77
Ir
Iridium
Atomic Mass 192.217
Electron Configuration [Xe]6s24f145d7
Oxidation States +4, +3
Year Discovered 1803

Identifiers

Element Name Iridium
Element Symbol Ir
InChI InChI=1S/Ir
InChIKey GKOZUEZYRPOHIO-UHFFFAOYSA-N

Properties

Atomic Weight

192.217(2)

192.217

192.2

192.217(3)

Electron Configuration

[Xe]6s24f145d7

Atomic Radius

Van der Waals Atomic Radius : 202 pm (Van der Waals)

Empirical Atomic Radius : 135pm (Empirical)

Covalent Atomic Radius : 141(6) pm (Covalent)

Oxidation States

+4, +3

-3, -1, 0, 1, 2, 3, 4, 5, 6, 7, 8, 9

Ground Level

4F9/2

Ionization Energy

9.1 eV

8.96702 ± 0.00022 eV

Electronegativity

Pauling Scale Electronegativity : 2.2(Pauling Scale)

Allen Scale Electronegativity : 1.68(Allen Scale)

Electron Affinity

1.565eV

1.97eV

Atomic Spectra

Lines Holdings

Levels Holdings

Physical Description

Solid

Element Classification

Metal

Element Period Number

6

Element Group Number

9

Density

22.42 grams per cubic centimeter

Melting Point

2719 K (2446°C or 4435°F)

2446°C

Boiling Point

4701 K (4428°C or 8002°F)

4130°C

Estimated Crustal Abundance

1×10-3 milligrams per kilogram

Estimated Oceanic Abundance

Not Applicable

History

The name derives from the Latin Iris, the Greek goddess of rainbows, because of the variety of colours in the element's salt solutions. Iridium and osmium were both discovered in a crude platinum ore in 1803 by the English chemist Smithson Tennant. Iridium was discovered independently by the French chemist H. V. Collet-Descotils, who actually published his paper one month before Tennant, but Tennant is given credit for the discovery, perhaps because he alone also found osmium in the ore.

Iridium and osmium were discovered at the same time by the British chemist Smithson Tennant in 1803. Iridium and osmium were identified in the black residue remaining after dissolving platinum ore with aqua regia, a mixture of 25% nitric acid (HNO3) and 75% hydrochloric acid (HCl). Today, iridium is still obtained from platinum ores and as a by-product of mining nickel.

From the Latin word iris meaning rainbow. Tennant discovered iridium in 1803 in the residue left when crude platinum is dissolved by aqua regia. The name iridium is appropriate because its salts are highly colored.

Historical Atomic Weights

Year Atomic Weight (uncertainty) [u] Reference
2017 192.217(2) https://doi.org/10.1515/pac-2019-0603
1993 192.217(3) https://doi.org/10.1351/pac199466122423
1969 192.22(3) https://doi.org/10.1351/pac197021010091
1953 192.2 https://doi.org/10.1039/JR9540004713
1909 193.1 https://doi.org/10.1021/ja01931a001
1902 193.0 https://doi.org/10.1007/BF01370337

Historical Isotopic Abundances

Year Isotope Abundance (uncertainty) Reference
2017 191Ir 0.3723(9)
2017 193Ir 0.6277(9)
1997 191Ir 0.373(2) https://doi.org/10.1351/pac199870010217
1997 193Ir 0.627(2) https://doi.org/10.1351/pac199870010217
1979 191Ir 0.373(3) https://doi.org/10.1351/pac198052102349
1979 193Ir 0.627(3) https://doi.org/10.1351/pac198052102349
1975 191Ir 0.373 https://doi.org/10.1351/pac197647010075
1975 193Ir 0.627 https://doi.org/10.1351/pac197647010075

Description

Iridium, a metal of the platinum family, is white (similar to platinum) but with a slight yellowish cast. Because iridium is very hard and brittle, it is hard to machine, form, or work.

It is the most corrosion-resistant metal known, and was used in making the standard meter bar of Paris, which is a 90 percent platinum and 10 percent iridium alloy. This meter bar was replaced in 1960 as a fundamental unit of length (see Krypton).

Iridium is not attacked by any of the acids nor by aqua regia, but is attacked by molten salts, such as NaCl and NaCN. The specific gravity of iridium is to osmium's specific gravity. Calculations of the densities of iridium and osmium from the space lattices give values of 22.65 and 22.61 g/cm^3, respectively. These values may be more reliable than actual physical measurements for determining which element is heavier.

Users

Pure iridium is very brittle and is nearly impossible to machine. It is primarily used as a hardening agent for platinum. Platinum-iridium alloys are used to make crucibles and other high temperature equipment. Iridium is also alloyed with osmium to make the tips of fountain pens and compass bearings.

Iridium is the most corrosive resistant metal known. For this reason, the standard meter bar was created from an alloy of 90% platinum and 10% iridium. This bar was replaced as the definition of the meter in 1960 when the meter was redefined in terms of the orange-red spectral line of krypton-86.

A thin, worldwide layer of iridium exists in a layer of sediment that was put down at the end of the Cretaceous period. Since meteors and asteroids contain a higher percentage of iridium than the earth's crust, this iridium enriched layer is seen as evidence that the earth was struck by a large meteor or asteroid at that time. Dust from the impact would have spread around the globe, depositing the iridium. The dust also would have blocked the sun for a time, resulting in the extinction of many plant and animal species, including the dinosaurs.

Although its principal use is as a hardening agent for platinum, iridium is also used to make crucibles and devices requiring high temperatures. It is also used for electrical contacts.

The element forms an alloy with osmium which is used for tipping pens and compass bearings.

Sources

Iridium occurs uncombined in nature with platinum and other metals of this family in alluvial deposits. It is recovered as a by-product from the nickel mining industry.

Compounds

See more information at the Iridium compound page.

Element Forms

CID Name Formula SMILES Molecular Weight
23924 iridium Ir [Ir] 192.22
66373 iridium-192 Ir [192Ir] 191.96260
168053 iridium(3+) Ir+3 [Ir+3] 192.22
178173 iridium-194 Ir [194Ir] 193.96508
185619 iridium-184 Ir [184Ir] 183.9575
16097723 iridium-191 Ir [191Ir] 190.96059
167365 iridium-188 Ir [188Ir] 187.9588
177484 iridium-187 Ir [187Ir] 186.9575
177690 iridium-195 Ir [195Ir] 194.96598
178177 iridium-189 Ir [189Ir] 188.9587
185569 iridium-186 Ir [186Ir] 185.9579
185674 iridium-182 Ir [182Ir] 181.9581
44146835 iridium-193 Ir [193Ir] 192.96292
167220 iridium-190 Ir [190Ir] 189.96054
185673 iridium-185 Ir [185Ir] 184.9567

Isotopes

Stable Isotope Count 2

Isotopes in Industry

Metallic 192Ir (with a half-life of 74 days) is used as a radiation source in gamma cameras for non-destructive testing of products for manufacturing flaws, such as aircraft parts, boilers, and pipeline welds (Fig. IUPAC.77.1) [274].

Fig. IUPAC.77.1: This is a radiograph of a weld using ¹⁹²Ir as the source of radiation. The gamma rays given off by the isotope enable imperfections in the weld to be seen on the radiograph. (Photo Source: Hayward and Currie, 2006) [274].

[274] P. Hayward, D. Currie. “Radiography of welds using seleniuim 75, Ir 192 and x-rays”, in Asia-Pacific Conference on NDT, Auckland, New Zealand (2006).

Isotopes in Medicine

Metallic 192Ir is used in brachytherapy [188], [521], [522], [523]. 191mIr (with a half-life of 5 s) is used for blood flow imaging (angiography), especially in pediatric populations [524], [525]. The m in the superscript 191mIr indicates a metastable state of the isotope.

[188] S. J. Adelstein, F. J. Manning. Isotopes for Medicine and the Life Sciences, pp. 20–25, National Academy Press, Washington DC (1995).
[521] A. Talamo, Y. Gohar. Radioactive Isotope Production for Medical Applications Using Kharkov Electron Driven Subcritical Assembly Facility, ANL-07/18, Argonne National Laboratory Argonne, Illinois (2007).
[522] S. A. Buzdar, M. A. Gadhi, M. A. Rao, N. A. Laghari, M. Anees. J. Pak. Med. Assoc.59, 113 (2009).
[523] T. Genkaa, S. Iwamotoa, E. Juitab, N. Takeuchia. Nucl. Inst. Methods Phys. Res. Section A: Accelerators, Spectrometers, Detectors and Associated Equipment.369, 709 (1996).
[524] K. J. Kairemo, M. S. Kestilä, S. Savolainen, O. A. Korhola, J. V. Hiltunen, R. I. Svahn, E. T. Korppi Tommola, F. F. Knapp, C. Brihaye. J. Nucl. Biol. Med.38, 86 (1994).
[525] S. T. Treves, A. B. Packard, L. C. T. Fung. J. Nucl. Med.45, 508 (2004).

Isotopes Used as a Source of Radioactive Isotope(s)

Iridium consists of two stable isotopes (191Ir and 193Ir) from which the radioactive isotopes 192Ir and 195mPt (with a half-life of 4 days) can be produced. Both are used in nuclear medicine. The m in the superscript 195mPt indicates a metastable state of the isotope.

Isotope Mass and Abundance

Isotope Atomic Mass (uncertainty) [u] Abundance (uncertainty)
191Ir 190.960 591(9) 0.3723(9)
193Ir 192.962 924(9) 0.6277(9)
Isotope Atomic Mass (uncertainty) [u] Abundance (uncertainty)
191Ir 190.9605893(21) 0.373(2)
193Ir 192.9629216(21) 0.627(2)

Atomic Mass, Half Life, and Decay

Nuclide Atomic Mass and Uncertainty [u] Half Life and Uncertainty Discovery Year Decay Modes, Intensities and Uncertainties [%]
163Ir 162.994299 ± 0.000429 [Estimated] Not-specified p ?
164Ir 163.991966 ± 0.000339 [Estimated] 1 ms [Estimated] p ?; α ?; β+ ?
164Irm 163.991966 ± 0.000339 [Estimated] 70 us ± 10 2001 p=?; α=4±0.2%; β+ ?
165Ir 164.987552 ± 0.00017 [Estimated] 50 ns [Estimated] p ?; α ?
165Irm 164.987552 ± 0.00017 [Estimated] 325 us ± 33 1997 p=88±0.2%; α=12±0.2%
166Ir 165.985716 ± 0.000215 [Estimated] 10.5 ms ± 2.2 1981 α=93±0.3%; p=7±0.3%
166Irm 165.985716 ± 0.000215 [Estimated] 15.1 ms ± 0.9 1996 α=98.2±0.6%; p=1.8±0.6%
167Ir 166.981671973 ± 0.000019694 29.3 ms ± 0.6 1981 α=43.5±1.9%; p=38.6±1.2%; β+ ?
167Irm 166.981671973 ± 0.000019694 28.5 ms ± 0.5 1995 α=89±0.3%; β+ ?; p=0.41±0.6%
168Ir 167.979960978 ± 0.000059277 230 ms ± 50 1978 α≈100%; β+ ?; β+p ?
168Irm 167.979960978 ± 0.000059277 163 ms ± 16 1996 α=77±0.9%; β+ ?; β+p ?
169Ir 168.976281743 ± 0.00002502 353 ms ± 4 1978 α=53±0.7%; β+ ?
169Irm 168.976281743 ± 0.00002502 280 ms ± 1 1984 α=79±0.5%; β+ ?; p ?
170Ir 169.975113 ± 0.000109 [Estimated] 910 ms ± 150 1977 β+ ?; α=5.2±1.7%
170Irm 169.975113 ± 0.000109 [Estimated] 811 ms ± 18 1977 α=38±0.5%; β+ ?; IT ?
171Ir 170.971645520 ± 0.000041295 3.1 s ± 0.3 1967 β+ ?; α=15±0.2%
171Irm 170.971645520 ± 0.000041295 1.47 s ± 0.06 1967 α=54±0.5%; β+ ?; p ?
172Ir 171.970607035 ± 0.000034785 4.4 s ± 0.3 1967 β+≈98%; α≈2%
172Irm 171.970607035 ± 0.000034785 2.19 s ± 0.07 1967 β+=90.5±1.1%; α=9.5±1.1%
173Ir 172.967505477 ± 0.000011316 9.0 s ± 0.8 1967 β+=96.5±2%; α=3.5±2%
173Irm 172.967505477 ± 0.000011316 2.20 s ± 0.05 1967 β+=88±0.1%; α=12±0.1%
174Ir 173.966949939 ± 0.000012046 7.9 s ± 0.6 1967 β+=99.5±0.3%; α=0.5±0.3%
174Irm 173.966949939 ± 0.000012046 4.9 s ± 0.3 1992 β+=97.5±0.3%; α=2.5±0.3%
175Ir 174.964149519 ± 0.000013295 9 s ± 2 1967 β+=99.15±2.8%; α=0.85±2.8%
175Irm 174.964149519 ± 0.000013295 33 s ± 4 1967 β+= ?; IT ?
175Irn 174.964149519 ± 0.000013295 6.58 us ± 0.15 2019 IT=100%
176Ir 175.963626261 ± 0.000008679 8.7 s ± 0.5 1967 β+=96.9±0.6%; α=3.1±0.6%
176Irm 175.963626261 ± 0.000008679 10 s [Estimated] β+= ?; IT ?
177Ir 176.961301500 ± 0.000021213 29.8 s ± 1.7 1967 β+≈100%; α=0.06±0.1%
177Irm 176.961301500 ± 0.000021213 >100 ns IT=100%
177Irn 176.961301500 ± 0.000021213 >100 ns 1991 IT=100%
178Ir 177.961079395 ± 0.000020204 12 s ± 2 1972 β+=100%
179Ir 178.959117594 ± 0.000010489 79 s ± 1 1992 β+=100%
180Ir 179.959229446 ± 0.000023302 1.5 m ± 0.1 1972 β+=100%
181Ir 180.957634691 ± 0.000005631 4.90 m ± 0.15 1972 β+=100%
181Irm 180.957634691 ± 0.000005631 298 ns 1992 IT=100%
181Irn 180.957634691 ± 0.000005631 126 ns ± 6 1992 IT=100%
182Ir 181.958076296 ± 0.000022509 15.0 m ± 1.0 1961 β+=100%
182Irm 181.958076296 ± 0.000022509 170 ns ± 40 1990 IT=100%
182Irn 181.958076296 ± 0.000022509 130 ns ± 50 1990 IT=100%
183Ir 182.956841231 ± 0.000026486 58 m ± 5 1961 β+≈100%; α ?
184Ir 183.957476000 ± 0.00003 3.09 h ± 0.03 1960 β+=100%
184Irm 183.957476000 ± 0.00003 470 us ± 30 1988 IT=100%
184Irn 183.957476000 ± 0.00003 350 ns ± 90 1988 IT=100%
185Ir 184.956698000 ± 0.00003 14.4 h ± 0.1 1958 β+=100%
185Irm 184.956698000 ± 0.00003 120 ns ± 20 1979 IT=100%
186Ir 185.957946754 ± 0.00001774 16.64 h ± 0.03 1958 β+=100%
186Irm 185.957946754 ± 0.00001774 1.92 h ± 0.05 1962 β+≈75%; IT≈25%
187Ir 186.957542000 ± 0.00003 10.5 h ± 0.3 1958 β+=100%
187Irm 186.957542000 ± 0.00003 30.3 ms ± 0.6 1963 IT=100%
187Irn 186.957542000 ± 0.00003 152 ns ± 12 1969 IT=100%
187Irp 186.957542000 ± 0.00003 1.8 us ± 0.5 2010 IT=100%
188Ir 187.958834999 ± 0.000010116 41.5 h ± 0.5 1950 β+=100%
188Irm 187.958834999 ± 0.000010116 4.15 ms ± 0.15 1971 IT≈100%; β+ ?
189Ir 188.958722602 ± 0.0000135 13.2 d ± 0.1 1955 ε=100%
189Irm 188.958722602 ± 0.0000135 13.3 ms ± 0.3 1960 IT=100%
189Irn 188.958722602 ± 0.0000135 3.7 ms ± 0.2 1975 IT=100%
190Ir 189.960543374 ± 0.00000147 11.78 d ± 0.10 1947 β+=100%; e+<0.002%
190Irm 189.960543374 ± 0.00000147 1.120 h ± 0.003 1964 IT=100%
190Irn 189.960543374 ± 0.00000147 >2 us 1996 IT=100%
190Irp 189.960543374 ± 0.00000147 3.087 h ± 0.012 1950 β+=91.4±0.2%; IT=8.6±0.2%
191Ir 190.960591455 ± 0.000001406 Stable 1935 IS=37.3±0.2%
191Irm 190.960591455 ± 0.000001406 4.899 s ± 0.023 1955 IT=100%
191Irn 190.960591455 ± 0.000001406 5.7 s ± 0.4 1979 IT=100%
192Ir 191.962602414 ± 0.00000141 73.820 d ± 0.014 1937 β-=95.24±0.4%; ε=4.76±0.4%
192Irm 191.962602414 ± 0.00000141 1.45 m ± 0.05 1937 IT≈100%; β-=0.0175%
192Irn 191.962602414 ± 0.00000141 241 y ± 9 1959 IT=100%
193Ir 192.962923753 ± 0.000001425 Stable 1935 IS=62.7±0.2%
193Irm 192.962923753 ± 0.000001425 10.53 d ± 0.04 1957 IT=100%
193Irn 192.962923753 ± 0.000001425 124.8 us ± 2.1 2012 IT=100%
194Ir 193.965075703 ± 0.000001429 19.35 h ± 0.07 1937 β-=100%
194Irm 193.965075703 ± 0.000001429 31.85 ms ± 0.24 1959 IT=100%
194Irn 193.965075703 ± 0.000001429 171 d ± 11 1968 β-=100%
195Ir 194.965976898 ± 0.000001431 2.29 h ± 0.17 1952 β-=100%
195Irm 194.965976898 ± 0.000001431 3.74 h ± 0.07 1968 β-≈100%; IT ?
195Irn 194.965976898 ± 0.000001431 4.4 us ± 0.6 2011 IT=100%
196Ir 195.968399669 ± 0.000041239 52.0 s ± 1.1 1966 β-=100%
196Irm 195.968399669 ± 0.000041239 1.40 h ± 0.02 1959 β-≈100%; IT ?
197Ir 196.969657217 ± 0.000021588 5.8 m ± 0.5 1952 β-=100%
197Irm 196.969657217 ± 0.000021588 8.9 m ± 0.3 1976 β-≈100%; IT ?
197Irn 196.969657217 ± 0.000021588 30 us ± 8 2005 IT=100%
197Irp 196.969657217 ± 0.000021588 15 us ± 9 2005 IT=100%
198Ir 197.972399 ± 0.000215 [Estimated] 8.7 s ± 0.4 1973 β-=100%
199Ir 198.973807097 ± 0.000044073 7 s ± 5 1993 β-=100%
200Ir 199.976844 ± 0.00021 [Estimated] 43 s ± 6 2008 β-=100%; β-n ?
201Ir 200.978701 ± 0.000215 [Estimated] 21 s ± 5 2008 β-=100%
202Ir 201.982136 ± 0.000322 [Estimated] 11 s ± 3 2008 β-=100%
202Irm 201.982136 ± 0.000322 [Estimated] 3.4 us ± 0.6 2011 IT=100%
203Ir 202.984573 ± 0.000429 [Estimated] 7 s >300ns [Estimated] 2009 β- ?
203Irm 202.984573 ± 0.000429 [Estimated] >100 ns [Estimated] IT ?; β- ?
203Irn 202.984573 ± 0.000429 [Estimated] 798 ns ± 350 2011 IT=100%
204Ir 203.989726 ± 0.000429 [Estimated] 2 s >300ns [Estimated] 2011 β- ?; β-n ?
205Ir 204.993988 ± 0.000537 [Estimated] 1 s >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
    Iridium

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