CAS: 7440-48-4
Description: Tough, silver-white metal
Classification: Transition Metal
Date of Discovery: 1737
Discoverer: George Brandt
Name Origin: German kobald "goblin or evil spirit"; Greek cobalos "mine"
Atomic Number: 27
Number of Neutrons: 32
Atomic Mass: 58.93320(1) amu
Melting Point: 1495 °C
Boiling Point: 2927 °C
Density (293 K): 8.9 g/cm3 Atomic volume: 6.7 cm3/mol
Electrical resistivity: 0.172 10-6/cm Thermal conductivity: 1.00 W/cmK
Enthalpy of atomization: 426.77 kJ/mol
Enthalpy of vaporization: 376.50 kJ/mol
Enthalpy of fusion: 16.190 kJ/mol
Specific heat capacity: 0.42 J/gK
Energy levels: 2-8-15-2
Electron configuration: [Ar]3d74s2 Crystal Structure: Hexagonal
Atomic radius: 1.67 Å
Covalent radius: 1.16 Å
Oxidation States: +2, +3
Electronegativity, Pauling: 1.88
Electron affinity: 0.662 eV
First ionization energy: 7.86 eV
2nd ionization energy: 17.06 eV
3rd ionization energy: 33.50 eV
Polarizability: 7.5 10-24cm3
Isotope
Natural Abundance
Atomic Mass
Half-life
Decay Mode
Spin
50Co
49.9812
+
51Co
50.9705
+
52Co
51.9632
+
53mCo
0.25 s
+, p
19/2-
53Co
52.95423
0.26 s
+
7/2-
54mCo
1.46 m
+
7+
54Co
53.948464
0.1932 s
+
0+
55Co
54.942003
17.53 h
+; EC
7/2
56Co
55.939844
77.3 d
+; EC
4+
57Co
56.936296
271.8 d
EC
7/2
58mCo
9.1 h
IT
5+
58Co
57.935757
70.88 d
+; EC
2+
59Co
100.
58.933200
Stable
7/2-
60mCo
10.47 m
IT;-
2+
60Co
59.933822
5.271 y
-
5+
61Co
60.932479
1.650 h
-
7/2-
62mCo
13.9 m
-
5+
62Co
61.93405
1.50 m
-
2+
63Co
62.93362
27.5 s
-
7/2-
64Co
63.93581
0.30 s
-
1+
65Co
64.93648
1.14 s
-
(7/2-)
66Co
65.9398
0.23 s
-
67Co
66.9406
-
68Co
67.9444
0.18 s
-
69Co
68.9452
0.27 s
-
70Co
69.9498
-
71Co
Discovered by Brandt about 1735. Cobalt occurs in the mineral cobaltite (CoAsS), smaltite [skutterudite, (Co,Ni)As3-x], erythrite [Co3(AsO4)2 · 8H2O], and linneite (Co3S4) 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 cloase to the the Hawaiian Islands and other U.S. Pacific territories. Cobalt is a brittle, hard metal, closely 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 -form predominates below 400 °C, and the -form above that temperature. The transformation is sluggish and accounts in part for the wide variation in reported data on physical properties of cobalt. 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. The salts have been used for centuries for the production of 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 (CoCl2 · 6H20) is used as a sympathetic ink. The cobalt amines are of interest; the oxide and the nitrate are important. 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. Cobalt-60, an artificial isotope, is an important gamma ray source, and is extensively used as a tracer and a radiotherapeutic agent. Twenty-six isotopes and isomers are known.
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