Niobium

Vapor pressure
41	zirconium ← niobium → molybdenum
	periodic table
General
Name, Symbol, Number	niobium, Nb, 41
Chemical series	transition metals
Group, Period, Block	5, 5, d
Appearance	gray metallic ;
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)
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

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Niobium (IPA: /niˈəʊbiəm, ˌnʌɪˈəʊbiəm/), or columbium (IPA: /kəˈlʌmbiəm/) is a chemical element in the periodic table that has the symbol Nb and atomic number 41. A rare, soft, gray, ductile transition metal, niobium is found in niobite and used in alloys. The most notable alloys are used to make special steels and strong welded joints. Niobium was discovered in a variety of columbite (now called niobite) and was at first named after this mineral.

Notable characteristics

Niobium is a shiny gray, ductile metal that takes on a bluish tinge when exposed to air at room temperature for extended periods. Niobium's chemical properties are almost identical to the chemical properties of tantalum, which appears below niobium in the periodic table.

When it is processed at even moderate temperatures niobium 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.

Applications

Niobium has a number of uses: it is a component of some stainless steels and an alloy of other nonferrous metals. These alloys are strong and are often used in pipeline construction. Other uses;

The metal has a low capture cross-section for thermal neutrons and so finds use in the nuclear industries.
It is also the metal used in arc welding rods for some stabilized grades of stainless steel.
Appreciable amounts of niobium in the form of high-purity ferroniobium and nickel niobium are used in nickel-, cobalt-, and iron-base superalloys for such applications as jet engine components, rocket subassemblies, and heat-resisting and combustion equipment. For example, advanced air frame systems such as those used in the Gemini program used this metal.
Niobium is being evaluated as an alternative to tantalum in capacitors.
Because niobium metal and some niobium alloys are physiologically inert (and thus hypoallergenic), they are used in jewelry and in medical devices. Niobium metal treated with sodium hydroxide forms a porous layer that aids osseointegration.^[1]
Along with titanium, tantalum, and aluminum, Niobium can also be electrically heated and anodized to a wide array of colors using a process known as reactive metal anodizing. This makes it very attractive for use in jewelry.
Niobium is also added to glass in order to attain a higher refractive index, a property used in the optical industry to make thinner corrective glasses.

Niobium becomes a superconductor when lowered to cryogenic temperatures. At atmospheric pressure, it has the highest critical temperature of the elemental superconductors: 9.3 K. In addition, it is one of the three elemental superconductors that are Type II (the others being vanadium and technetium), meaning it remains a superconductor when subjected to high magnetic fields. Niobium-tin and niobium-titanium alloys are used as wires for superconducting magnets capable of producing exceedingly strong magnetic fields. Niobium is also used in its pure form to make superconducting accelerating structures for particle accelerators.

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. There was a considerable amount of confusion about the difference between the closely-related niobium and tantalum that wasn't resolved until 1846 by Heinrich Rose and Jean Charles Galissard de Marignac, who rediscovered the element. Since Rose was unaware of Hatchett's work, he 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.

Columbium (symbol Cb) was the name originally given to this element by Hatchett, but 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, however, 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."

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 in Russia. A large producer in Brazil is CBMM located in Araxá, Minas Gerais.

See also niobium minerals.

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 (half life: 20300 years), and Nb-91 with a half life of 680 years. There is also a meta state at 0.031 megaelectronvolts whose half-life is 16.13 years. Twenty three other radioisotopes have been characterized. 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). The primary decay mode before the stable Nb-93 is electron capture and the primary mode after is beta emission with some neutron emission occurring in the first mode of the two mode decay of Nb-104, 109 and 110. It is worth 4 dollars a gram

Precautions

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

References
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↑ 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.

Los Alamos National Laboratory – Niobium

External links

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Niobium

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[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.

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