27
Co
Cobalt
Atomic Mass 58.933194
Electron Configuration [Ar]4s23d7
Oxidation States +3, +2
Year Discovered 1735

Identifiers

Element Name Cobalt
Element Symbol Co
InChI InChI=1S/Co
InChIKey GUTLYIVDDKVIGB-UHFFFAOYSA-N

Properties

Atomic Weight

58.933 194(3)

58.933194

58.93

58.933194(4)

Electron Configuration

[Ar]4s23d7

Atomic Radius

Van der Waals Atomic Radius : 192 pm (Van der Waals)

Empirical Atomic Radius : 135pm (Empirical)

Covalent Atomic Radius : 126(3)[l.s.], 150(7)[h.s.] pm (Covalent)

Oxidation States

+3, +2

-3, -1, +1, +2, +3, +4, +5 ​(an amphoteric oxide)

Ground Level

4F9/2

Ionization Energy

7.881 eV

7.88101 ± 0.00012 eV

Electronegativity

Pauling Scale Electronegativity : 1.88(Pauling Scale)

Allen Scale Electronegativity : 1.84(Allen Scale)

Electron Affinity

0.661eV

1.06eV

Atomic Spectra

Lines Holdings

Levels Holdings

Physical Description

Solid

Element Classification

Metal

Element Period Number

4

Element Group Number

9

Density

8.86 grams per cubic centimeter

Melting Point

1768 K (1495°C or 2723°F)

1495°C

Boiling Point

3200 K (2927°C or 5301°F)

2927°C

Estimated Crustal Abundance

2.5×101 milligrams per kilogram

Estimated Oceanic Abundance

2×10-5 milligrams per liter

History

The name derives from the German Kobold for "evil spirits" or "goblins", who were superstitiously thought to cause trouble for miners because the mineral contained arsenic that injured their health and the metallic ores did not yield metals when treated with the normal methods. Cobalt was discovered in 1735 by the Swedish chemist Georg Brandt.

Cobalt was discovered by Georg Brandt, a Swedish chemist, in 1739. Brandt was attempting to prove that the ability of certain minerals to color glass blue was due to an unknown element and not to bismuth, as was commonly believed at the time. Cobalt's primary ores are cobaltite (CoAsS) and erythrite (Co3(AsO4)2). Cobalt is usually recovered as a byproduct of mining and refining nickel, silver, lead, copper and iron.

From the German word Kobald, goblin or evil spirit; also from the Greek cobalos, mine. George Brandt discovered cobalt in 1735.

Historical Atomic Weights

Year Atomic Weight (uncertainty) [u] Reference
2017 58.933 194(3) https://doi.org/10.1515/pac-2019-0603
2013 58.933 194(4) https://doi.org/10.1515/pac-2015-0305
2005 58.933 195(5) https://doi.org/10.1351/pac200678112051
1995 58.933 200(9) https://doi.org/10.1351/pac199668122339
1985 58.933 20(1) https://doi.org/10.1351/pac198658121677
1969 58.9332(1) https://doi.org/10.1351/pac197021010091
1961 58.9332 https://doi.org/10.1021/ja00881a001
1925 58.94 https://doi.org/10.1039/CT9252700913
1909 58.97 https://doi.org/10.1021/ja01931a001
1902 59.0 https://doi.org/10.1007/BF01370337

Historical Isotopic Abundances

Year Isotope Abundance (uncertainty) Reference
1975, 59Co, 1, doi:10.1351/pac197647010075

Description

Cobalt is a brittle, hard metal, resembling iron and nickel in appearance. It has a metallic permeability of about two thirds that of iron. Cobalt tends to exist as a mixture of two allotropes over a wide temperature range. The transformation is sluggish and accounts in part for the wide variation in reported data on physical properties of cobalt.

Users

Although cobalt is used in electroplating to give objects an attractive surface that resists oxidation, it is more widely used to form alloys. Alnico, an alloy consisting of aluminum, nickel and cobalt is used to make powerful permanent magnets. Stellite alloys, which contain cobalt, chromium and tungsten, are used to make high-speed and high temperature cutting tools and dyes. Cobalt is also used to make alloys for jet engines and gas turbines, magnetic steels and some types of stainless steels.

Cobalt-60, a radioactive isotope of cobalt, is an important source of gamma rays and is used to treat some forms of cancer and as a medical tracer. Cobalt-60 has a half-life of 5.27 years and decays into nickel-60 through beta decay.

Cobalt compounds have been used for centuries to color porcelain, glass, pottery, tile and enamel. Some of these compounds are known as: cobalt blue, ceruleum, new blue, smalt, cobalt yellow and cobalt green. In addition to being used as a dye, cobalt is also important to human nutrition as it is an essential part of vitamin B12.

It is alloyed with iron, nickel and other metals to make Alnico, an alloy of unusual magnetic strength with many important uses. Stellite alloys, containing cobalt, chromium, and tungsten, are used for high-speed, heavy-duty, high temperature cutting tools, and for dies.

Cobalt is also used in other magnetic steels and stainless steels, and in alloys used in jet turbines and gas turbine generators. The metal is used in electroplating because of its appearance, hardness, and resistance to oxidation.

Cobalt salts have been used for centuries to produce brilliant and permanent blue colors in porcelain, glass, pottery, tiles, and enamels. It is the principal ingredient in Sevre's and Thenard's blue. A solution of the chloride is used as a sympathetic ink. Cobalt carefully used in the form of the chloride, sulfate, acetate, or nitrate has been found effective in correcting a certain mineral deficiency disease in animals.

Soils should contain 0.13 to 0.30 ppm of cobalt for proper animal nutrition.

Sources

Cobalt occurs in the minerals cobaltite, smaltite, and erythrite, and is often associated with nickel, silver, lead, copper, and iron ores, from which it is most frequently obtained as a by-product. It is also present in meteorites.

Important ore deposits are found in Zaire, Morocco, and Canada. The U.S. Geological Survey has announced that the bottom of the north central Pacific Ocean may have cobalt-rich deposits at relatively shallow depths in water close to the the Hawaiian Islands and other U.S. Pacific territories.

Compounds

See more information at the Cobalt compound page.

Element Forms

CID Name Formula SMILES Molecular Weight
104730 cobalt Co [Co] 58.93319
104729 cobalt(2+) Co+2 [Co+2] 58.93319
61492 cobalt-60 Co [60Co] 59.933816
105146 cobalt(3+) Co+3 [Co+3] 58.93319
104844 cobalt-58 Co [58Co] 57.93575
104851 cobalt-57 Co [57Co] 56.936290
166968 cobalt-55 Co [55Co] 54.941996
166998 cobalt-56 Co [56Co] 55.939838
71510781 cobalt-57(2+) Co+2 [57Co+2] 56.936290
182512 cobalt-60(2+) Co+2 [60Co+2] 59.933816
71510783 cobalt-58(2+) Co+2 [58Co+2] 57.93575
177473 cobalt-62 Co [62Co] 61.9341
178158 cobalt-61 Co [61Co] 60.932476
11528329 cobalt-59 Co [59Co] 58.933194
156022700 cobalt-59(3+) Co+3 [59Co+3] 58.933194

Handling And Storage

Exposure to cobalt (metal fumes and dust) should be limited to 0.05 mg/m3 (8-hour time-weighted average 40-hour week).

Isotopes

Stable Isotope Count 1
Summary Cobalt-60, an artificial isotope, is an important gamma ray source, and is extensively used as a tracer and a radiotherapeutic agent.

Isotopes in Industry

60Co (with a half-life of 5.27 years) is used to irradiate food sources as a method of preserving food (Fig. IUPAC.27.1). The gamma radiation from 60Co kills bacteria and other organisms that cause disease and spoilage of food (see Fig. IUPAC.27.1). The use of radioactive compounds for preserving food is not always viewed positively. Some individuals are concerned that harmful compounds will be produced during the irradiation process. However, there is no evidence to support the claim that irradiation is dangerous for food preservation [108]. Many medical products today are sterilized using gamma rays from a 60Co source. This technique of sterilization is generally much cheaper and more effective than steam-heat sterilization because it is a cold process. For example, it can be performed on packaged items, such as disposable syringes. This sterilization technique is applicable to a wide range of heat-sensitive items, such as powders, ointments, and solutions, as well as biological preparations, such as bone, nerve, skin, etc., used in tissue grafts [108].

60Co is also used in industrial radiography to detect structural flaws in metal parts. The radiation can penetrate metals and the X-ray pattern produced by the radiating material can provide information on its strength, composition, and other properties [108]. Because of the above property, 60Co is also used in leveling devices and thickness gauges used to test welds and castings [108].

Fig. IUPAC.27.1: Plants growing in the gamma greenhouse at Brookhaven National Laboratory. The plants are arranged in concentric rings around the radioactive ⁶⁰Co source, which is in the pipe extending into the floor (circa 1959) [223]. (Photo Source: Life Sciences Foundation (LSF) Magazine).

[108] World Nuclear Association. Radioisotopes in Industry: Industrial Uses of Radioisotopes, World Nuclear Association (2014), Feb. 24; http://www.world-nuclear.org/info/inf56.html.
[223] Atomic Gardens, Public Perceptions and Public Policy, in LSF Magazine.

Isotopes in Medicine

60Co is a radioactive metal isotope that is used in cancer treatments by radiotherapy. When 60Co undergoes radioactive decay, high-energy gamma rays (energies of 1.17 MeV and 1.33 MeV) are emitted and have been used in brachytherapy to treat various types of cancer. Brachytherapy (brachy is Greek meaning “short distance”) is a method of radiation treatment in which sealed sources are used to deliver a radiation dose at a distance of up to a few centimeters by surface, intracavitary (insertion of the radioactive isotope in a body cavity), or interstitial (between cells) application [75]. 60Co is used as a source of high-energy ionizing gamma radiation that can be directed to cancer cells from a device outside the body (external radiotherapy).

60Co (and sometimes 57Co and 58Co, with half-lives of 0.75 year and 71 days, respectively) is the key component of the Schilling test, which is a method for determining whether a patient’s body is making and using vitamin B12 properly. The cobalt isotope is used to label cobalt in vitamin B12 to monitor how the body processes this essential vitamin [224].

57Co delivers the smallest radiation dose of all the cobalt isotopes. As a result, it has been used in the past for imaging and estimating organ size and location and in evaluating tumors of the head and neck [75], [99], [225], [226], [227].

[75] J. Peterson, M. McDonell, L. Haroun, F. Monette, R. D. Hildebrand, A. Taboas. Radiological and Chemical Fact Sheets to Support Health Risk Analyses for Contaminated Areas, Prepared by Argonne National Laboratory Environmental Science Division in collaboration with U.S. Department of Energy, Richland Operations Office and Chicago Operations Office (2014), Feb. 22; http://www.remm.nlm.gov/ANL_ContaminantFactSheets_All_070418.pdf.
[99] World Nuclear Association. Radioisotopes in Medicine, World Nuclear Association (2014), Feb. 23; http://www.world-nuclear.org/info/inf55.html.
[224] B. R. Krynyckyi, L. S. Zuckier. J. Nucl. Med.36, 1659 (1995).
[225] Royal Society of Chemistry. Cobalt, Royal Society of Chemistry (2017), Feb. 26; http://www.rsc.org/periodic-table/element/27/cobalt.
[226] US Environmental Protection Agency. Cobalt, US Environmental Protection Agency (2017), Feb. 26; https://www.epa.gov/radiation/radionuclide-basics-cobalt-60.
[227] Washington State Department of Health. Cobalt-60, Washington State Department of Health (2014), Feb. 26; http://www.doh.wa.gov/Portals/1/Documents/Pubs/320-078_co60_fs.pdf.

Isotope Mass and Abundance

Isotope Atomic Mass (uncertainty) [u] Abundance (uncertainty)
59Co 58.933 194(3) 1
Isotope Atomic Mass (uncertainty) [u] Abundance (uncertainty)
59Co 58.93319429(56) 1

Atomic Mass, Half Life, and Decay

Nuclide Atomic Mass and Uncertainty [u] Half Life and Uncertainty Discovery Year Decay Modes, Intensities and Uncertainties [%]
47Co 47.011401 ± 0.000644 [Estimated] Not-specified p ?
48Co 48.001857 ± 0.000537 [Estimated] Not-specified p ?
49Co 48.989501 ± 0.000537 [Estimated] Not-specified <35ns p ?
50Co 49.981117000 ± 0.000135 38.8 ms ± 0.2 1987 β+=100%; β+p=70.5±0.7%; β+2p ?
51Co 50.970647000 ± 0.000052 68.8 ms ± 1.9 1987 β+=100%; β+p<3.8%
52Co 51.963130224 ± 0.000005669 111.7 ms ± 2.1 1987 β+=100%; β+p ?
52Com 51.963130224 ± 0.000005669 102 ms ± 5 2016 β+≈100%; IT ?; β+p ?
53Co 52.954203278 ± 0.000001854 244.6 ms ± 2.8 1970 β+=100%
53Com 52.954203278 ± 0.000001854 250 ms ± 10 1970 β+=?; p≈1.5%
54Co 53.948459075 ± 0.00000038 193.27 ms ± 0.06 1952 β+=100%
54Com 53.948459075 ± 0.00000038 1.48 m ± 0.02 1962 β+=100%
55Co 54.941996416 ± 0.000000434 17.53 h ± 0.03 1938 β+=100%
56Co 55.939838032 ± 0.00000051 77.236 d ± 0.026 1941 β+=100%
57Co 56.936289819 ± 0.000000553 271.811 d ± 0.032 1941 ε=100%
58Co 57.935751292 ± 0.000001237 70.844 d ± 0.020 1941 β+=100%; e+=14.79±2.4%; ε=85.21±2.4%
58Com 57.935751292 ± 0.000001237 8.853 h ± 0.023 1950 IT=99.99880±0.5%; ε=0.00120±0.5%
58Con 57.935751292 ± 0.000001237 10.5 us ± 0.3 1964 IT=100%
59Co 58.933193524 ± 0.000000426 Stable 1923 IS=100%
60Co 59.933815536 ± 0.000000433 5.2714 y ± 0.0006 1941 β-=100%
60Com 59.933815536 ± 0.000000433 10.467 m ± 0.006 1963 IT≈100%; β-=0.25±0.3%
61Co 60.932476031 ± 0.000000901 1.649 h ± 0.005 1947 β-=100%
62Co 61.934058198 ± 0.00001994 1.54 m ± 0.10 1949 β-=100%
62Com 61.934058198 ± 0.00001994 13.86 m ± 0.09 1957 β-≈100%; IT<0.5%
63Co 62.933599630 ± 0.000019941 26.9 s ± 0.4 1960 β-=100%
64Co 63.935810176 ± 0.000021476 300 ms ± 30 1969 β-=100%
64Com 63.935810176 ± 0.000021476 300 ms [Estimated] 2008 β- ?; IT ?
65Co 64.936462071 ± 0.000002235 1.16 s ± 0.03 1978 β-=100%
66Co 65.939442943 ± 0.000015 194 ms ± 17 1985 β-=100%; β-n ?
66Com 65.939442943 ± 0.000015 824 ns ± 22 1998 IT=100%
66Con 65.939442943 ± 0.000015 >100 us 1998 IT=100%
67Co 66.940609625 ± 0.000006917 329 ms ± 28 1985 β-=100%; β-n ?
67Com 66.940609625 ± 0.000006917 496 ms ± 33 2008 IT>80%; β- ?
68Co 67.944559401 ± 0.000004142 200 ms ± 20 1985 β-=100%; β-n ?
68Com 67.944559401 ± 0.000004142 1.6 s ± 0.3 1998 β-=100%; β-n>2.6%
68Con 67.944559401 ± 0.000004142 101 ns ± 10 2010 IT=100%
69Co 68.945909000 ± 0.000092 180 ms ± 20 1985 β-=100%; β-n ?
69Com 68.945909000 ± 0.000092 750 ms ± 250 2015 β-=100%
70Co 69.950053400 ± 0.0000118 508 ms ± 7 1998 β-=100%; β-n ?; β-2n ?
70Com 69.950053400 ± 0.0000118 112 ms ± 7 1985 β-=100%; IT ?; β-n ?; β-2n ?
71Co 70.952366923 ± 0.00049923 80 ms ± 3 1992 β-=100%; β-n=3±0.1%
72Co 71.956736 ± 0.000322 [Estimated] 51.5 ms ± 0.3 1992 β-=100%; β-n>4%; β-2n ?
72Com 71.956736 ± 0.000322 [Estimated] 47.8 ms ± 0.5 2016 β-=100%
73Co 72.959238 ± 0.000322 [Estimated] 42.0 ms ± 0.8 1995 β-=100%; β-n=6±0.3%; β-2n ?
74Co 73.963993 ± 0.000429 [Estimated] 31.3 ms ± 1.3 1995 β-=100%; β-n=18±1.5%; β-2n ?
75Co 74.967192 ± 0.000429 [Estimated] 26.5 ms ± 1.2 1995 β-=100%; β-n<16%; β-2n ?
76Co 75.972453 ± 0.000537 [Estimated] 23 ms ± 6 2010 β-=100%; β-n ?; β-2n ?
76Com 75.972453 ± 0.000537 [Estimated] 16 ms ± 4 2015 β-=100%
76Con 75.972453 ± 0.000537 [Estimated] 2.99 us ± 0.27 2015 IT=100%
77Co 76.976479 ± 0.000644 [Estimated] 15 ms ± 6 2014 β-=100%; β-n ?; β-2n ?; β-3n ?
78Co 77.983553 ± 0.000751 [Estimated] 11 ms >410ns [Estimated] 2017 β- ?

Information Sources

  1. 1.  PubChem
  2. 2.  Atomic Mass Data Center (AMDC), International Atomic Energy Agency (IAEA)
  3. 3.  IUPAC Commission on Isotopic Abundances and Atomic Weights (CIAAW)
  4. 4.  Jefferson Lab, U.S. Department of Energy
    LICENSE
    Please see citation and linking information https https://www.jlab.org/privacy-and-security-notice
  5. 5.  Los Alamos National Laboratory, U.S. Department of Energy
  6. 6.  NIST Physical Measurement Laboratory
  7. 7.  IUPAC Periodic Table of the Elements and Isotopes (IPTEI)
    LICENSE
    Copyright (c) 2020 International Union of Pure and Applied Chemistry. The International Union of Pure and Applied Chemistry (IUPAC) contribution within Pubchem is provided under a CC-BY-NC-ND 4.0 license, unless otherwise stated.
    https://creativecommons.org/licenses/by-nc-nd/4.0/
  8. 8.  PubChem Elements
    Cobalt

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