78
Pt
Platinum
Atomic Mass 195.084
Electron Configuration [Xe]6s14f145d9
Oxidation States +4, +2
Year Discovered 1735

Identifiers

Element Name Platinum
Element Symbol Pt
InChI InChI=1S/Pt
InChIKey BASFCYQUMIYNBI-UHFFFAOYSA-N

Properties

Atomic Weight

195.084(9)

195.084

195.1

195.084(9)

Electron Configuration

[Xe]6s14f145d9

Atomic Radius

Van der Waals Atomic Radius : 209 pm (Van der Waals)

Empirical Atomic Radius : 135pm (Empirical)

Covalent Atomic Radius : 136(5) pm (Covalent)

Oxidation States

+4, +2

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

Ground Level

3D3

Ionization Energy

9 eV

8.95883 ± 0.00010 eV

Electronegativity

Pauling Scale Electronegativity : 2.28(Pauling Scale)

Allen Scale Electronegativity : 1.72(Allen Scale)

Electron Affinity

2.128eV

2.56eV

Atomic Spectra

Lines Holdings

Levels Holdings

Physical Description

Solid

Element Classification

Metal

Element Period Number

6

Element Group Number

10

Density

21.46 grams per cubic centimeter

Melting Point

2041.55 K (1768.4°C or 3215.1°F)

1768.3°C

Boiling Point

4098 K (3825°C or 6917°F)

3825°C

Estimated Crustal Abundance

5×10-3 milligrams per kilogram

Estimated Oceanic Abundance

Not Applicable

History

The name derives from the Spanish platina for "silver". In 1735, the Spanish astronomer Antonio de Ulloa found platinum in Peru, South America. In 1741, the English metallurgist Charles Wood found platinum from Colombia, South America. In 1750, the English physician William Brownrigg prepared purified platinum metal.

Used by the pre-Columbian Indians of South America, platinum wasn't noticed by western scientists until 1735. Platinum can occur free in nature and is sometimes found in deposits of gold-bearing sands, primarily those found in the Ural mountains, Columbia and the western United States. Platinum, in the form of the mineral sperrylite (PtAs2), is also obtained as a byproduct of the nickel mining operation in the Sudbury region of Ontario, Canada. Credit for the modern rediscovery of platinum is usually given to Antonio de Ulloa.

Discovered in South America by Ulloa in 1735 and by Wood in 1741. The metal was used by pre-Columbian Indians.

Historical Atomic Weights

Year Atomic Weight (uncertainty) [u] Reference
2005 195.084(9) https://doi.org/10.1351/pac200678112051
1995 195.078(2) https://doi.org/10.1351/pac199668122339
1979 195.08(3) https://doi.org/10.1351/pac198052102349
1969 195.09(3) https://doi.org/10.1351/pac197021010091
1955 195.09 https://doi.org/10.1021/ja01595a001
1925 195.23 https://doi.org/10.1039/CT9252700913
1911 195.2 https://doi.org/10.1021/ja01928a001
1909 195.0 https://doi.org/10.1021/ja01931a001
1902 194.8 https://doi.org/10.1007/BF01370337

Historical Isotopic Abundances

Year Isotope Abundance (uncertainty) Reference
2013 190Pt 0.000 12(2) https://doi.org/10.1515/pac-2015-0503
2013 192Pt 0.007 82(24) https://doi.org/10.1515/pac-2015-0503
2013 194Pt 0.328 64(410) https://doi.org/10.1515/pac-2015-0503
2013 195Pt 0.337 75(240) https://doi.org/10.1515/pac-2015-0503
2013 196Pt 0.252 11(340) https://doi.org/10.1515/pac-2015-0503
2013 198Pt 0.073 56(130) https://doi.org/10.1515/pac-2015-0503
2009 190Pt 0.000 12(2) https://doi.org/10.1351/PAC-REP-10-06-02
2009 192Pt 0.007 82(24) https://doi.org/10.1351/PAC-REP-10-06-02
2009 194Pt 0.3286(40) https://doi.org/10.1351/PAC-REP-10-06-02
2009 195Pt 0.3378(24) https://doi.org/10.1351/PAC-REP-10-06-02
2009 196Pt 0.2521(34) https://doi.org/10.1351/PAC-REP-10-06-02
2009 198Pt 0.073 56(130) https://doi.org/10.1351/PAC-REP-10-06-02
1997 190Pt 0.000 14(1) https://doi.org/10.1351/pac199870010217
1997 192Pt 0.007 82(7) https://doi.org/10.1351/pac199870010217
1997 194Pt 0.329 67(99) https://doi.org/10.1351/pac199870010217
1997 195Pt 0.338 32(10) https://doi.org/10.1351/pac199870010217
1997 196Pt 0.252 42(41) https://doi.org/10.1351/pac199870010217
1997 198Pt 0.071 63(55) https://doi.org/10.1351/pac199870010217
1989 190Pt 0.0001(1) https://doi.org/10.1351/pac199163070991
1989 192Pt 0.0079(6) https://doi.org/10.1351/pac199163070991
1989 194Pt 0.329(6) https://doi.org/10.1351/pac199163070991
1989 195Pt 0.338(6) https://doi.org/10.1351/pac199163070991
1989 196Pt 0.253(6) https://doi.org/10.1351/pac199163070991
1989 198Pt 0.072(2) https://doi.org/10.1351/pac199163070991
1979 190Pt 0.000 10(3) https://doi.org/10.1351/pac198052102349
1979 192Pt 0.0079(5) https://doi.org/10.1351/pac198052102349
1979 194Pt 0.329(5) https://doi.org/10.1351/pac198052102349
1979 195Pt 0.338(5) https://doi.org/10.1351/pac198052102349
1979 196Pt 0.253(5) https://doi.org/10.1351/pac198052102349
1979 198Pt 0.072(2) https://doi.org/10.1351/pac198052102349
1975 190Pt 0.0001 https://doi.org/10.1351/pac197647010075
1975 192Pt 0.0079 https://doi.org/10.1351/pac197647010075
1975 194Pt 0.329 https://doi.org/10.1351/pac197647010075
1975 195Pt 0.338 https://doi.org/10.1351/pac197647010075
1975 196Pt 0.253 https://doi.org/10.1351/pac197647010075
1975 198Pt 0.072 https://doi.org/10.1351/pac197647010075

Description

Platinum is a beautiful silvery-white metal, when pure, and is malleable and ductile. It has a coefficient of expansion almost equal to that of soda-lime-silica glass, and is therefore used to make sealed electrodes in glass systems. The metal does not oxidize in air at any temperature, but is corroded by halogens, cyanides, sulfur, and caustic alkalis.

It is insoluble in hydrochloric and nitric acid, but dissolves when they are mixed as aqua regia, forming chloroplatinic acid.

Users

Platinum is a soft, dense, ductile metal that is very resistant to corrosion. It is used to make jewelry, wire, electrical contacts and laboratory vessels. Platinum expands at nearly the same rate as soda-lime-silica glass, so it is used to make sealed electrodes in glass systems. Platinum is used to coat missile nose cones, jet engine fuel nozzles and other devices that must operate reliably for long periods of time at high temperatures. Platinum resistance wires are used in high temperature electric furnaces. Platinum anodes are used in cathodic protection systems to prevent ships, pipelines and steel piers from corroding in salt water.

Platinum is widely used as a catalyst. It will convert methyl alcohol vapors (CH4O) into formaldehyde (CH2O) on contact, glowing red hot in the process. This effect is used to make small hand warmers. Platinum is also used in a device called a catalytic converter, a device found in the exhaust systems of most cars. Catalytic converters combine carbon monoxide (CO) and unburned fuel from a car's exhaust with oxygen from the air, forming carbon dioxide (CO2) and water vapor (H2O). Platinum is also used as a catalyst in the production of sulfuric acid (H2SO4) and in the cracking of petroleum products. Fuel cells, devices that combine hydrogen and oxygen to produce electricity and water, also use platinum as a catalyst.

The metal is extensively used in jewelry, wire, and vessels for laboratory use, and in many valuable instruments including therocouple elements. It is also used for electrical contacts, corrosion-resistant apparatus, and in dentistry.

Platinum-cobalt alloys have magnetic properties. One such alloy made of 76.7% Pt and 23.3% Co, by weight, is an extremely powerful magnet that offers a B-H (max) almost twice that of Alnico V. Platinum resistance wires are used for constructing high-temperature electric furnaces.

The metal is used for coating missile nose cones, jet engine fuel nozzles, etc., which must perform reliably at high temperatures for long periods of time. The metal, like palladium, absorbs large volumes of hydrogen, retaining it at ordinary temperatures but giving it up when heated.

In the finely divided state platinum is an excellent catalyst, having long been used in the contact process for producing sulfuric acid. It is also used as a catalyst in cracking petroleum products. Much interest exists in using platinum as a catalyst in fuel cells and in antipollution devices for automobiles.

Platinum anodes are extensively used in cathodic protection systems for large ships and ocean-going vessels, pipelines, steel piers, etc. Fine platinum wire will glow red hot when placed in the vapor of methyl alcohol. It acts here as a catalyst, converting the alcohol to formaldehyde. The phenomenon has been used commercially to produce cigarette lighters and hand warmers. Hydrogen and oxygen explode in the presence of platinum.

Sources

Platinum occurs natively, accompanied by small quantities of iridium, osmium, palladium, ruthenium, and rhodium, all belonging to the same group of metals. These are found in the alluvial deposits of the Ural mountains, of Columbia, and of certain western American states. Sperrylite, occurring with the nickel-bearing deposits of Sudbury, Ontario, is the source of a considerable amount of metal.

The large production of nickel makes up for the fact that is only one part of the platinum metals in two million parts of ore.

Compounds

See more information at the Platinum compound page.

Element Forms

CID Name Formula SMILES Molecular Weight
23939 platinum Pt [Pt] 195.08
105166 platinum(2+) Pt+2 [Pt+2] 195.08
105160 platinum(4+) Pt+4 [Pt+4] 195.08
161142 platinum-191 Pt [191Pt] 190.96168
167028 platinum-195 Pt [195Pt] 194.964794
167343 platinum-199 Pt [199Pt] 198.97060
167351 platinum-193 Pt [193Pt] 192.96298
177513 platinum-188 Pt [188Pt] 187.95940
177537 platinum-186 Pt [186Pt] 185.9594
177652 platinum-197 Pt [197Pt] 196.967343
185697 platinum-200 Pt [200Pt] 199.9714
177550 platinum-189 Pt [189Pt] 188.9608
46898737 platinum-195(4+) Pt+4 [195Pt+4] 194.964794

Isotopes

Stable Isotope Count 5

Isotopes in Earth/Planetary Science

Astrophysicists have confirmed an anomaly in the isotopic composition of platinum in the chemically peculiar HgMn star χ Lupi, where the platinum isotopic composition was shown to be a mixture of 196Pt and 198Pt (Fig. IUPAC.78.1) [526].

Fig. IUPAC.78.1: Observed spectra of the chemically peculiar HgMn star χ Lupi (solid blue line) compared to a synthetic spectra calculated with a mixture of 70 percent ¹⁹⁶Pt and 30 percent ¹⁹⁸Pt (dotted pink line) (modified after [526]).

[526] G. Kalus, S. Johansson, G. M. Wahlgren, D. S. Leckrone, A. P. Thorne, J. C. Brandt. Astrophys. J.494, 792 (1998).

Isotopes in Geochronology

The decay of 190Pt (with a half-life of 4.9×1011 years) to 186Os over time has been used for dating rocks and iron meteorites [527].

[527] J. A. Coggona, G. M. Nowella, D. G. Pearsona, T. Oberthürb, J.-P. Lorandc, F. Melcherb, S. W. Parmand. Chem. Geol.302-303, 48 (2012).

Isotopes in Medicine

195mPt (with a half-life of 4 days) is used for pharmacokinetic studies of platinum-based anti-tumor agents in cancer diagnosis and cancer therapy [188]. The m in the superscript of 195mPt indicates a metastable state of the isotope. 195mPt can be produced from the stable isotopes 192Os or 195Pt via the 192Os (α, n) 195mPt reaction and the 195Pt (n, n′) 195mPt reaction, respectively.

[188] S. J. Adelstein, F. J. Manning. Isotopes for Medicine and the Life Sciences, pp. 20–25, National Academy Press, Washington DC (1995).

Isotope Mass and Abundance

Isotope Atomic Mass (uncertainty) [u] Abundance (uncertainty)
190Pt 189.959 950(5) 0.000 12(2) 0.00012(2)
192Pt 191.961 04(2) 0.007 82(24) 0.00782(24)
194Pt 193.962 683(3) 0.328 64(410) 0.3286(40)
195Pt 194.964 794(3) 0.337 75(240) 0.3378(24)
196Pt 195.964 955(3) 0.252 11(340) 0.2521(34)
198Pt 197.967 90(2) 0.073 56(130) 0.07356(130)

Atomic Mass, Half Life, and Decay

Nuclide Atomic Mass and Uncertainty [u] Half Life and Uncertainty Discovery Year Decay Modes, Intensities and Uncertainties [%]
165Pt 164.999658 ± 0.000429 [Estimated] 370 us ± 180 2019 α=100%
166Pt 165.994866 ± 0.000322 [Estimated] 294 us ± 62 1996 α=100%
167Pt 166.992750 ± 0.000329 [Estimated] 915 us ± 123 1996 α=100%
168Pt 167.988180196 ± 0.00016096 2.02 ms ± 0.10 1981 α≈100%; β+ ?
169Pt 168.986619 ± 0.000215 [Estimated] 6.99 ms ± 0.09 1981 α≈100%; β+ ?
170Pt 169.982502087 ± 0.000019588 13.93 ms ± 0.16 1981 α≈100%; β+ ?
171Pt 170.981248868 ± 0.000086904 45.5 ms ± 2.5 1981 α=86±0.3%; β+ ?
171Ptm 170.981248868 ± 0.000086904 901 ns ± 9 2010 IT=100%
172Pt 171.977341059 ± 0.000011139 97.6 ms ± 1.3 1981 α=96±0.3%; β+ ?
173Pt 172.976449922 ± 0.000068096 382 ms ± 2 1966 α=86±0.4%; β+ ?
174Pt 173.972820431 ± 0.000011098 862 ms ± 8 1966 α=74.9±2.4%; β+ ?
175Pt 174.972400593 ± 0.000019982 2.43 s ± 0.04 1966 α=64±0.5%; β+ ?
176Pt 175.968938162 ± 0.000013647 6.33 s ± 0.15 1966 β+ ?; α=40±0.2%
177Pt 176.968469541 ± 0.00001609 10.0 s ± 0.4 1966 β+=94.3±0.5%; α=5.7±0.5%
177Ptm 176.968469541 ± 0.00001609 2.35 us ± 0.04 1979 IT=100%
178Pt 177.965649288 ± 0.000010878 20.7 s ± 0.7 1966 β+=92.3±0.3%; α=7.7±0.3%
179Pt 178.965358742 ± 0.000008563 21.2 s ± 0.4 1966 β+≈100%; α=0.24±0.3%
180Pt 179.963038010 ± 0.00001079 56 s ± 3 1966 β+=99.48±0.5%; α=0.52±0.5%
181Pt 180.963089946 ± 0.000014695 52.0 s ± 2.2 1966 β+≈100%; α=0.074±1%
181Ptm 180.963089946 ± 0.000014695 >300 ns 1992 IT=100%
182Pt 181.961171605 ± 0.000014057 2.67 m ± 0.12 1963 β+=0.962±0.2%; α=0.038±0.2%
183Pt 182.961595895 ± 0.000015261 6.5 m ± 1.0 1963 β+≈100%; α=0.0096±0.5%
183Ptm 182.961595895 ± 0.000015261 43 s ± 5 1979 β+=96.9±0.8%; IT=3.1±0.8%; α ?
183Ptn 182.961595895 ± 0.000015261 >150 ns 1990 IT=100%
184Pt 183.959921929 ± 0.000015828 17.3 m ± 0.2 1963 β+≈100%; α=0.0017±0.7%
184Ptm 183.959921929 ± 0.000015828 1.01 ms ± 0.05 1966 IT=100%
185Pt 184.960613659 ± 0.000027731 70.9 m ± 2.4 1960 β+≈100%; α=0.0050±2%
185Ptm 184.960613659 ± 0.000027731 33.0 m ± 0.8 1970 β+≈100%; IT ?
185Ptn 184.960613659 ± 0.000027731 728 ns ± 20 1996 IT=100%
186Pt 185.959350845 ± 0.000023344 2.08 h ± 0.05 1961 β+=100%; α≈1.4e-4%
187Pt 186.960616646 ± 0.000025837 2.35 h ± 0.03 1961 β+=100%
187Ptm 186.960616646 ± 0.000025837 311 us ± 15 1976 IT=100%
188Pt 187.959397521 ± 0.000005694 10.16 d ± 0.18 1954 ε=100%; α=2.6e-5±0.3%
189Pt 188.960848485 ± 0.000010832 10.87 h ± 0.12 1955 β+=100%
189Ptm 188.960848485 ± 0.000010832 464 ns ± 25 1970 IT=100%
189Ptn 188.960848485 ± 0.000010832 143 us ± 5 1976 IT=100%
190Pt 189.959949823 ± 0.000000705 483 Gy ± 3 1949 IS=0.012±0.2%; α=100%; 2β+ ?
191Pt 190.961676261 ± 0.00000443 2.83 d ± 0.02 1948 ε=100%
191Ptm 190.961676261 ± 0.00000443 >1 us 1976 IT=100%
191Ptn 190.961676261 ± 0.00000443 95 us ± 5 1967 IT=100%
192Pt 191.961042667 ± 0.000002758 Stable >60Py 1935 IS=0.782±2.4%; α ?
192Ptm 191.961042667 ± 0.000002758 272 ns ± 23 1976 IT=100%
193Pt 192.962984546 ± 0.000001458 50 y ± 6 1948 ε=100%
193Ptm 192.962984546 ± 0.000001458 4.33 d ± 0.03 1949 IT=100%
194Pt 193.962683498 ± 0.000000532 Stable 1935 IS=32.864±41%
195Pt 194.964794325 ± 0.00000054 Stable >6.3Ey 1935 IS=33.775±24%; α ?
195Ptm 194.964794325 ± 0.00000054 4.010 d ± 0.005 1960 IT=100%
196Pt 195.964954648 ± 0.000000547 Stable 1935 IS=25.211±34%
197Pt 196.967343030 ± 0.000000575 19.8915 h ± 0.0019 1936 β-=100%
197Ptm 196.967343030 ± 0.000000575 95.41 m ± 0.18 1941 IT=96.7±0.4%; β-=3.3±0.4%
198Pt 197.967896718 ± 0.000002254 Stable 1935 IS=7.356±13%; 2β- ?; α ?
199Pt 198.970597022 ± 0.000002317 30.80 m ± 0.21 1937 β-=100%
199Ptm 198.970597022 ± 0.000002317 13.48 s ± 0.16 1959 IT=100%
200Pt 199.971444609 ± 0.000021588 12.6 h ± 0.3 1957 β-=100%
201Pt 200.974513305 ± 0.000053788 2.5 m ± 0.1 1962 β-=100%
201Ptm 200.974513305 ± 0.000053788 10 s [Estimated] IT ?
202Pt 201.975639000 ± 0.000027 44 h ± 15 1992 β-=100%
202Ptm 201.975639000 ± 0.000027 141 us ± 7 2005 IT=100%
203Pt 202.979055 ± 0.000215 [Estimated] 22 s ± 4 2008 β-=100%
203Ptm 202.979055 ± 0.000215 [Estimated] 12 s ± 5 2008 β-≈100%; IT ?
203Ptn 202.979055 ± 0.000215 [Estimated] >100 ns [Estimated] 2008 IT=100%
203Ptp 202.979055 ± 0.000215 [Estimated] 641 ns ± 55 2011 IT=100%
204Pt 203.981084 ± 0.000215 [Estimated] 10.3 s ± 1.4 2008 β-=100%
204Ptm 203.981084 ± 0.000215 [Estimated] 5.5 us ± 0.7 2009 IT=100%
204Ptn 203.981084 ± 0.000215 [Estimated] 55 us ± 3 2009 IT=100%
204Ptp 203.981084 ± 0.000215 [Estimated] 146 ns ± 14 2009 IT=100%
205Pt 204.986237 ± 0.000322 [Estimated] 2 s >300ns [Estimated] 2009 β- ?
206Pt 205.990080 ± 0.000322 [Estimated] 500 ms >300ns [Estimated] 2012 β- ?; β-n ?
207Pt 206.995556 ± 0.000429 [Estimated] 600 ms >300ns [Estimated] 2012 β- ?; β-n ?
208Pt 207.999463 ± 0.000429 [Estimated] 220 ms >300ns [Estimated] 2012 β- ?; β-n ?

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
    Platinum

Shall we send you a message when we have discounts available?

Remind me later

Thank you! Please check your email inbox to confirm.

Oops! Notifications are disabled.