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Cobalt-57
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Standard atomic weight Ar°(Co) | ||||||||||||||||||||||||||||||||||||
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Naturally occurring cobalt (27Co) consists of a single stable isotope, 59Co. Twenty-eight radioisotopes have been characterized; the most stable are 60Co with a half-life of 5.2714 years, 57Co (271.8 days), 56Co (77.27 days), and 58Co (70.86 days). All other isotopes have half-lives of less than 18 hours and most of these have half-lives of less than 1 second. This element also has 11 meta states, all of which have half-lives of less than 15 minutes.
The isotopes of cobalt range in atomic weight from 47Co to 75Co. The main decay mode for isotopes with atomic mass less than that of the stable isotope, 59Co, is electron capture and the main mode of decay for those of greater than 59 atomic mass units is beta decay. The main decay products before 59Co are iron isotopes and the main products after are nickel isotopes.
Radioactive isotopes can be produced by various nuclear reactions. For example, 57Co is produced by cyclotron irradiation of iron. The main reaction is the (d,n) reaction 56Fe + 2H → n + 57Co.
List of isotopes
Nuclide |
Z | N |
Isotopic mass (Da) |
Half-life |
Decay mode |
Daughter isotope |
Spin and parity |
Natural abundance (mole fraction) | |||||||||||
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Excitation energy | Normal proportion | Range of variation | |||||||||||||||||
47Co | 27 | 20 | 47.01149(54)# | 7/2−# | |||||||||||||||
48Co | 27 | 21 | 48.00176(43)# | p | 47Fe | 6+# | |||||||||||||
49Co | 27 | 22 | 48.98972(28)# | <35 ns | p (>99.9%) | 48Fe | 7/2−# | ||||||||||||
β+ (<.1%) | 49Fe | ||||||||||||||||||
50Co | 27 | 23 | 49.98154(18)# | 44(4) ms | β+, p (54%) | 49Mn | (6+) | ||||||||||||
β+ (46%) | 50Fe | ||||||||||||||||||
51Co | 27 | 24 | 50.97072(16)# | 60# ms [>200 ns] | β+ | 51Fe | 7/2−# | ||||||||||||
52Co | 27 | 25 | 51.96359(7)# | 115(23) ms | β+ | 52Fe | (6+) | ||||||||||||
52mCo | 380(100)# keV | 104(11)# ms | β+ | 52Fe | 2+# | ||||||||||||||
IT | 52Co | ||||||||||||||||||
53Co | 27 | 26 | 52.954219(19) | 242(8) ms | β+ | 53Fe | 7/2−# | ||||||||||||
53mCo | 3197(29) keV | 247(12) ms | β+ (98.5%) | 53Fe | (19/2−) | ||||||||||||||
p (1.5%) | 52Fe | ||||||||||||||||||
54Co | 27 | 27 | 53.9484596(8) | 193.28(7) ms | β+ | 54Fe | 0+ | ||||||||||||
54mCo | 197.4(5) keV | 1.48(2) min | β+ | 54Fe | (7)+ | ||||||||||||||
55Co | 27 | 28 | 54.9419990(8) | 17.53(3) h | β+ | 55Fe | 7/2− | ||||||||||||
56Co | 27 | 29 | 55.9398393(23) | 77.233(27) d | β+ | 56Fe | 4+ | ||||||||||||
57Co | 27 | 30 | 56.9362914(8) | 271.74(6) d | EC | 57Fe | 7/2− | ||||||||||||
58Co | 27 | 31 | 57.9357528(13) | 70.86(6) d | β+ | 58Fe | 2+ | ||||||||||||
58m1Co | 24.95(6) keV | 9.04(11) h | IT | 58Co | 5+ | ||||||||||||||
58m2Co | 53.15(7) keV | 10.4(3) μs | 4+ | ||||||||||||||||
59Co | 27 | 32 | 58.9331950(7) | Stable | 7/2− | 1.0000 | |||||||||||||
60Co | 27 | 33 | 59.9338171(7) | 5.2713(8) y | β−, γ | 60Ni | 5+ | ||||||||||||
60mCo | 58.59(1) keV | 10.467(6) min | IT (99.76%) | 60Co | 2+ | ||||||||||||||
β− (.24%) | 60Ni | ||||||||||||||||||
61Co | 27 | 34 | 60.9324758(10) | 1.650(5) h | β− | 61Ni | 7/2− | ||||||||||||
62Co | 27 | 35 | 61.934051(21) | 1.50(4) min | β− | 62Ni | 2+ | ||||||||||||
62mCo | 22(5) keV | 13.91(5) min | β− (99%) | 62Ni | 5+ | ||||||||||||||
IT (1%) | 62Co | ||||||||||||||||||
63Co | 27 | 36 | 62.933612(21) | 26.9(4) s | β− | 63Ni | 7/2− | ||||||||||||
64Co | 27 | 37 | 63.935810(21) | 0.30(3) s | β− | 64Ni | 1+ | ||||||||||||
65Co | 27 | 38 | 64.936478(14) | 1.20(6) s | β− | 65Ni | (7/2)− | ||||||||||||
66Co | 27 | 39 | 65.93976(27) | 0.18(1) s | β− | 66Ni | (3+) | ||||||||||||
66m1Co | 175(3) keV | 1.21(1) μs | (5+) | ||||||||||||||||
66m2Co | 642(5) keV | >100 μs | (8-) | ||||||||||||||||
67Co | 27 | 40 | 66.94089(34) | 0.425(20) s | β− | 67Ni | (7/2−)# | ||||||||||||
68Co | 27 | 41 | 67.94487(34) | 0.199(21) s | β− | 68Ni | (7-) | ||||||||||||
68mCo | 150(150)# keV | 1.6(3) s | (3+) | ||||||||||||||||
69Co | 27 | 42 | 68.94632(36) | 227(13) ms | β− (>99.9%) | 69Ni | 7/2−# | ||||||||||||
β−, n (<.1%) | 68Ni | ||||||||||||||||||
70Co | 27 | 43 | 69.9510(9) | 119(6) ms | β− (>99.9%) | 70Ni | (6-) | ||||||||||||
β−, n (<.1%) | 69Ni | ||||||||||||||||||
70mCo | 200(200)# keV | 500(180) ms | (3+) | ||||||||||||||||
71Co | 27 | 44 | 70.9529(9) | 97(2) ms | β− (>99.9%) | 71Ni | 7/2−# | ||||||||||||
β−, n (<.1%) | 70Ni | ||||||||||||||||||
72Co | 27 | 45 | 71.95781(64)# | 62(3) ms | β− (>99.9%) | 72Ni | (6- ,7-) | ||||||||||||
β−, n (<.1%) | 71Ni | ||||||||||||||||||
73Co | 27 | 46 | 72.96024(75)# | 41(4) ms | 7/2−# | ||||||||||||||
74Co | 27 | 47 | 73.96538(86)# | 50# ms [>300 ns] | 0+ | ||||||||||||||
75Co | 27 | 48 | 74.96833(86)# | 40# ms [>300 ns] | 7/2−# | ||||||||||||||
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Use of cobalt radioisotopes in medicine
Cobalt-57 (57Co or Co-57) is used in medical tests; it is used as a radiolabel for vitamin B12 uptake. It is useful for the Schilling test.
Cobalt-60 (60Co or Co-60) is used in radiotherapy. It produces two gamma rays with energies of 1.17 MeV and 1.33 MeV. The 60Co source is about 2 cm in diameter and as a result produces a geometric penumbra, making the edge of the radiation field fuzzy. The metal has the unfortunate habit of producing fine dust, causing problems with radiation protection. The 60Co source is useful for about 5 years but even after this point is still very radioactive, and so cobalt machines have fallen from favor in the Western world where linacs are common.
Industrial uses for radioactive isotopes
Cobalt-60 (60Co) is useful as a gamma ray source because it can be produced in predictable quantities, and for its high radioactivity simply by exposing natural cobalt to neutrons in a reactor. The uses for industrial cobalt include:
- Sterilization of medical supplies and medical waste
- Radiation treatment of foods for sterilization (cold pasteurization)
- Industrial radiography (e.g., weld integrity radiographs)
- Density measurements (e.g., concrete density measurements)
- Tank fill height switches
Cobalt-57 is used as a source in Mössbauer spectroscopy of iron-containing samples. Electron capture by 57Co forms an excited state of the 57Fe nucleus, which in turn decays to the ground state with the emission of a gamma ray. Measurement of the gamma-ray spectrum provides information about the chemical state of the iron atom in the sample.
- Isotope masses from:
- Audi, Georges; Bersillon, Olivier; Blachot, Jean; Wapstra, Aaldert Hendrik (2003), "The NUBASE evaluation of nuclear and decay properties", Nuclear Physics A, 729: 3–128, Bibcode:2003NuPhA.729....3A, doi:10.1016/j.nuclphysa.2003.11.001
- Isotopic compositions and standard atomic masses from:
- de Laeter, John Robert; Böhlke, John Karl; De Bièvre, Paul; Hidaka, Hiroshi; Peiser, H. Steffen; Rosman, Kevin J. R.; Taylor, Philip D. P. (2003). "Atomic weights of the elements. Review 2000 (IUPAC Technical Report)". Pure and Applied Chemistry. 75 (6): 683–800. doi:10.1351/pac200375060683.
- Wieser, Michael E. (2006). "Atomic weights of the elements 2005 (IUPAC Technical Report)". Pure and Applied Chemistry. 78 (11): 2051–2066. doi:10.1351/pac200678112051.
- "News & Notices: Standard Atomic Weights Revised". International Union of Pure and Applied Chemistry. 19 October 2005.
- Half-life, spin, and isomer data selected from the following sources.
- Audi, Georges; Bersillon, Olivier; Blachot, Jean; Wapstra, Aaldert Hendrik (2003), "The NUBASE evaluation of nuclear and decay properties", Nuclear Physics A, 729: 3–128, Bibcode:2003NuPhA.729....3A, doi:10.1016/j.nuclphysa.2003.11.001
- National Nuclear Data Center. "NuDat 2.x database". Brookhaven National Laboratory.
- Holden, Norman E. (2004). "11. Table of the Isotopes". In Lide, David R. (ed.). CRC Handbook of Chemistry and Physics (85th ed.). Boca Raton, Florida: CRC Press. ISBN 978-0-8493-0485-9.
Isotopes of the chemical elements
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