โ–ธโ–ธ
  • ๐Ÿ‡ฌ๐Ÿ‡ง Cobalt
  • ๐Ÿ‡บ๐Ÿ‡ฆ ะšะพะฑะฐะปัŒั‚
  • ๐Ÿ‡จ๐Ÿ‡ณ ้ˆท
  • ๐Ÿ‡ณ๐Ÿ‡ฑ Kobalt
  • ๐Ÿ‡ซ๐Ÿ‡ท Cobalt
  • ๐Ÿ‡ฉ๐Ÿ‡ช Cobalt
  • ๐Ÿ‡ฎ๐Ÿ‡ฑ ืงื•ื‘ืœื˜
  • ๐Ÿ‡ฎ๐Ÿ‡น Cobalto
  • ๐Ÿ‡ฏ๐Ÿ‡ต ใ‚ณใƒใƒซใƒˆ
  • ๐Ÿ‡ต๐Ÿ‡น Cobalto
  • ๐Ÿ‡ช๐Ÿ‡ธ Cobalto
  • ๐Ÿ‡ธ๐Ÿ‡ช Kobolt
  • ๐Ÿ‡ท๐Ÿ‡บ ะšะพะฑะฐะปัŒั‚

Cobalt atoms have 27 electrons and the shell structure is 2.8.15.2. The ground state electronic configuration of neutral cobalt is [Ar].3d7.4s2 and the term symbol of cobalt is 4F9/2.

Cobalt: description  

Cobalt is a brittle, hard, silver-grey transition metal with magnetic properties similar to those of iron (ferromagnetic). Cobalt is present in meteorites. Ore deposits are found in Zaire, Morocco and Canada. The isotope cobalt-60 (60Co) is an artificially produced isotope used as a source of γ rays (its high energy radiation is useful for sterilisation in medicine and of foods). Cobalt salts colour glass a beautiful deep blue colour. Cobalt compounds are important catalysts in a number of industrial processes. Cobalt is required in small amounts for life and is the only metal found in vitamins (cobalt is the critical component of vitamin B12.

Marmite, which we eat here in England and love it or hate it is a source of vitamin B12, actually a cobalt complex. The equivalent, but blander, in Australia is Vegemite. Marmite is available in the USA. Try mixing it with peanut butter.

Cobalt: physical properties

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Cobalt: heat properties

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Cobalt: electronegativities

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Cobalt: orbital properties

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Cobalt: abundances

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Cobalt: crystal structure

Co crystal structure
The solid state structure of cobalt is: hcp (hexagonal close-packed).

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Cobalt: biological data

Cobalt salts in small amounts are essential to many life forms, including humans. It is at the core of a vitamin called vitamin-B12. Grazing animals do not to do well in areas where there is little cobalt in the soil.

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Cobalt: uses

Uses...

Cobalt: reactions

Reactions of cobalt as the element with air, water, halogens, acids, and bases where known.

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Cobalt: binary compounds

Binary compounds with halogens (known as halides), oxygen (known as oxides), hydrogen (known as hydrides), and other compounds of cobalt where known.

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Cobalt: compound properties

Bond strengths; lattice energies of cobalt halides, hydrides, oxides (where known); and reduction potentials where known.

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Cobalt: history

Cobalt was discovered by Georg Brandt in 1735 at Sweden. Origin of name: from the German word "kobald" meaning "goblin" or evil spirit.

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Cobalt: isotopes

Isotope abundances of cobalt
Isotope abundances of cobalt with the most intense signal set to 100%.

Naturally occurring cobalt consists of a single stable isotope: 59Co. Cobalt-59 has spin 7/2. The usual NMR reference is K3[Co(CN)6] in D2O. Cobalt-60 is an artifical isotope, and is an important γ-ray source.

More isotope and NMR data...

Cobalt: isolation

Isolation: it is not normally necessary to make cobalt in the laboratory as it is available readily commercially. Many ores contain cobalt but not many are of economic importance. These include the sulphides and arsenides linnaeite, Co3S4, cobaltite, CoAsS, and smaltite, CoAs2. Industrially, however, it is normally produced as a byproduct from the produstion of copper, nickel, and lead.

Normally the ore is "roasted" to form a mixture of metals and metal oxides. Treatment with sulphuric acid leaves metallic copper as a residue and disolves out iron, cobalt, and nickel as the sulphates. Iron is obtained by precipitation with lime (CaO) while cobalt is produced as the hydroxide by precipitation with sodium hypochlorite (NaOCl)

2Co2+(aq) + NaOCl(aq) + 4OH-(aq) + H2O → 2Co(OH)3(s) + NaCl(aq)

The trihydroxide Co(OH)3 is heated to form the oxide and then reduced with carbon (as charcoal) to form cobalt metal.

2Co(OH)3 (heat) → Co2O3 + 3H2O

2Co2O3 + 3C → Co + 3CO2