41
Nb
Niobium
Atomic Mass 92.90637
Electron Configuration [Kr]5s14d4
Oxidation States +5, +3
Year Discovered 1801

Identifiers

Element Name Niobium
Element Symbol Nb
InChI InChI=1S/Nb
InChIKey GUCVJGMIXFAOAE-UHFFFAOYSA-N

Properties

Atomic Weight

92.906 37(1)

92.90637

92.91

92.90637(2)

Electron Configuration

[Kr]5s14d4

Atomic Radius

Van der Waals Atomic Radius : 207 pm (Van der Waals)

Empirical Atomic Radius : 145pm (Empirical)

Covalent Atomic Radius : 164(6) pm (Covalent)

Oxidation States

+5, +3

5, 4, 3, 2, 1, -1, -3 ​(a mildly acidic oxide)

Ground Level

6D1/2

Ionization Energy

6.759 eV

6.75885 ± 0.00004 eV

Electronegativity

Pauling Scale Electronegativity : 1.6(Pauling Scale)

Allen Scale Electronegativity : 1.41(Allen Scale)

Electron Affinity

0.893eV

1.13eV

Atomic Spectra

Lines Holdings

Levels Holdings

Physical Description

Solid

Element Classification

Metal

Element Period Number

5

Element Group Number

5

Density

8.57 grams per cubic centimeter

Melting Point

2750 K (2477°C or 4491°F)

2477°C

Boiling Point

5017 K (4744°C or 8571°F)

4744°C

Estimated Crustal Abundance

2.0×101 milligrams per kilogram

Estimated Oceanic Abundance

1×10-5 milligrams per liter

History

The name derives from the Greek mythological character Niobe, who was the daughter of Tantalus, because the elements niobium and tantalum were originally thought to be identical. Niobium was discovered in a black mineral from America called columbite by the British chemist and manufacturer Charles Hatchett in 1801 and he called the element columbium. In 1809, the English chemist William Hyde Wollaston claimed that columbium and tantalum were identical.

Forty years later, the German chemist and pharmacist, Heinrich Rose, determined that they were two different elements in 1846 and gave the name niobium because it was so difficult to distinguish it from tantalum. The name columbium continued to be used in America and niobium in Europe until IUPAC adopted the name niobium in 1949. Niobium was first isolated by the chemist C. W. Blomstrand in 1846.

The story of niobium's discovery is a bit confusing. The first governor of Connecticut, John Winthrop the Younger, discovered a new mineral around 1734. He named the mineral columbite ((Fe, Mn, Mg)(Nb, Ta)2O6) and sent a sample of it to the British Museum in London, England. The columbite sat in the museum's mineral collection for years until it was analyzed by Charles Hatchett in 1801. Hatchett could tell that there was an unknown element in the columbite, but he was not able to isolate it. He named the new element columbium. The fate of columbium took a drastic turn in 1809 when William Hyde Wollaston, an English chemist and physicist, compared the minerals columbite and tantalite ((Fe, Mn)(Ta, Nb)2O6) and declared that columbium was actually the element tantalum. This confusion arose because tantalum and niobium are similar metals, are always found together and are very difficult to isolate.

Niobium was rediscovered and renamed by Heinrich Rose in 1844 when he produced two new acids, niobic acid and pelopic acid, from samples of columbite and tantalite. These acids are very similar to each other and it took another twenty-two years and a Swiss chemist named Jean Charles Galissard de Marignac to prove that these were two distinct chemicals produced from two different elements. Metallic niobium was finally isolated by the Swedish chemist Christian Wilhelm Blomstrand in 1864. Today, niobium is primarily obtained from the minerals columbite and pyrochlore ((Ca, Na)2Nb2O6(O, OH, F)).

Named after Niobe, the daughter of Tantalu. Discovered in 1801 by Hatchett in an ore sent to England. The metal was first prepared in 1864 by Blomstrand, who reduced the chloride by heating it in a hydrogen atmosphere. The name niobium was adopted by the International Union of Pure and Applied Chemicstry (IUPAC) in 1950 after 100 years of controversy. Many leading chemical societies and government organizations refer to it by this name. Most metallurgists, leading metal societies, and all but one of the leading U.S. commercial producers, however, still refer to the metal as "columbium."

Historical Atomic Weights

Year Atomic Weight (uncertainty) [u] Reference
2017 92.906 37(1) https://doi.org/10.1515/pac-2019-0603
2013 92.906 37(2) https://doi.org/10.1515/pac-2015-0305
1985 92.906 38(2) https://doi.org/10.1351/pac198658121677
1969 92.9064(1) https://doi.org/10.1351/pac197021010091
1961 92.906 https://doi.org/10.1021/ja00881a001
1935 92.91 https://doi.org/10.1039/JR9350000788
1931 93.3 https://doi.org/10.1039/JR9310001617
1917 93.1 https://doi.org/10.1021/ja02268a001
1909 93.5 https://doi.org/10.1021/ja01931a001
1902 94 https://doi.org/10.1007/BF01370337

Historical Isotopic Abundances

Year Isotope Abundance (uncertainty) Reference
1975, 93Nb, 1, doi:10.1351/pac197647010075

Description

Niobium is a shiny, white, soft, and ductile metal, and takes on a bluish cast when exposed to air at room temperatures for a long time. The metal starts to oxidize in air at 200°C, and when processed at even moderate temperatures must be placed in a protective atmosphere.

Users

Niobium is used as an alloying agent and for jewelry, but perhaps its most interesting applications are in the field of superconductivity. Superconductive wire can be made from an alloy of niobium and titanium which can then be used to make superconductive magnets. Other alloys of niobium, such as those with tin and aluminum, are superconductive as well. Pure niobium is itself a superconductor when it is cooled below 9.25 K (-442.75°F). Superconductive niobium cavities are at the heart of a machine built at the Thomas Jefferson National Accelerator Facility. This machine, called an electron accelerator, is used by scientists to study the quark structure of matter. The accelerator's 338 niobium cavities are bathed in liquid helium and accelerate electrons to nearly the speed of light.

Niobium is used in arc-welding rods for stabilized grades of stainless steel. Thousands of pounds of niobium have been used in advanced air frame systems such as were used in the Gemini space program. The element has superconductive properties; superconductive magnets have been made with Nb-Zr wire, which retains its superconductivity in strong magnetic fields. This type of application offers hope of direct large-scale generation of electric power. Niobium is also commonly used for jewelry.

Sources

The element is found in niobite (or columbite), niobite-tantalite, parochlore, and euxenite. Large deposits of niobium have been found associated with carbonatites (carbon-silicate rocks), as a constituent of parochlore. Extensive ore reserves are found in Canada, Brazil, Nigeria, Zaire, and in Russia.

Compounds

See more information at the Niobium compound page.

Element Forms

CID Name Formula SMILES Molecular Weight
23936 niobium Nb [Nb] 92.90637
104776 niobium-95 Nb [95Nb] 94.906831
177442 niobium-90 Nb [90Nb] 89.91126
115134 niobium-94 Nb [94Nb] 93.90728
167723 niobium-97 Nb [97Nb] 96.90810
177443 niobium-88 Nb [88Nb] 87.9182
177624 niobium-89 Nb [89Nb] 88.9134
177625 niobium-98 Nb [98Nb] 97.91033
177692 niobium-96 Nb [96Nb] 95.908102
42626441 niobium-93 Nb [93Nb] 92.90637
44148211 niobium-92 Nb [92Nb] 91.90719
3863468 niobium(5+) Nb+5 [Nb+5] 92.90637
10171235 niobium(3+) Nb+3 [Nb+3] 92.90637
11366952 niobium(2+) Nb+2 [Nb+2] 92.90637

Isotopes

Stable Isotope Count 1
Summary Eighteen isotopes of niobium are known. The metal can be isolated from tantalum, and prepared in several ways.

Isotopes in Biology

95Nb (with a half-life of 35 days) and 95Nb-oxalates have been used to study the absorption, retention and distribution of niobium in the body [309], [310].

[309] F. R. Mraz, G. R. Eisele. Radiat. Res.72, 533 (1977).
[310] F. Paquet, P. Houpert, M. Verry, G. Grillon, J. D. Harrison, H. Métivier. Radiat. Prot. Dosim.79, 191 (1998).

Isotopes in Earth/Planetary Science

Nuclear physicists are trying to study the generation of new isotopes and their elements in stars (astrophysical nucleosynthesis) via the rapid neutron capture process (r-process). Physicists at the Radioactive Isotope Beam Facility (RIBF) of the RIKEN Nishina Center for Accelerator-Based Science in Wako, Japan, have begun creating and studying highly neutron-rich isotopes that are thought to only be produced by the r-process. The data for many neutron-rich isotopes is incomplete, and the RIKEN team is filling in key missing information that is needed to simulate the r-process (including information on the half-lives of the neutron-rich isotopes). So far, the half-lives of 38 neutron-rich isotopes have been measured from krypton to technetium, including 111Nb and 112Nb. When the missing information has been obtained, physicists will have a better understanding of the r-process and how elements are created [311], [312].

[311] RIKEN Research. The Importance of Fundamental Measurements, RIKEN Research (2017), Feb. 26; http://www.riken.jp/en/research/rikenresearch/highlights/6600/.
[312] S. Nishimura, Z. Li, H. Watanabe, K. Yoshinaga, T. Sumikama, T. Tachibana, K. Yamaguchi, M. Kurata-Nishimura, G. Lorusso, Y. Miyashita, A. Odahara, H. Baba, J. S. Berryman, N. Blasi, A. Bracco, F. Camera, J. Chiba, P. Doornenbal, S. Go, T. Hashimoto, S. Hayakawa, C. Hinke, E. Ideguchi, T. Isobe, Y. Ito, D. G. Jenkins, Y. Kawada, N. Kobayashi, Y. Kondo, R. Krücken, S. Kubono, T. Nakano, H. J. Ong, S. Ota, Z. Podolyák, H. Sakurai, H. Scheit, K. Steiger, D. Steppenbeck, K. Sugimoto, S. Takano, A. Takashima, K. Tajiri, T. Teranishi, Y. Wakabayashi, P. M. Walker, O. Wieland, H. Yamaguchi. Phys. Rev. Lett.106, 052502 (2011).

Isotopes in Medicine

95Nb and 95mNb (with a half-life of 3.6 days) have been used in tumor research and tumor imaging studies (Fig. IUPAC.41.1) [313], [314], [315]. The m in the superscript of 95mNb indicates a metastable state of the isotope.

Fig. IUPAC.41.1: Tumor/Non-tumor ratios of ⁹⁵Nb-bevacizumab at 4, 24, 48 and 168 h post injection (modified from [315]). Bevacizumab, sold under the trade name Avastin, is a drug that slows the growth of new blood vessels and was approved by the U.S. Food and Drug Administration for selected metastatic cancers, including colon cancer. This in vivo biodistribution study (a distribution of compounds within a biological system or organism) shows increased tumor uptake of ⁹⁵Nb-bevacizumab and a satisfactory tumor/blood ratio.

[313] A. Ando, I. Ando. J. Radiat. Res.31, 97 (1990).
[314] A. Ando, I. Ando. Acta Radiol. Suppl.374, 65 (1990).
[315] V. Radchenko, P. Bouziotis, G. Loudos, S. Xanthopoulos, H. Hauser, M. Esienhut, B. Ponsard, F. Roesch. J. Labelled Comp. Radiopharm.56, S69 (2013).

Isotope Mass and Abundance

Isotope Atomic Mass (uncertainty) [u] Abundance (uncertainty)
93Nb 92.906 37(1) 1
Isotope Atomic Mass (uncertainty) [u] Abundance (uncertainty)
93Nb 92.9063730(20) 1

Atomic Mass, Half Life, and Decay

Nuclide Atomic Mass and Uncertainty [u] Half Life and Uncertainty Discovery Year Decay Modes, Intensities and Uncertainties [%]
79Nb 78.966022 ± 0.000537 [Estimated] Not-specified p ?; β+ ?; β+p ?
80Nb 79.958754 ± 0.000429 [Estimated] Not-specified p ?; β+ ?; β+p ?
81Nb 80.950230 ± 0.000429 [Estimated] Not-specified <44ns p ?; β+ ?; β+p ?
82Nb 81.944380 ± 0.000322 [Estimated] 51 ms ± 5 1992 β+=100%; β+p ?
82Nbm 81.944380 ± 0.000322 [Estimated] 93 ns ± 20 2008 IT=100%
83Nb 82.938150000 ± 0.000174 3.9 s ± 0.2 1988 β+=100%
84Nb 83.934305711 ± 0.00000043 9.8 s ± 0.9 1977 β+=100%
84Nbm 83.934305711 ± 0.00000043 176 ns ± 46 2009 IT=100%
84Nbn 83.934305711 ± 0.00000043 92 ns ± 5 2000 IT=100%
85Nb 84.928845836 ± 0.0000044 20.5 s ± 0.7 1988 β+=100%
85Nbm 84.928845836 ± 0.0000044 3.3 s ± 0.9 1988 IT=?; β+=?
85Nbn 84.928845836 ± 0.0000044 12 s ± 5 β- ?; IT ?
86Nb 85.925781536 ± 0.000005903 88 s ± 1 1974 β+=100%
86Nbm 85.925781536 ± 0.000005903 20 s [Estimated] 1994 β+=100%; IT ?
86Nbn 85.925781536 ± 0.000005903 56.3 s ± 8.3 β+= ?; IT ?
87Nb 86.920692473 ± 0.000007302 3.7 m ± 0.1 1971 β+=100%
87Nbm 86.920692473 ± 0.000007302 2.6 m ± 0.1 1972 β+=100%
88Nb 87.918226476 ± 0.000062059 14.50 m ± 0.11 1964 β+=100%
88Nbm 87.918226476 ± 0.000062059 7.7 m ± 0.1 1971 β+=100%
89Nb 88.913444696 ± 0.000025367 2.03 h ± 0.07 1954 β+=100%
89Nbm 88.913444696 ± 0.000025367 1.10 h ± 0.03 1954 β+=100%
90Nb 89.911259201 ± 0.000003561 14.60 h ± 0.05 1951 β+=100%
90Nbm 89.911259201 ± 0.000003561 63 us ± 2 1967 IT=100%
90Nbn 89.911259201 ± 0.000003561 18.81 s ± 0.06 1969 IT=100%
90Nbp 89.911259201 ± 0.000003561 <1 us 1981 IT=100%
90Nbq 89.911259201 ± 0.000003561 6.19 ms ± 0.08 1967 IT=100[gs=0,m=100]
90Nbr 89.911259201 ± 0.000003561 471 ns ± 6 1978 IT=100%
91Nb 90.906990256 ± 0.00000314 680 y ± 130 1951 ε≈100%; e+=0.0138±2.5%
91Nbm 90.906990256 ± 0.00000314 60.86 d ± 0.22 1950 IT=96.6±0.5%; ε=3.4±0.5%; e+=0.0028±0.2%
91Nbn 90.906990256 ± 0.00000314 3.76 us ± 0.12 1974 IT=100%
92Nb 91.907188580 ± 0.000001915 34.7 My ± 2.4 1938 β+=100%
92Nbm 91.907188580 ± 0.000001915 10.116 d ± 0.013 1959 β+=100%
92Nbn 91.907188580 ± 0.000001915 5.9 us ± 0.2 1958 IT=100%
92Nbp 91.907188580 ± 0.000001915 167 ns ± 4 1989 IT=100%
93Nb 92.906373170 ± 0.000001599 Stable 1932 IS=100%
93Nbm 92.906373170 ± 0.000001599 16.12 y ± 0.12 1965 IT=100%
93Nbn 92.906373170 ± 0.000001599 1.5 us ± 0.5 2007 IT=100%
94Nb 93.907279001 ± 0.0000016 20.4 ky ± 0.4 1938 β-=100%
94Nbm 93.907279001 ± 0.0000016 6.263 m ± 0.004 1962 IT=99.50±0.6%; β-=0.50±0.6%
95Nb 94.906831110 ± 0.000000545 34.991 d ± 0.006 1951 β-=100%
95Nbm 94.906831110 ± 0.000000545 3.61 d ± 0.03 1969 IT=94.4±0.6%; β-=5.6±0.6%
96Nb 95.908101586 ± 0.000000157 23.35 h ± 0.05 1949 β-=100%
97Nb 96.908101622 ± 0.000004556 72.1 m ± 0.7 1951 β-=100%
97Nbm 96.908101622 ± 0.000004556 58.7 s ± 1.8 1950 IT=100%
98Nb 97.910332645 ± 0.000005369 2.86 s ± 0.06 1960 β-=100%
98Nbm 97.910332645 ± 0.000005369 51.1 m ± 0.4 1948 β-≈100%; IT ?
99Nb 98.911609377 ± 0.000012886 15.0 s ± 0.2 1950 β-=100%
99Nbm 98.911609377 ± 0.000012886 2.5 m ± 0.2 1960 β-≈100%; IT=?
100Nb 99.914340578 ± 0.000008562 1.5 s ± 0.2 1967 β-=100%
100Nbm 99.914340578 ± 0.000008562 2.99 s ± 0.11 1967 β-=100%
100Nbn 99.914340578 ± 0.000008562 460 ns ± 60 1986 IT=100%
100Nbp 99.914340578 ± 0.000008562 12.43 us ± 0.26 1980 IT=100%
101Nb 100.915306508 ± 0.000004024 7.1 s ± 0.3 1970 β-=100%
102Nb 101.918090447 ± 0.000002695 4.3 s ± 0.4 1972 β-=100%
102Nbm 101.918090447 ± 0.000002695 1.31 s ± 0.16 1976 β-=100%; IT ?
103Nb 102.919453416 ± 0.000004224 1.34 s ± 0.07 1971 β-=100%; β-n ?
104Nb 103.922907728 ± 0.000001915 0.98 s ± 0.05 1976 β-=100%; β-n=0.05±0.3%
104Nbm 103.922907728 ± 0.000001915 4.9 s ± 0.3 1971 β-=100%; β-n=0.06±0.3%
105Nb 104.924942577 ± 0.000004324 2.91 s ± 0.05 1984 β-=100%; β-n=1.7±0.9%
106Nb 105.928928505 ± 0.00000152 900 ms ± 20 1976 β-=100%; β-n=4.5±0.3%
106Nbm 105.928928505 ± 0.00000152 1.20 s ± 0.06 1976 β-=100%; IT ?
106Nbn 105.928928505 ± 0.00000152 820 ns ± 38 1999 IT=100%
107Nb 106.931589685 ± 0.000008612 286 ms ± 8 1992 β-=100%; β-n=7.4±0.8%
108Nb 107.936075604 ± 0.000008844 201 ms ± 4 1994 β-=100%; β-n=6.3±0.5%; β-2n ?
108Nbm 107.936075604 ± 0.000008844 109 ns ± 2 2012 IT=100%
109Nb 108.939141000 ± 0.0004625 106.9 ms ± 4.9 1994 β-=100%; β-n=31±0.5%
109Nbm 108.939141000 ± 0.0004625 115 ns ± 8 2011 IT=100%
110Nb 109.943843000 ± 0.0009 75 ms ± 1 1994 β-=100%; β-n=40±0.8%; β-2n ?
110Nbm 109.943843000 ± 0.0009 94 ms ± 9 2020 β-=100%; IT ?; β-n=40±0.8%; β-2n ?
111Nb 110.947439 ± 0.000322 [Estimated] 54 ms ± 2 1997 β-=100%; β-n ?; β-2n ?
112Nb 111.952689 ± 0.000322 [Estimated] 38 ms ± 2 1997 β-=100%; β-n ?; β-2n ?
113Nb 112.956833 ± 0.000429 [Estimated] 32 ms ± 4 1997 β-=100%; β-n ?; β-2n ?
114Nb 113.962469 ± 0.000537 [Estimated] 17 ms ± 5 2010 β-=100%; β-n ?; β-2n ?
115Nb 114.966849 ± 0.000537 [Estimated] 23 ms ± 8 2010 β-=100%; β-n ?; β-2n ?
116Nb 115.972914 ± 0.000322 [Estimated] 12 ms >550ns [Estimated] 2018 β- ?; β-n ?; β-2n ?

Information Sources

  1. 1.  PubChem
  2. 2.  Atomic Mass Data Center (AMDC), International Atomic Energy Agency (IAEA)
  3. 3.  IUPAC Commission on Isotopic Abundances and Atomic Weights (CIAAW)
  4. 4.  Jefferson Lab, U.S. Department of Energy
    LICENSE
    Please see citation and linking information https https://www.jlab.org/privacy-and-security-notice
  5. 5.  Los Alamos National Laboratory, U.S. Department of Energy
  6. 6.  NIST Physical Measurement Laboratory
  7. 7.  IUPAC Periodic Table of the Elements and Isotopes (IPTEI)
    LICENSE
    Copyright (c) 2020 International Union of Pure and Applied Chemistry. The International Union of Pure and Applied Chemistry (IUPAC) contribution within Pubchem is provided under a CC-BY-NC-ND 4.0 license, unless otherwise stated.
    https://creativecommons.org/licenses/by-nc-nd/4.0/
  8. 8.  PubChem Elements
    Niobium

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