74
W
Tungsten
Atomic Mass 183.84
Electron Configuration [Xe]6s24f145d4
Oxidation States +6
Year Discovered 1783

Identifiers

Element Name Tungsten
Element Symbol W
InChI InChI=1S/W
InChIKey WFKWXMTUELFFGS-UHFFFAOYSA-N

Properties

Atomic Weight

183.84(1)

183.84

183.9

183.84(1)

Electron Configuration

[Xe]6s24f145d4

Atomic Radius

Van der Waals Atomic Radius : 210 pm (Van der Waals)

Empirical Atomic Radius : 135pm (Empirical)

Covalent Atomic Radius : 162(7) pm (Covalent)

Oxidation States

+6

6, 5, 4, 3, 2, 1, 0, -1, -2, -4 ​(a mildly acidic oxide)

Ground Level

5D0

Ionization Energy

7.98 eV

7.86403 ± 0.00010 eV

Electronegativity

Pauling Scale Electronegativity : 2.36(Pauling Scale)

Allen Scale Electronegativity : 1.47(Allen Scale)

Electron Affinity

0.815eV

1.23eV

Atomic Spectra

Lines Holdings

Levels Holdings

Physical Description

Solid

Element Classification

Metal

Element Period Number

6

Element Group Number

6

Density

19.3 grams per cubic centimeter

Melting Point

3695 K (3422°C or 6192°F)

3422°C

Boiling Point

5828 K (5555°C or 10031°F)

5930°C

Estimated Crustal Abundance

1.25 milligrams per kilogram

Estimated Oceanic Abundance

1×10-4 milligrams per liter

History

The name derives from the Swedish tungsten for "heavy stone". The symbol W derives from the German wolfram, which was found with tin and interfered with the smelting of tin. It was said to eat up tin like a wolf eats up sheep. The element was discovered by the Swedish pharmacist and chemist Carl-Wilhelm Scheele in 1781. Tungsten metal was first isolated by the Spanish chemists Fausto Elhuyar and his brother Juan José in 1783.

Tungsten was discovered by Juan José and Fausto Elhuyar, Spanish chemists and brothers, in 1783 in samples of the mineral wolframite ((Fe, Mn)WO4). Today, tungsten is primarily obtained from wolframite and scheelite (CaWO4) using the same basic method developed by José and Elhuyar. Tungsten ores are crushed, cleaned and treated with alkalis to form tungsten trioxide (WO3). Tungsten trioxide is then heated with carbon or hydrogen gas (H2), forming tungsten metal and carbon dioxide (CO2) or tungsten metal and water vapor (H2O).

From Swedish, tung sten meanig heavy stone. In 1779 Peter Woulfe examined the mineral now known as wolframite and concluded it must contain a new substance. Scheele, in 1781, found that a new acid could be made from tungsten (a name first applied about 1758 to a mineral now known as scheelite). Scheele and Berman suggested the possibility of obtaining a new metal by reducing this acid. The de Elhuyar brothers found acid in wolframite in 1783 that was identical to the acid of tungsten (tungstic acid) of Scheele, and in that year they succeeded in obtaining the element by reduction of this acid with charcoal. Tungsten occurs in wolframite, scheelite, huebnertie, and ferberite. Important deposits of tungsten occur in California, Colorado, South Korea, Bolivia, Russia, and Portugal. China is reported to have about 75% of the world's tungsten resources. Natural tungsten contains five stable isotopes. Twenty one other unstable isotopes are recognized. The metal is obtained commercially be reducing tungsten oxide with hydrogen or carbon.

Historical Atomic Weights

Year Atomic Weight (uncertainty) [u] Reference
1991 183.84(1) https://doi.org/10.1351/pac199264101519
1969 183.85(3) https://doi.org/10.1351/pac197021010091
1961 183.85 https://doi.org/10.1021/ja00881a001
1955 183.86 https://doi.org/10.1021/ja01595a001
1938 183.92 https://doi.org/10.1039/JR9380001101
1902 184.0 https://doi.org/10.1007/BF01370337

Historical Isotopic Abundances

Year Isotope Abundance (uncertainty) Reference
1997 180W 0.0012(1) https://doi.org/10.1351/pac199870010217
1997 182W 0.2650(16) https://doi.org/10.1351/pac199870010217
1997 183W 0.1431(4) https://doi.org/10.1351/pac199870010217
1997 184W 0.3064(2) https://doi.org/10.1351/pac199870010217
1997 186W 0.2843(19) https://doi.org/10.1351/pac199870010217
1989 180W 0.0013(4) https://doi.org/10.1351/pac199163070991
1989 182W 0.263(2) https://doi.org/10.1351/pac199163070991
1989 183W 0.143(1) https://doi.org/10.1351/pac199163070991
1989 184W 0.3067(15) https://doi.org/10.1351/pac199163070991
1989 186W 0.286(2) https://doi.org/10.1351/pac199163070991
1979 180W 0.0010(3) https://doi.org/10.1351/pac198052102349
1979 182W 0.263(2) https://doi.org/10.1351/pac198052102349
1979 183W 0.143(1) https://doi.org/10.1351/pac198052102349
1979 184W 0.307(2) https://doi.org/10.1351/pac198052102349
1979 186W 0.286(2) https://doi.org/10.1351/pac198052102349
1975 180W 0.001 https://doi.org/10.1351/pac197647010075
1975 182W 0.263 https://doi.org/10.1351/pac197647010075
1975 183W 0.143 https://doi.org/10.1351/pac197647010075
1975 184W 0.307 https://doi.org/10.1351/pac197647010075
1975 186W 0.286 https://doi.org/10.1351/pac197647010075

Description

Pure tungsten is a steel-gray to tin-white metal. Very pure tungsten can be cut with a hacksaw, forged, spun, drawn, and extruded. The impure metal is brittle and can be worked only with difficulty. Tungsten has the highest melting point of all metals, and at temperatures over 1650°C has the highest tensile strength. The metal oxidizes in air and must be protected at elevated temperatures. It has excellent corrosion resistance and is attacked only slightly by most mineral acids. The thermal expansion is about the same as borosilicate glass, which makes the metal useful for glass-to-metal seals.

Users

Pure tungsten is a light gray or whitish metal that is soft enough to be cut with a hacksaw and ductile enough to be drawn into wire or extruded into various shapes. If contaminated with other materials, tungsten becomes brittle and difficult to work with. Tungsten has the highest melting point of all metallic elements and is used to make filaments for incandescent light bulbs, fluorescent light bulbs and television tubes. Tungsten expands at nearly the same rate as borosilicate glass and is used to make metal to glass seals. Tungsten is also used as a target for X-ray production, as heating elements in electric furnaces and for parts of spacecraft and missiles which must withstand high temperatures.

Tungsten is alloyed with steel to form tough metals that are stable at high temperatures. Tungsten-steel alloys are used to make such things as high speed cutting tools and rocket engine nozzles.

Tungsten carbide (WC) is an extremely hard tungsten compound. It is used in the tips of drill bits, high speed cutting tools and in mining machinery. Tungsten disulfide (WS2) is a dry lubricant that can be used to temperatures as high as 500°C. Tungsten forms compounds with calcium and magnesium that have phosphorescent properties and are used in fluorescent light bulbs.

Tungsten and its alloys are used extensively for filaments for electric lamps, electron and television tubes, and for metal evaporation work; for electrical contact points for automobile distributors; X-ray targets; windings and heating elements for electrical furnaces; and for numerous spacecraft and high-temperature applications. High-speed tool steels, Hastelloy(R), Stellite(R), and many other alloys contain tungsten. Tungsten carbide is of great importance to the metal-working, mining, and petroleum industries. Calcium and magnesium tungstates are widely used in fluorescent lighting; other salts of tungsten are used in the chemical and tanning industries. Tungsten disulfide is a dry, high-temperature lubricant, stable to 500C. Tungsten bronzes and other tungsten compounds are used in paints.

Compounds

See more information at the Tungsten compound page.

Element Forms

CID Name Formula SMILES Molecular Weight
23964 tungsten W [W] 183.84
161097 tungsten-185 W [185W] 184.953421
161143 tungsten-181 W [181W] 180.94822
168174 tungsten-188 W [188W] 187.95849
177549 tungsten-178 W [178W] 177.9459
25087157 tungsten-180 W [180W] 179.94671
25087158 tungsten-182 W [182W] 181.948206
25087159 tungsten-183 W [183W] 182.950224
114937 tungsten-187 W [187W] 186.95716
177450 tungsten-179 W [179W] 178.9471
177661 tungsten-176 W [176W] 175.9456
177662 tungsten-177 W [177W] 176.9466
12598109 tungsten-186 W [186W] 185.95437
25087160 tungsten-184 W [184W] 183.950933
20070202 tungsten(2+) W+2 [W+2] 183.84

Isotopes

Stable Isotope Count 2

Isotopes in Earth/Planetary Science

182W is the stable product of the decay of 182Hf, which has a half-life of 8.9×106 years. Although 182Hf was present at the dawn of the Solar System, this isotope has long since decayed. During the formation of the planets, including Earth, the elements hafnium and tungsten were partitioned into silicate minerals (rock forming minerals with silicon-oxygen bonds that constitute more than 90 percent of the Earth’s crust) and metal phases, respectively. The measurement of excessive amounts of 182W, arising from the decay of 182Hf that accumulated in silicate minerals, has been used to estimate the time that elapsed between the formation of the Solar System and accretion of the planets (Fig. IUPAC.74.1) [512], [513].

Fig. IUPAC.74.1: Core formation scenarios. ¹⁸²Hf is produced during the end stages of a supernova explosion and decays to ¹⁸²W. The Early Core Scenario shows that when a core forms relatively early after a supernova explosion, a small amount of ¹⁸²Hf will be present in the mantle that will produce a significant amount of ¹⁸²W. The Late Core Scenario shows that ¹⁸²Hf was produced and decays to ¹⁸²W prior to the formation of the metallic core. Once the metallic core begins to form, it will attract tungsten because it is strongly attracted to metals. Almost all of the ¹⁸²W is partitioned into the metallic core and only a small amount will be left in the mantle. (Diagram Source: Steven Earle, Vancouver Island University) [514].

[512] E. B. Norman, D. N. Schramm. Nature304, 515 (1983).
[513] C. Vockenhuber, F. Oberli, M. Bichler, I. Ahmad, G. Quitté, M. Meier, A. N. Halliday, D. C. Lee, W. Kutschera, P. Steier, R. J. Gehrke, R. G. Helmer. Phys. Rev. Lett.93, 172501-1 (2004).
[514] S. Earle. Little Time Lost in Formation of the Planets, Vancouver Island University (2014), Feb. 26; http://records.viu.ca/∼earles/early-core-aug02.htm.

Isotopes Used as a Source of Radioactive Isotope(s)

Tungsten-rhenium generators use 188W, which is produced from 186W, via the following double neutron capture reaction 186W (n, γ) 187W (n, γ) 188W.

Isotope Mass and Abundance

Isotope Atomic Mass (uncertainty) [u] Abundance (uncertainty)
180W 179.946 71(1) 0.0012(1)
182W 181.948 206(5) 0.2650(16)
183W 182.950 224(5) 0.1431(4)
184W 183.950 933(5) 0.3064(2)
186W 185.954 365(8) 0.2843(19)
Isotope Atomic Mass (uncertainty) [u] Abundance (uncertainty)
180W 179.9467108(20) 0.0012(1)
182W 181.94820394(91) 0.2650(16)
183W 182.95022275(90) 0.1431(4)
184W 183.95093092(94) 0.3064(2)
186W 185.9543628(17) 0.2843(19)

Atomic Mass, Half Life, and Decay

Nuclide Atomic Mass and Uncertainty [u] Half Life and Uncertainty Discovery Year Decay Modes, Intensities and Uncertainties [%]
157W 156.978862 ± 0.000429 [Estimated] 275 ms ± 40 2010 β+=100%; α=0%
157Wp 156.978862 ± 0.000429 [Estimated] Not-specified 2010 IT ?
158W 157.974565 ± 0.000322 [Estimated] 1.43 ms ± 0.18 1981 α=100%
158Wm 157.974565 ± 0.000322 [Estimated] 143 us ± 19 1995 α=100%; IT ?
159W 158.972696 ± 0.000322 [Estimated] 8.2 ms ± 0.7 1981 α≈100%; β+ ?
160W 159.968513946 ± 0.000160828 90 ms ± 5 1979 α=87±0.8%; β+ ?
161W 160.967249 ± 0.000215 [Estimated] 409 ms ± 16 1973 α=73±0.3%; β+=27±0.3%
162W 161.963500341 ± 0.000018955 1.19 s ± 0.12 1973 β+ ?; α=45.2±1.6%
163W 162.962524251 ± 0.000062722 2.63 s ± 0.09 1973 β+ ?; α=14±0.2%
163Wm 162.962524251 ± 0.000062722 154 ns ± 3 2010 IT=100%
164W 163.958952445 ± 0.000010384 6.3 s ± 0.2 1973 β+=96.2±1.2%; α=3.8±1.2%
165W 164.958280663 ± 0.000027649 5.1 s ± 0.5 1975 β+=100%; α ?
166W 165.955031952 ± 0.000010159 19.2 s ± 0.6 1975 β+=99.965±1.2%; α=0.035±1.2%
167W 166.954811080 ± 0.000020078 19.9 s ± 0.5 1985 β+=99.96±0.1%; α=0.04±0.1%
167Wm 166.954811080 ± 0.000020078 >1 us [Estimated] IT ?; β+ ?
168W 167.951805459 ± 0.000014233 50.9 s ± 1.9 1971 β+≈100%; α=0.0032±1%
169W 168.951778689 ± 0.000016571 74 s ± 6 1985 β+=100%
170W 169.949231235 ± 0.000014165 2.42 m ± 0.04 1971 β+=100%
171W 170.949451000 ± 0.00003 2.38 m ± 0.04 1983 β+=100%
172W 171.947292000 ± 0.00003 6.6 m ± 0.9 1964 β+=100%
173W 172.947689000 ± 0.00003 7.6 m ± 0.2 1963 β+=100%
174W 173.946079000 ± 0.00003 33.2 m ± 2.1 1964 β+=100%
174Wm 173.946079000 ± 0.00003 >187 ns 1976 IT=100%
174Wn 173.946079000 ± 0.00003 187 ns ± 25 1976 IT=100%
174Wp 173.946079000 ± 0.00003 158 ns ± 3 2006 IT=100%
174Wq 173.946079000 ± 0.00003 128 ns ± 8 2006 IT=100%
175W 174.946717000 ± 0.00003 35.2 m ± 0.6 1963 β+=100%
175Wm 174.946717000 ± 0.00003 216 ns ± 6 1978 IT=100%
176W 175.945634000 ± 0.00003 2.5 h ± 0.1 1950 ε=100%
177W 176.946643000 ± 0.00003 132.4 m ± 2.0 1950 β+=100%
178W 177.945885791 ± 0.000016316 21.6 d ± 0.3 1950 ε=100%
178Wm 177.945885791 ± 0.000016316 220 ns ± 10 1998 IT=100%
179W 178.947079378 ± 0.000015644 37.05 m ± 0.16 1950 β+=100%
179Wm 178.947079378 ± 0.000015644 6.40 m ± 0.07 1950 IT≈100%; β+=0.29±0.4%
179Wn 178.947079378 ± 0.000015644 390 ns ± 30 1978 IT=100%
179Wp 178.947079378 ± 0.000015644 750 ns ± 80 1978 IT=100%
180W 179.946713304 ± 0.000001545 1.59 Ey ± 0.5 1937 IS=0.12±0.1%; α≈100%; 2β+ ?
180Wm 179.946713304 ± 0.000001545 5.47 ms ± 0.09 1978 IT=100%
180Wn 179.946713304 ± 0.000001545 2.33 us ± 0.19 1966 IT=100%
181W 180.948218733 ± 0.000001554 120.956 d ± 0.019 1947 ε=100%
181Wm 180.948218733 ± 0.000001554 14.59 us ± 0.15 1968 IT=100%
181Wn 180.948218733 ± 0.000001554 200 ns ± 13 1973 IT=100%
182W 181.948205636 ± 0.000000799 Stable >7.7Zy 1930 IS=26.50±1.6%; α ?
182Wm 181.948205636 ± 0.000000799 1.3 us ± 0.1 1969 IT=100%
183W 182.950224416 ± 0.000000798 Stable >670Ey 1930 IS=14.31±0.4%; α ?
183Wm 182.950224416 ± 0.000000798 5.30 s ± 0.08 1961 IT=100%
184W 183.950933180 ± 0.000000792 Stable >8.9Zy 1930 IS=30.64±0.2%; α ?
184Wm 183.950933180 ± 0.000000792 8.33 us ± 0.18 1969 IT=100%
184Wn 183.950933180 ± 0.000000792 188 ns ± 38 2004 IT=100%
185W 184.953421206 ± 0.000000793 75.1 d ± 0.3 1940 β-=100%
185Wm 184.953421206 ± 0.000000793 1.597 m ± 0.004 1950 IT=100%
186W 185.954365140 ± 0.000001302 Stable >4.1Ey 1930 IS=28.43±1.9%; 2β- ?; α ?
186Wm 185.954365140 ± 0.000001302 18 us ± 1 1998 IT=100%
186Wn 185.954365140 ± 0.000001302 2.0 s ± 0.2 1998 IT=100%
187W 186.957161249 ± 0.000001302 23.809 h ± 0.025 1940 β-=100%
187Wm 186.957161249 ± 0.000001302 1.38 us ± 0.07 2008 IT=100%
188W 187.958488325 ± 0.000003316 69.77 d ± 0.05 1951 β-=100%
188Wm 187.958488325 ± 0.000003316 109.5 ns ± 3.5 2010 IT=100%
189W 188.961557 ± 0.000215 [Estimated] 11.6 m ± 0.2 1963 β-=100%
190W 189.963103542 ± 0.000037993 30.0 m ± 1.5 1976 β-=100%
190Wm 189.963103542 ± 0.000037993 111 ns ± 17 2010 IT=100%
190Wn 189.963103542 ± 0.000037993 166 us ± 6 2000 IT=100%
191W 190.966531000 ± 0.000045 14 s >300ns [Estimated] 1999 β- ?
191Wm 190.966531000 ± 0.000045 340 ns ± 14 2009 IT=100%
192W 191.968202 ± 0.000215 [Estimated] 40 s >300ns [Estimated] 1999 β- ?
193W 192.971884 ± 0.000215 [Estimated] 30 s >300ns [Estimated] 2009 β- ?
194W 193.973795 ± 0.000322 [Estimated] 20 s >300ns [Estimated] 2008 β- ?
195W 194.977735 ± 0.000322 [Estimated] 30 s >160ns [Estimated] 2012 β- ?
196W 195.979882 ± 0.000429 [Estimated] 25 s >300ns [Estimated] 2012 β- ?
197W 196.984036 ± 0.000429 [Estimated] 1 s >300ns [Estimated] 2012 β- ?

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
    Tungsten

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