68
Er
Erbium
Atomic Mass 167.259
Electron Configuration [Xe]6s24f12
Oxidation States +3
Year Discovered 1843

Identifiers

Element Name Erbium
Element Symbol Er
InChI InChI=1S/Er
InChIKey UYAHIZSMUZPPFV-UHFFFAOYSA-N

Properties

Atomic Weight

167.259(3)

167.259

167.3

167.259(3)

Electron Configuration

[Xe]6s24f12

Atomic Radius

Van der Waals Atomic Radius : 235 pm (Van der Waals)

Empirical Atomic Radius : 175pm (Empirical)

Covalent Atomic Radius : 189(6) pm (Covalent)

Oxidation States

+3

3, 2, 1 ​(a basic oxide)

Ground Level

3H6

Ionization Energy

6.108 eV

6.1077 ± 0.0010 eV

Electronegativity

Pauling Scale Electronegativity : 1.24(Pauling Scale)

Atomic Spectra

Lines Holdings

Levels Holdings

Physical Description

Solid

Element Classification

Metal

Element Period Number

6

Element Group Number

- Lanthanide

Density

9.07 grams per cubic centimeter

Melting Point

1802 K (1529°C or 2784°F)

1529°C

Boiling Point

3141 K (2868°C or 5194°F)

2868°C

Estimated Crustal Abundance

3.5 milligrams per kilogram

Estimated Oceanic Abundance

8.7×10-7 milligrams per liter

History

The name derives from the Swedish town of Ytterby, where the ore gadolinite (in which it was found) was first mined. Erbium was discovered by the Swedish surgeon and chemist Carl-Gustav Mosander in 1843 in a yttrium sample. He separated the yttrium into yttrium, a rose-coloured salt he called terbium and a deep-yellow peroxide that he called erbium.

The mineral gadolinite ((Ce, La, Nd, Y)2FeBe2Si2O10), discovered in a quarry near the town of Ytterby, Sweden, has been the source of a great number of rare earth elements. In 1843, Carl Gustaf Mosander, a Swedish chemist, was able to separate gadolinite into three materials, which he named yttria, erbia and terbia. As might be expected considering the similarities between their names and properties, scientists soon confused erbia and terbia and, by 1877, had reversed their names. What Mosander called erbia is now called terbia and visa versa. From these two substances, Mosander discovered two new elements, terbium and erbium. Today, erbium is primarily obtained through an ion exchange process from the minerals xenotime (YPO4) and euxenite ((Y, Ca, Er, La, Ce, U, Th)(Nb, Ta, Ti)2O6).

Erbium, one of the so-called rare-earth elements on the lanthanide series, is found in the minerals mentioned under dysprosium. In 1842 Mosander separated "yttria" found in the mineral gadolinite, into three fractions which he called yttria, erbia, and terbia. The names erbia and terbia became confused in this early period. After 1860, Mosander's terbia was known as erbia, and after 1877, the earlier known erbia became terbia. The erbia of this period was later shown to consist of five oxides, now known as erbia, scandia, holmia, thulia and ytterbia. By 1905 Urbain and James independently succeeded in isolating fairly pure Er2O3. Klemm and Bommer first produced reasonably pure erbium metal in 1934 by reducing the anhydrous chloride with potassium vapor.

Historical Atomic Weights

Year Atomic Weight (uncertainty) [u] Reference
1999 167.259(3) https://doi.org/10.1351/pac200173040667
1969 167.26(3) https://doi.org/10.1351/pac197021010091
1961 167.26 https://doi.org/10.1021/ja00881a001
1955 167.27 https://doi.org/10.1021/ja01595a001
1938 167.2 https://doi.org/10.1039/JR9380001101
1931 167.64 https://doi.org/10.1039/JR9310001617
1912 167.7 https://doi.org/10.1021/ja02224a601
1909 167.4 https://doi.org/10.1021/ja01931a001
1902 166 https://doi.org/10.1007/BF01370337

Historical Isotopic Abundances

Year Isotope Abundance (uncertainty) Reference
2001 162Er 0.001 39(5) https://doi.org/10.1063/1.1836764
2001 164Er 0.016 01(3) https://doi.org/10.1063/1.1836764
2001 166Er 0.335 03(36) https://doi.org/10.1063/1.1836764
2001 167Er 0.228 69(9) https://doi.org/10.1063/1.1836764
2001 168Er 0.269 78(18) https://doi.org/10.1063/1.1836764
2001 170Er 0.149 10(36) https://doi.org/10.1063/1.1836764
1997 162Er 0.0014(1) https://doi.org/10.1351/pac199870010217
1997 164Er 0.0161(3) https://doi.org/10.1351/pac199870010217
1997 166Er 0.3361(35) https://doi.org/10.1351/pac199870010217
1997 167Er 0.2293(17) https://doi.org/10.1351/pac199870010217
1997 168Er 0.2678(26) https://doi.org/10.1351/pac199870010217
1997 170Er 0.1493(27) https://doi.org/10.1351/pac199870010217
1989 162Er 0.0014(1) https://doi.org/10.1351/pac199163070991
1989 164Er 0.0161(2) https://doi.org/10.1351/pac199163070991
1989 166Er 0.336(2) https://doi.org/10.1351/pac199163070991
1989 167Er 0.2295(15) https://doi.org/10.1351/pac199163070991
1989 168Er 0.268(2) https://doi.org/10.1351/pac199163070991
1989 170Er 0.149(2) https://doi.org/10.1351/pac199163070991
1979 162Er 0.0014(1) https://doi.org/10.1351/pac198052102349
1979 164Er 0.0156(6) https://doi.org/10.1351/pac198052102349
1979 166Er 0.334(6) https://doi.org/10.1351/pac198052102349
1979 167Er 0.229(4) https://doi.org/10.1351/pac198052102349
1979 168Er 0.271(6) https://doi.org/10.1351/pac198052102349
1979 170Er 0.149(4) https://doi.org/10.1351/pac198052102349
1975 162Er 0.001 https://doi.org/10.1351/pac197647010075
1975 164Er 0.016 https://doi.org/10.1351/pac197647010075
1975 166Er 0.334 https://doi.org/10.1351/pac197647010075
1975 167Er 0.229 https://doi.org/10.1351/pac197647010075
1975 168Er 0.27 https://doi.org/10.1351/pac197647010075
1975 170Er 0.15 https://doi.org/10.1351/pac197647010075

Description

The pure metal is soft and malleable and has a bright, silvery, metallic luster. As with other rare-earth metals, its properties depend to a certain extent on the impurities present. The metal is fairly stable in air and does not oxidize as rapidly as some of the other rare-earth metals. Naturally occurring erbium is a mixture of six isotopes, all of which are stable. Nine radioactive isotopes of erbium are also recognized. Recent production techniques, using ion-exchange reactions, have resulted in much lower prices of the rare-earth metals and their compounds in recent years. Most of the rare-earth oxides have sharp absorption bands in the visible, ultraviolet, and near infrared. This property, associated with the electronic structure, gives beautiful pastel colors to many of the rare-earth salts.

Users

Erbium is alloyed with vanadium to make it softer and easier to shape. Erbium is added to fiber optic cables as a doping agent where it is used as a signal amplifier. Erbium also has some uses in the nuclear power industry.

Erbia, the renamed material that Mosander discovered in 1843, is erbium oxide (Er2O3), one of erbium's compounds. Erbia has a pink color and is used to color glass and glazes. Other erbium compounds include: erbium fluoride (ErF3, erbium chloride (ErCl3 and erbium iodide (ErI3).

Erbium is finding nuclear and metallurgical uses. Added to vanadium, for example, erbium lowers the hardness and improves workability. Erbium oxide gives a pink color and has been used as a colorant in glasses and porcelain enamel glazes.

Compounds

See more information at the Erbium compound page.

Element Forms

CID Name Formula SMILES Molecular Weight
23980 erbium Er [Er] 167.26
3779597 erbium(3+) Er+3 [Er+3] 167.26
161153 erbium-169 Er [169Er] 168.934598
177431 erbium-171 Er [171Er] 170.93804
177481 erbium-168 Er [168Er] 167.932378
177526 erbium-161 Er [161Er] 160.93000
177635 erbium-170 Er [170Er] 169.93547
178160 erbium-165 Er [165Er] 164.930733
177497 erbium-166 Er [166Er] 165.930301
177697 erbium-172 Er [172Er] 171.93936
131708394 erbium-162 Er [162Er] 161.928787
131708395 erbium-164 Er [164Er] 163.929208
131708396 erbium-167 Er [167Er] 166.932056

Isotopes

Stable Isotope Count 6

Isotopes in Biology

Radiolabeled 171Er (with a half-life of 7.5 h) tablets have been used to study bowel movements of individuals using external scintigraphy. Such tablets have an enteric coating and contain small amounts of stable erbium oxide (170Er) initially. The tablets are then irradiated at a low neutron flux to produce radioactively labeled 171Er tablets, via the 170Er (n, γ) 171Er reaction. This method is a noninvasive approach for determining gastric emptying rates and visualizing segments of the digestive system in an individual [479], [480].

[479] A. Parr, R. M. Beihn, M. Jay. Int. J. Pharm.32, 251 (1986).
[480] M. C. Theodorakis. Am. Physiol. Soc. Gastrointest. Liver Physiol.239, G39 (1980).

Isotopes in Medicine

169Er (with a half-life of 9.4 days) is used in radiosynovectomy, which is a regularly practiced radiotherapy, on rheumatoid arthritis patients whose condition is resistant to standard methods of treatment (Fig. IUPAC.68.1). Rheumatoid arthritis is a chronic, inflammatory, autoimmune disease of the joint capsule (synovial sac), which is lined with a thin membrane called the synovium, of an individual’s moveable joints (synovial joints). In radiosynovectomy, the radiopharmaceutical called 169Er- citrate colloid, which contains colloidal particles that are labeled with β-emitting 169Er, is directly injected into the synovial cavity (the cavity between the bones in a moveable joint inside of the synovium) of the affected joint. These radioactive-colloid particles are then phagocytized (engulfed) by macrophage-like synoviocytes as well as other phagocytizing inflammatory cells in the patient’s synovium. Necrosis (tissue death) and the inhabitation of cell proliferation (increase in number of cells) result from the radiation of the synovium and therefore, temporarily halts synovitis (which is the condition of when the synovium thickens with inflammation) and improves synovial joint function [481], [482], [483], [484].

Fig. IUPAC.68.1: Normal joint (top) vs. joint affected by rheumatoid arthritis (bottom) (modified from [485]).

[481] F. M. van der Zanta, Z. N. Jahangierb, G. G. M. Gommansa, J. D. Moolenburghc, J. W. G. Jacobs. Appl. Radiat. Isot.65, 649 (2007).
[482] S. J. Kim, K. A. Jung. Clin. Med. Res.5, 244 (2007).
[483] M. E. A. McNeil. The First Year Rheumatoid Arthritis: An Essential Guide for the Newly Diagnosed, Marlowe & Company, New York, NY (2005).
[484] G. Prabhakar, S. S. Sachdev, N. Sivaprasad. Pharma Times41, 11 (2009).
[485] National Institute of Arthritis and Musculoskeletal and Skin Diseases. Normal Joint Versus Joint Affected by Rheumatoid Arthritis.

Isotope Mass and Abundance

Isotope Atomic Mass (uncertainty) [u] Abundance (uncertainty)
162Er 161.928 787(6) 0.001 39(5) 0.00139(5)
164Er 163.929 207(5) 0.016 01(3) 0.01601(3)
166Er 165.930 299(8) 0.335 03(36) 0.33503(36)
167Er 166.932 054(8) 0.228 69(9) 0.22869(9)
168Er 167.932 376(8) 0.269 78(18) 0.26978(18)
170Er 169.935 47(1) 0.149 10(36) 0.14910(36)

Atomic Mass, Half Life, and Decay

Nuclide Atomic Mass and Uncertainty [u] Half Life and Uncertainty Discovery Year Decay Modes, Intensities and Uncertainties [%]
142Er 141.970016 ± 0.000537 [Estimated] 10 us [Estimated] p ?
143Er 142.966548 ± 0.000429 [Estimated] 200 ms [Estimated] 2005 β+ ?; β+p ?
144Er 143.960700 ± 0.00021 [Estimated] 400 ms >200ns [Estimated] 2003 β+ ?
145Er 144.957874 ± 0.000215 [Estimated] 900 ms ± 200 1989 β+=100%; β+p=?
145Erm 144.957874 ± 0.000215 [Estimated] 1.0 s ± 0.3 2010 β+=100%; IT ?; β+p=?
146Er 145.952418357 ± 0.000007197 1.7 s ± 0.6 1993 β+=100%; β+p=?
147Er 146.949964456 ± 0.000041 3.2 s ± 1.2 1992 β+=100%; β+p=?
147Erm 146.949964456 ± 0.000041 1.6 s ± 0.2 1982 β+=100%; β+p=?
148Er 147.944735026 ± 0.000011 4.6 s ± 0.2 1982 β+=100%; β+p≈0.15%
148Erm 147.944735026 ± 0.000011 13 us ± 3 1982 IT=100%
149Er 148.942306000 ± 0.00003 4 s ± 2 1984 β+=100%; β+p=7±0.2%
149Erm 148.942306000 ± 0.00003 8.9 s ± 0.2 1984 β+=96.5±0.7%; IT=3.5±0.7%; β+p=0.18±0.7%
149Ern 148.942306000 ± 0.00003 610 ns ± 80 1987 IT=100%
149Erp 148.942306000 ± 0.00003 4.8 us ± 0.1 1987 IT=100%
150Er 149.937915524 ± 0.000018458 18.5 s ± 0.7 1982 β+=100%
150Erm 149.937915524 ± 0.000018458 2.55 us ± 0.10 1984 IT=100%
151Er 150.937448567 ± 0.000017681 23.5 s ± 2.0 1970 β+=100%
151Erm 150.937448567 ± 0.000017681 580 ms ± 20 1980 IT=95.3±0.3%; β+=4.7±0.3%
151Ern 150.937448567 ± 0.000017681 420 ns ± 50 1990 IT=100%
152Er 151.935050347 ± 0.000009478 10.3 s ± 0.1 1963 α=90±0.4%; β+=10±0.4%
153Er 152.935086350 ± 0.000009967 37.1 s ± 0.2 1963 α=53±0.3%; β+=47±0.3%
153Erm 152.935086350 ± 0.000009967 373 ns ± 9 1979 IT=100%
153Ern 152.935086350 ± 0.000009967 248 ns ± 32 1979 IT=100%
154Er 153.932790799 ± 0.000005325 3.73 m ± 0.09 1963 β+≈100%; α=0.47±1.3%
155Er 154.933215710 ± 0.00000652 5.3 m ± 0.3 1969 β+=99.978±0.7%; α=0.022±0.7%
156Er 155.931065926 ± 0.00002644 19.5 m ± 1.0 1967 β+=100%; α=1.2e-5±0.3%
157Er 156.931922652 ± 0.000028454 18.65 m ± 0.10 1966 β+=100%
157Erm 156.931922652 ± 0.000028454 76 ms ± 6 1971 IT=100%
158Er 157.929893474 ± 0.000027074 2.29 h ± 0.06 1961 ε=100%
159Er 158.930690790 ± 0.00000391 36 m ± 1 1962 β+=100%
159Erm 158.930690790 ± 0.00000391 337 ns ± 14 1971 IT=100%
159Ern 158.930690790 ± 0.00000391 590 ns ± 60 1971 IT=100%
160Er 159.929077193 ± 0.000026029 28.58 h ± 0.09 1954 ε=100%
161Er 160.930003530 ± 0.000009419 3.21 h ± 0.03 1954 β+=100%
161Erm 160.930003530 ± 0.000009419 7.5 us ± 0.7 1969 IT=100%
162Er 161.928787299 ± 0.000000811 Stable >140Ty 1938 IS=0.139±0.5%; α ?; 2β+ ?
162Erm 161.928787299 ± 0.000000811 88 ns ± 16 1974 IT=100%
163Er 162.930039908 ± 0.000004967 75.0 m ± 0.4 1953 β+=100%
163Erm 162.930039908 ± 0.000004967 580 ns ± 100 1974 IT=100%
164Er 163.929207739 ± 0.000000755 Stable 1938 IS=1.601±0.3%; α ?; 2β+ ?
165Er 164.930733482 ± 0.000000985 10.36 h ± 0.04 1950 ε=100%
165Erm 164.930733482 ± 0.000000985 250 ns ± 30 1970 IT=100%
165Ern 164.930733482 ± 0.000000985 370 ns ± 40 2012 IT=100%
166Er 165.930301067 ± 0.000000358 Stable 1934 IS=33.503±3.6%
167Er 166.932056192 ± 0.000000306 Stable 1934 IS=22.869±0.9%
167Erm 166.932056192 ± 0.000000306 2.269 s ± 0.006 1986 IT=100%
168Er 167.932378282 ± 0.00000028 Stable 1934 IS=26.978±1.8%
168Erm 167.932378282 ± 0.00000028 109.0 ns ± 0.7 1974 IT=100%
169Er 168.934598444 ± 0.000000326 9.392 d ± 0.018 1956 β-=100%
169Erm 168.934598444 ± 0.000000326 285 ns ± 20 1969 IT=100%
169Ern 168.934598444 ± 0.000000326 200 ns ± 10 1969 IT=100%
170Er 169.935471933 ± 0.000001488 Stable >410Py 1934 IS=14.910±3.6%; 2β- ?; α ?
171Er 170.938037372 ± 0.000001511 7.516 h ± 0.002 1938 β-=100%
171Erm 170.938037372 ± 0.000001511 210 ns ± 10 1969 IT=100%
172Er 171.939363461 ± 0.000004253 49.3 h ± 0.5 1956 β-=100%
172Erm 171.939363461 ± 0.000004253 579 ns ± 62 2006 IT=100%
173Er 172.942400 ± 0.00021 [Estimated] 1.434 m ± 0.017 1972 β-=100%
174Er 173.944230 ± 0.00032 [Estimated] 3.2 m ± 0.2 1989 β-=100%
174Erm 173.944230 ± 0.00032 [Estimated] 3.9 s ± 0.3 2006 IT=100%
175Er 174.947770 ± 0.00043 [Estimated] 1.2 m ± 0.3 1996 β-=100%
176Er 175.949940 ± 0.00043 [Estimated] 12 s >300ns [Estimated] 2012 β- ?
177Er 176.953990 ± 0.00054 [Estimated] 8 s >300ns [Estimated] 2012 β- ?
178Er 177.956779 ± 0.00064 [Estimated] 4 s >300ns [Estimated] 2012 β- ?
179Er 178.961267 ± 0.000537 [Estimated] 3 s >550ns [Estimated] 2018 β- ?; β-n ?
180Er 179.964380 ± 0.000537 [Estimated] 2 s >550ns [Estimated] 2018 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
    Erbium

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