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Sulfur(16S) has 23 knownisotopeswith mass numbers ranging from 27 to 49, four of which are stable:32S (95.02%),33S (0.75%),34S (4.21%), and36S (0.02%). The preponderance of sulfur-32 is explained by its production from carbon-12 plus successive fusion capture of fivehelium-4nuclei, in the so-calledalpha processof exploding type II supernovas (seesilicon burning).
34S abundances vary greatly (between 3.96 and 4.77 percent) in natural samples. | ||||||||||||||||||||||||||||||||||||
Standard atomic weightAr°(S) | ||||||||||||||||||||||||||||||||||||
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Other than35S, theradioactive isotopesof sulfur are all comparatively short-lived.35S is formed fromcosmic ray spallationof40Arin theatmosphere.It has ahalf-lifeof 87 days. The next longest-lived radioisotope is sulfur-38, with a half-life of 170 minutes. The shortest-lived is49S, with a half-life shorter than 200 nanoseconds. Heavier radioactive isotopes of sulfur decay tochlorine.
When sulfidemineralsare precipitated, isotopic equilibration among solids and liquid may cause small differences in the δ34S values of co-genetic minerals. The differences between minerals can be used to estimate the temperature of equilibration. Theδ13Cand δ34S of coexistingcarbonatesand sulfides can be used to determine thepHandoxygenfugacityof the ore-bearing fluid during ore formation.
In mostforestecosystems, sulfate is derived mostly from the atmosphere; weathering of ore minerals and evaporites also contribute some sulfur. Sulfur with a distinctive isotopic composition has been used to identify pollution sources, and enriched sulfur has been added as a tracer inhydrologicstudies. Differences in thenatural abundancescan also be used in systems where there is sufficient variation in the34S of ecosystem components.Rocky Mountainlakes thought to be dominated by atmospheric sources of sulfate have been found to have different δ34S values from oceans believed to be dominated by watershed sources of sulfate.
List of isotopes
editNuclide[3] [n 1] |
Z | N | Isotopic mass(Da)[4] [n 2][n 3] |
Half-life |
Decay mode [n 4] |
Daughter isotope [n 5] |
Spinand parity [n 6][n 7] |
Natural abundance(mole fraction) | |||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
Excitation energy | Normal proportion | Range of variation | |||||||||||||||||
27S[n 8] | 16 | 11 | 27.01828(43)# | 15.5(15) ms | β+(96.6%) | 27P | (5/2+) | ||||||||||||
β+,p (2.3%) | 26Si | ||||||||||||||||||
β+,2p (1.1%) | 25Al | ||||||||||||||||||
28S | 16 | 12 | 28.00437(17) | 125(10) ms | β+(79.3%) | 28P | 0+ | ||||||||||||
β+,p (20.7%) | 27Si | ||||||||||||||||||
29S | 16 | 13 | 28.99661(5) | 188(4) ms | β+(53.6%) | 29P | 5/2+# | ||||||||||||
β+,p (46.4%) | 28Si | ||||||||||||||||||
30S | 16 | 14 | 29.98490677(22) | 1.1759(17) s | β+ | 30P | 0+ | ||||||||||||
31S | 16 | 15 | 30.97955701(25) | 2.5534(18) s | β+ | 31P | 1/2+ | ||||||||||||
32S[n 9] | 16 | 16 | 31.9720711744(14) | Stable | 0+ | 0.9499(26) | 0.94454-0.95281 | ||||||||||||
33S | 16 | 17 | 32.9714589099(15) | Stable | 3/2+ | 0.0075(2) | 0.00730-0.00793 | ||||||||||||
34S | 16 | 18 | 33.96786701(5) | Stable | 0+ | 0.0425(24) | 0.03976-0.04734 | ||||||||||||
35S | 16 | 19 | 34.96903232(4) | 87.37(4) d | β− | 35Cl | 3/2+ | Trace[n 10] | |||||||||||
36S | 16 | 20 | 35.96708070(20) | Stable | 0+ | 0.0001(1) | 0.00013−0.00027 | ||||||||||||
37S | 16 | 21 | 36.97112551(21) | 5.05(2) min | β− | 37Cl | 7/2− | ||||||||||||
38S | 16 | 22 | 37.971163(8) | 170.3(7) min | β− | 38Cl | 0+ | ||||||||||||
39S | 16 | 23 | 38.97513(5) | 11.5(5) s | β− | 39Cl | (7/2)− | ||||||||||||
40S | 16 | 24 | 39.975483(4) | 8.8(22) s | β− | 40Cl | 0+ | ||||||||||||
41S | 16 | 25 | 40.979593(4) | 1.99(5) s | β−(>99.9%) | 41Cl | 7/2−# | ||||||||||||
β−,n (<.1%) | 40Cl | ||||||||||||||||||
42S | 16 | 26 | 41.981065(3) | 1.016(15) s | β−(>96%) | 42Cl | 0+ | ||||||||||||
β−,n (<4%) | 41Cl | ||||||||||||||||||
43S | 16 | 27 | 42.986908(5) | 265(13) ms | β−(60%) | 43Cl | 3/2−# | ||||||||||||
β−,n (40%) | 42Cl | ||||||||||||||||||
43mS | 319(5) keV | 415.0(26) ns | IT | 43S | (7/2−) | ||||||||||||||
44S | 16 | 28 | 43.990119(6) | 100(1) ms | β−(81.7%) | 44Cl | 0+ | ||||||||||||
β−,n (18.2%) | 43Cl | ||||||||||||||||||
44mS | 1365.0(8) keV | 2.619(26) μs | IT | 44S | 0+ | ||||||||||||||
45S | 16 | 29 | 44.99572(111) | 68(2) ms | β−,n (54%) | 44Cl | 3/2−# | ||||||||||||
β−(46%) | 45Cl | ||||||||||||||||||
46S | 16 | 30 | 46.00037(54)# | 50(8) ms | β− | 46Cl | 0+ | ||||||||||||
47S | 16 | 31 | 47.00791(54)# | 20# ms [>200 ns] |
β− | 47Cl | 3/2−# | ||||||||||||
48S | 16 | 32 | 48.01370(64)# | 10# ms [>200 ns] |
β− | 48Cl | 0+ | ||||||||||||
49S[5] | 16 | 33 | 49.02264(72)# | β− | 49Cl | 3/2−# | |||||||||||||
This table header & footer: |
- ^mS – Excitednuclear isomer.
- ^( ) – Uncertainty (1σ) is given in concise form in parentheses after the corresponding last digits.
- ^# – Atomic mass marked #: value and uncertainty derived not from purely experimental data, but at least partly from trends from the Mass Surface (TMS).
- ^
Modes of decay:
IT: Isomeric transition n: Neutron emission p: Proton emission - ^Bold symbolas daughter – Daughter product is stable.
- ^( ) spin value – Indicates spin with weak assignment arguments.
- ^# – Values marked # are not purely derived from experimental data, but at least partly from trends of neighboring nuclides (TNN).
- ^Has 2haloprotons
- ^Heaviest theoretically stable nuclide with equal numbers of protons and neutrons
- ^Cosmogenic
• The beams of several radioactive isotopes (such as those of44S) have been studied theoretically within the framework of the synthesis of superheavy elements, especially those ones in the vicinity ofisland of stability.[6][7]
See also
editReferences
edit- ^"Standard Atomic Weights: Sulfur".CIAAW.2009.
- ^Prohaska, Thomas; Irrgeher, Johanna; Benefield, Jacqueline; Böhlke, John K.; Chesson, Lesley A.; Coplen, Tyler B.; Ding, Tiping; Dunn, Philip J. H.; Gröning, Manfred; Holden, Norman E.; Meijer, Harro A. J. (2022-05-04)."Standard atomic weights of the elements 2021 (IUPAC Technical Report)".Pure and Applied Chemistry.doi:10.1515/pac-2019-0603.ISSN1365-3075.
- ^Half-life, decay mode, nuclear spin, and isotopic composition is sourced in:
Audi, G.; Kondev, F. G.; Wang, M.; Huang, W. J.; Naimi, S. (2017)."The NUBASE2016 evaluation of nuclear properties"(PDF).Chinese Physics C.41(3): 030001.Bibcode:2017ChPhC..41c0001A.doi:10.1088/1674-1137/41/3/030001. - ^Wang, M.; Audi, G.; Kondev, F. G.; Huang, W. J.; Naimi, S.; Xu, X. (2017)."The AME2016 atomic mass evaluation (II). Tables, graphs, and references"(PDF).Chinese Physics C.41(3): 030003-1–030003-442.doi:10.1088/1674-1137/41/3/030003.
- ^Neufcourt, L.; Cao, Y.; Nazarewicz, W.; Olsen, E.; Viens, F. (2019). "Neutron drip line in the Ca region from Bayesian model averaging".Physical Review Letters.122(6): 062502–1–062502–6.arXiv:1901.07632.Bibcode:2019PhRvL.122f2502N.doi:10.1103/PhysRevLett.122.062502.PMID30822058.S2CID73508148.
- ^Zagrebaev, Valery; Greiner, Walter (2008-09-24)."Synthesis of superheavy nuclei: A search for new production reactions".Physical Review C.78(3): 034610.arXiv:0807.2537.Bibcode:2008PhRvC..78c4610Z.doi:10.1103/PhysRevC.78.034610.S2CID122586703.
- ^Zhu, Long (2019-12-01)."Possibilities of producing superheavy nuclei in multinucleon transfer reactions based on radioactive targets *".Chinese Physics C.43(12): 124103.Bibcode:2019ChPhC..43l4103Z.doi:10.1088/1674-1137/43/12/124103.ISSN1674-1137.S2CID250673444.