sulfate Reduction-Microbial Sulfides Sulfosalts Sulfur Sulfur Cycle Sulfur Isotope Fractionation in Biological Processes, etc., pp. 1123 - 58. [Pg.648]

R. Krol SE and V. A, Grinenko (eds.). Stable Isotopes Natural and Anthropogenic Sulfur in the Environment, SCOPE Report 43. Wiley. Chichesier. 1991. 466 pp,... [Pg.649]

Only within the past few years have serious attempts been made to estimate quantitatively the differences in reactivity between thiophene and benzene and between the 2- and 3-position of thiophene. Careful investigation on the acid-induced exchange of deuterium and tritium have shown that the ratios of the exchange rates in the 2- and 3-positions are 1045 61 for deuterium and 911 60 for tritium in 57% by weight aqueous sulfuric acid at 24.6°C. A kinetic isotope effect in the isotopic exchange has been found to be k-r/kr, = 0.51 0.03 in the 2-position and kr/kjy — 0.59 0.04 in the... [Pg.44]

Atomic masses calculated in this manner, using data obtained with a mass spectrometer can in principle be precise to seven or eight significant figures. The accuracy of tabulated atomic masses is limited mostly by variations in natural abundances. Sulfur is an interesting case in point. It consists largely of two isotopes, fiS and fgS. The abundance of sulfur-34 varies from about 4.18% in sulfur deposits in Texas and Louisiana to 4.34% in volcanic sulfur from Italy. This leads to an uncertainty of 0.006 amu in the atomic mass of sulfur. [Pg.53]

Look for characteristic isotopic abundances that show the presence of bromine, chlorine, sulfur, silicon, and so on. If the deduced molecular ion is of sufficient intensity, the probable molecular formula may be determined using the observed isotopic abundances of the molecular ion region. Set the deduced molecular ion, M, at 100% abundance, and then calculate the relative abundances of M + 1 and M + 2 either manually or using the data system. [Pg.21]

Molecular ion The presence of sulfur can be detected by the 34S isotope (4.4%) and the large mass defect of sulfur in accurate mass measurements. In primary aliphatic thiols, the molecular ion intensities range from 5-100% of the base peak. [Pg.123]

The mass spectrum of the unknown compound showed a molecular ion at m/z 246 with an isotope pattern indicating that one chlorine atom and possibly a sulfur atom are present. The fragment ion at m/z 218 also showed the presence of chlorine and sulfur. The accurate mass measurement showed the molecular formula to be C]3FI7OSCl R + DB = 10. [Pg.214]


See other pages where Sulfur isotopic is mentioned: [Pg.307]    [Pg.37]    [Pg.4887]    [Pg.143]    [Pg.27]    [Pg.340]    [Pg.347]    [Pg.307]    [Pg.37]    [Pg.4887]    [Pg.143]    [Pg.27]    [Pg.340]    [Pg.347]    [Pg.81]    [Pg.16]    [Pg.102]    [Pg.19]    [Pg.117]    [Pg.402]    [Pg.535]    [Pg.21]    [Pg.359]    [Pg.38]    [Pg.81]    [Pg.17]    [Pg.661]    [Pg.661]    [Pg.73]    [Pg.194]    [Pg.208]    [Pg.352]   
See also in sourсe #XX -- [ Pg.6 , Pg.9 ]




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Anhydrite sulfur isotopes

Barite sulfur isotopes

Coal sulfur isotopes

Gypsum sulfur isotopes

Isotope effects with sulfur

Isotope-labelled sulfur

Isotopic biomarker sulfur isotopes

Isotopic ratio of sulfur

Meteorites, sulfur isotopes

Petroleum sulfur isotopes

Primary kinetic isotope effect of sulfur

Sediments sulfur isotopes

Stable isotopes sulfur

Sulfate/hydrogen sulfide, sulfur isotopic

Sulfate/hydrogen sulfide, sulfur isotopic composition

Sulfur Isotope Composition of Ore Deposits

Sulfur elemental isotope effects

Sulfur elemental isotope fractionation

Sulfur isotope analysis

Sulfur isotope anomalous

Sulfur isotope anomalous fractionations

Sulfur isotope data

Sulfur isotope dilution analysis

Sulfur isotope effects

Sulfur isotope pattern

Sulfur isotope separation

Sulfur isotopes

Sulfur isotopes

Sulfur isotopes and their properties

Sulfur isotopes biogenic

Sulfur isotopes exchange

Sulfur isotopes fractionations

Sulfur isotopes inverse

Sulfur isotopes kinetics

Sulfur isotopes mass dependent

Sulfur isotopes mass independent

Sulfur isotopes metabolism

Sulfur isotopes models

Sulfur isotopes preparation

Sulfur isotopes reservoirs

Sulfur isotopes, studies

Sulfur isotopic analysis

Sulfur isotopic budget

Sulfur isotopic composition

Sulfur isotopic data analysis of crude

Sulfur isotopic data analysis of crude oils

Sulfur isotopic fractionation

Sulfur isotopic processes, applications

Sulfur isotopic studies

Sulfur, isotope ratios

Sulfur, relative isotopic abundance

Thermal sulfur isotopes

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