Properties | More Info | Isotopes | Spectra
Compounds | Reactions | Production
Atomic: M.A.C. | Reference
Diagrams: Shell | Atomic Radius | Electron || Images
Cobalt [Co] locate me
CAS-ID: 7440-48-4
An: 27 N: 32
Am: 58.933195 g/mol
Group No: 9
Group Name: Transition metals
Period: 4
State: solid at 298 K
Colour: lustrous, metallic, greyish tinge Classification: Metallic
Boiling Point: 3200K (2927°C)
Melting Point: 1768K (1495°C)
Density: 8.90g/cm3
Discovery Information
Who: George Brandt
When: 1737
Where: Sweden
Name Origin
German: kobalt or kobold (evil spirit); Greek: cobalos (mines).
 "Cobalt" in different languages.
Sources
Occurs in compounds with arsenic, oxygen and sulfur as in cobaltine (CoAsS) and linneite (Co3S4). Primary production occurs in Zaire, Morocco, Sweden and Canada. Annual production is around 17 thousand tons.
Abundance
 Universe: 3 ppm (by weight)
 Sun: 4 ppm (by weight)
 Carbonaceous meteorite: 600 ppm
 Earth's Crust: 20 ppm
 Seawater:
   Atlantic surface: n/a ppm
   Atlantic deep: n/a ppm
   Pacific surface: 6.9 x 10-6 ppm
   Pacific deep: 1.1 x 10-6 ppm
 Human:
   20 ppb by weight
   2 ppb by atoms
Uses
Used in many hard alloys; for magnets, ceramics and special glasses. Also used in permanent magnets, razor blades and catalitic converters.
Cobalt compounds have been used for centuries to impart a rich blue colour to glass, glazes, and ceramics. Cobalt has been detected in Egyptian sculpture and Persian jewellery from the third millennium BC, in the ruins of Pompeii (destroyed AD 79), and in China dating from the Tang dynasty (AD 618-907) and the Ming dynasty (AD 1368-1644).
Cobalt-60 is used in cancer therapy, food sterilization and industrial radiography (to detect structural flaws in metal parts).
History
Cobalt compounds have been used for centuries to impart a rich blue colour to glass, glazes, and ceramics. Cobalt has been detected in Egyptian sculpture and Persian jewelry from the third millennium BC, in the ruins of Pompeii (destroyed AD 79), and in China dating from the Tang dynasty (AD 618-907) and the Ming dynasty (AD 1368-1644).
Swedish chemist Georg Brandt (1694-1768) is credited with isolating cobalt sometime between 1730 and 1737. He was able to show that cobalt was the source of the blue colour in glass, which previously had been attributed to the bismuth found with cobalt.
During the 19th century, cobalt blue was produced at the Norwegian Blaafarvevaerket (70-80% of world production), led by the Prussian industrialist Benjamin Wegner. In 1938, John Livingood and Glenn Seaborg discovered cobalt-60.
The word cobalt is derived from the German kobalt, from kobold meaning "goblin", a term used for the ore of cobalt by miners. The first attempts at smelting the cobalt ores to produce cobalt metal failed, yielding cobalt(II) oxide instead; not only that, but because of cobalt's curious affinity for arsenic, the primary ores of cobalt always contain arsenic, and upon smelting the arsenic oxidized into the highly toxic As4O6, which was breathed in by workers.
Notes
Cobalt in small amounts is essential to many living organisms, including humans. Having 0.13 to 0.30 mg/kg of cobalt in soils markedly improves the health of grazing animals. Cobalt is a central component of the vitamin cobalamin, or vitamin B-12.
Hazards
Cobalt is recognised by NIOSH as a neurotoxic agent.
Powdered cobalt in metal form is a fire hazard. Cobalt compounds should be handled with care due to cobalt's slight toxicity. 60Co is a powerful gamma ray emitter and exposure to it is therefore a cancer risk.