Niobium

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41 zirconiumniobiummolybdenum
V

Nb

Ta
Nb-TableImage.png
periodic table
General
Name, Symbol, Number niobium, Nb, 41
Chemical series transition metals
Group, Period, Block 5, 5, d
Appearance gray metallic
Nb,41.jpg
Atomic mass 92.90638(2) g/mol
Electron configuration [Kr] 4d4 5s1
Electrons per shell 2, 8, 18, 12, 1
Physical properties
Phase solid
Density (near r.t.) 8.57 g/cm³
Melting point 2750 K
(2477 °C, 4491 °F)
Boiling point 5017 K
(4744 °C, 8571 °F)
Heat of fusion 30 kJ/mol
Heat of vaporization 689.9 kJ/mol
Heat capacity (25 °C) 24.60 J/(mol·K)
Vapor pressure
P/Pa 1 10 100 1 k 10 k 100 k
at T/K 2942 3207 3524 3910 4393 5013
Atomic properties
Crystal structure cubic body centered
Oxidation states 5, 3
(mildly acidic oxide)
Electronegativity 1.6 (Pauling scale)
Ionization energies
(more)
1st: 652.1 kJ/mol
2nd: 1380 kJ/mol
3rd: 2416 kJ/mol
Atomic radius 145 pm
Atomic radius (calc.) 198 pm
Covalent radius 137 pm
Miscellaneous
Magnetic ordering no data
Electrical resistivity (0 °C) 152 nΩ·m
Thermal conductivity (300 K) 53.7 W/(m·K)
Thermal expansion (25 °C) 7.3 µm/(m·K)
Speed of sound (thin rod) (20 °C) 3480 m/s
Speed of sound (thin rod) (r.t.) 105 m/s
Shear modulus 38 GPa
Bulk modulus 170 GPa
Poisson ratio 0.40
Mohs hardness 6.0
Vickers hardness 1320 MPa
Brinell hardness 736 MPa
CAS registry number 7440-03-1
Notable isotopes
Main article: Isotopes of niobium
iso NA half-life DM DE (MeV) DP
91Nb syn 6.8×102 y ε - 91Zr
91mNb syn 60.86 d IT 0.104e 91Nb
92Nb syn 10.15 d ε - 92Zr
γ 0.934 -
92Nb syn 3.47×107y ε - 92Zr
γ 0.561, 0.934 -
93Nb 100% Nb is stable with 52 neutrons
93mNb syn 16.13 y IT 0.031e 93Nb
94Nb syn 2.03×104 y β- 0.471 94Mo
γ 0.702, 0.871 -
95Nb syn 34.991 d β- 0.159 95Mo
γ 0.765 -
95mNb syn 3.61 d IT 0.235 95Nb

Niobium or columbium (chemical symbol Nb, atomic number 41) is a rare, soft, gray metal. It was discovered in a variety of columbite (now called niobite) and was at first named after this mineral. It is used in alloys to make special steels and strong welded joints. At extremely low temperatures, it acts as a superconductor.

Occurrence

Niobium metal

The element is never found as a free element but does occur in the minerals columbite ((Fe,Mn)(Nb,Ta)2O6), columbite-tantalite or coltan ((Fe,Mn)(Ta,Nb)2O6), pyrochlore ((Na,Ca)2Nb2O6OH,F), and euxenite ((Y,Ca,Ce,U,Th)(Nb,Ta,Ti)2O6). Minerals that contain niobium often also contain tantalum. Large deposits of niobium have been found associated with carbonatites (carbon-silicate igneous rocks) and as a constituent of pyrochlore. Brazil and Canada are the major producers of niobium mineral concentrates and extensive ore reserves are also in Nigeria, Democratic Republic of Congo, and Russia.

History

Niobium (Greek mythology: Niobe, daughter of Tantalus) was discovered by Charles Hatchett in 1801. Hatchett found niobium in columbite ore that was sent to England in the 1750s by John Winthrop, the first governor of Connecticut. Hatchett named the element columbium (symbol Cb).

Around that time, there was considerable confusion about the difference between this element and the closely related tantalum. This confusion was not resolved until 1846 by Heinrich Rose and Jean Charles Galissard de Marignac, who rediscovered the element. Rose was unaware of Hatchett's work and gave the element a different name, niobium. In 1864, Christian Blomstrand was the first to prepare the pure metal, reducing niobium chloride by heating it in a hydrogen atmosphere.

The International Union of Pure and Applied Chemistry (IUPAC) officially adopted "niobium" as the name for element 41 in 1950, after 100 years of controversy. This was a compromise of sorts; the IUPAC accepted tungsten instead of wolfram, in deference to North American usage; and niobium instead of columbium, in deference to European usage. Not everyone agreed, and while many leading chemical societies and government organizations refer to it by the official IUPAC name, many leading metallurgists, metal societies, and most leading American commercial producers still refer to the metal by the original "columbium."

Notable characteristics

Niobium is a transition metal that lies in period 5 of the periodic table, between zirconium and molybdenum. It is also located in group 5 (former group 5B), between vanadium and tantalum. Its chemical properties are almost identical to those of tantalum.

This shiny gray, ductile metal takes on a bluish tinge when exposed to air at room temperature for extended periods. When it is processed at even moderate temperatures, it must be placed in a protective atmosphere. The metal begins to oxidize in air at 200° C. Its most common oxidation states are +3, and +5, although others are also known.

Isotopes

Naturally occurring niobium is composed of one stable isotope: Nb-93. The most stable radioisotopes are Nb-92, with a half-life of 34.7 million years; Nb-94, with a half-life of 20,300 years; and Nb-91, with a half-life of 680 years. There is also a meta state at 0.031 megaelectronvolts, with a half-life is 16.13 years. Many other radioisotopes have been characterized, with mass numbers ranging from 81 to 113. Most of these have half-lives that are less than two hours, except Nb-95 (35 days), Nb-96 (23.4 hours), and Nb-90 (14.6 hours).

Compounds

Applications

Precautions

Niobium has no known biological role. Dust of the metal is an eye and skin irritant and can also be a fire hazard. Niobium-containing compounds are relatively rarely encountered by most people, but many are highly toxic and should be handled with care.

See also

Footnotes

  1. Godley, Reut and David Starosvetsky, and Irena Gotman (2004). Bonelike apatite formation on niobium metal treated in aqueous NaOH. Journal of Materials Science: Materials in Medicine 15: 1073–1077.

References
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External links

All links retrieved November 14, 2022.

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  • Niobium  history
  • Niobium_carbide  history
  • Niobium(V)_chloride  history
  • Niobium-tin  history

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