71
Lu
Lutetium
Atomic Mass 174.9668
Electron Configuration [Xe]6s24f145d1
Oxidation States +3
Year Discovered 1907

Identifiers

Element Name Lutetium
Element Symbol Lu
InChI InChI=1S/Lu
InChIKey OHSVLFRHMCKCQY-UHFFFAOYSA-N

Properties

Atomic Weight

174.966 69(5)

174.9668

175.0

174.9668(1)

Electron Configuration

[Xe]6s24f145d1

Atomic Radius

Van der Waals Atomic Radius : 221 pm (Van der Waals)

Empirical Atomic Radius : 175pm (Empirical)

Covalent Atomic Radius : 187(8) pm (Covalent)

Oxidation States

+3

3, 2, 1 ​(a weakly basic oxide)

Ground Level

2D3/2

Ionization Energy

5.426 eV

5.425871 ± 0.000012 eV

Electronegativity

Pauling Scale Electronegativity : 1.27(Pauling Scale)

Allen Scale Electronegativity : 1.09(Allen Scale)

Atomic Spectra

Lines Holdings

Levels Holdings

Physical Description

Solid

Element Classification

Metal

Element Period Number

6

Element Group Number

3 - Lanthanide

Density

9.84 grams per cubic centimeter

Melting Point

1936 K (1663°C or 3025°F)

1652°C

Boiling Point

3675 K (3402°C or 6156°F)

3402°C

Estimated Crustal Abundance

8×10-1 milligrams per kilogram

Estimated Oceanic Abundance

1.5×10-7 milligrams per liter

History

The name derives from Lutetia, the ancient name for the city of Paris. The discovery of lutetium is credited to the French chemist Georges Urbain in 1907 although it had been separated earlier and independently by the Austrian chemist Carl Auer (Baron von Welsbach) from an ytterbium sample.

Von Welsbach had named the element cassiopeium after the constellation Cassiopeia. However, because Urbain published his results before Auer, his name for the element was adopted by IUPAC in 1949.

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. In 1878 Jean Charles Galissard de Marignac, a Swiss chemist, discovered that erbia was itself composed of two components. One component was named ytterbia by Marignac while the other component retained the name erbia. Marignac believed that ytterbia was a compound of a new element, which he named ytterbium. Other chemists produced and experimented with ytterbium in an attempt to determine some of it's properties. Unfortunately, different scientists obtained different results from the same experiments. While some scientists believed that these inconsistent results were caused by poor procedures or faulty equipment, Georges Urbain, a French chemist, believed that ytterbium wasn't an element at all, but a mixture of two elements. In 1907, Urbain was able to separate ytterbium into two elements. Urbain named one of the elements neoytterbium (new ytterbium) and the other element lutecium. Carl Auer von Welsbach, an Austrian chemist working independently of Urbain, reached the same conclusions at nearly the same time. Welsbach chose the names albebaranium and cassiopium for these elements. Urbain was eventually credited with the discovery of the elements and won the right to name them, although chemists later changed the name neoytterbium back to ytterbium and changed the spelling of lutecium to lutetium. Today, lutetium is primarily obtained through an ion exchange process from monazite sand ((Ce, La, Th, Nd, Y)PO4), a material rich in rare earth elements.

Lutetia is the ancient name for Paris. In 1907, Urbain described a process by which Marignac's ytterbium (1879) could be separated into the two elements, ytterbium (neoytterbium) and lutetium. These elements were identical with "aldebaranium" and "cassiopeium," independently discovered at this time. The spelling of the element was changed from lutecium to lutetium in 1949.

Historical Atomic Weights

Year Atomic Weight (uncertainty) [u] Reference
2024 174.966 69(5)
2007 174.9668(1) https://doi.org/10.1351/PAC-REP-09-08-03
1981 174.967(1) https://doi.org/10.1351/pac198355071101
1977 174.967(3) https://doi.org/10.1351/pac197951020405
1969 174.97(1) https://doi.org/10.1351/pac197021010091
1961 174.97 https://doi.org/10.1021/ja00881a001
1940 174.99 https://doi.org/10.1039/JR9400000475
1916 175.0 https://doi.org/10.1021/ja02176a001
1909 174.0 https://doi.org/10.1021/ja01931a001

Historical Isotopic Abundances

Year Isotope Abundance (uncertainty) Reference
2024 175Lu 0.974 14(5)
2024 176Lu 0.025 86(5)
2009 175Lu 0.974 01(13) https://doi.org/10.1351/PAC-REP-10-06-02
2009 176Lu 0.025 99(13) https://doi.org/10.1351/PAC-REP-10-06-02
1983 175Lu 0.9741(2) https://doi.org/10.1351/pac198456060675
1983 176Lu 0.0259(2) https://doi.org/10.1351/pac198456060675
1979 175Lu 0.9739(2) https://doi.org/10.1351/pac198052102349
1979 176Lu 0.0261(2) https://doi.org/10.1351/pac198052102349
1975 175Lu 0.974 https://doi.org/10.1351/pac197647010075
1975 176Lu 0.026 https://doi.org/10.1351/pac197647010075

Description

Lutetium occurs in very small amounts in nearly all minerals containing yttrium, and is present in monazite to the extent of about 0.003%, which is a commercial source. The pure metal has been isolated only in recent years and is one of the most difficult to prepare. It can be prepared by the reduction of anhydrous LuCl3 or LuF3 by an alkali or alkaline earth metal. The metal is silvery white and relatively stable in air. 176Lu occurs naturally (2.6%) with 175Lu (97.4%). It is radioactive with a half-life of about 3 x 1010 years.

Users

Lutetium is one of the most difficult elements to prepare and has no large scale practical uses, although some of its radioactive isotopes can be used as a catalyst in the cracking of petroleum products and a catalyst in some hydrogenation and polymerization processes.

Stable lutetium nuclides, which emit pure beta radiation after thermal neutron activation, can be used as catalysts in cracking, alkylation, hydrogenation, and polymerization. Virtually no other commercial uses have been found yet for lutetium.

Compounds

See more information at the Lutetium compound page.

Element Forms

CID Name Formula SMILES Molecular Weight
23929 lutetium Lu [Lu] 174.9667
185495 lutetium(3+) Lu+3 [Lu+3] 174.9667
161046 lutetium-177 Lu [177Lu] 176.94376
167100 lutetium-176 Lu [176Lu] 175.94269
167366 lutetium-171 Lu [171Lu] 170.93792
177502 lutetium-174 Lu [174Lu] 173.94034
177657 lutetium-170 Lu [170Lu] 169.9385
178165 lutetium-172 Lu [172Lu] 171.93909
46829796 lutetium-177(3+) Lu+3 [177Lu+3] 176.94376
167377 lutetium-179 Lu [179Lu] 178.94733
177429 lutetium-173 Lu [173Lu] 172.93894
177449 lutetium-178 Lu [178Lu] 177.94596
177642 lutetium-169 Lu [169Lu] 168.93765
9898892 lutetium-157 Lu [157Lu] 156.9501

Handling And Storage

While lutetium, like other rare-earth metals, is thought to have a low toxicity rating, it should be handled with care until more information is available.

Isotopes

Stable Isotope Count 1

Isotopes in Biology

176Lu (with a half-life of 3.73×1010 years) is used in labeling experiments to quantify absolute protein abundance (absolute quantities of proteins in a cell) and examine the extent of synthesis of proteins under specific biological conditions [500]. 175Lu has been used as a yield tracer in inductively coupled plasma mass spectrometry (ICP-MS) determination of plutonium in urine [500].

[500] C. Rappel, D. Schaumloöffel. Anal. Chem.81, 385 (2009).

Isotopes in Medicine

177Lu (with a half-life of 160 h) has potential for use as an isotope for radioimmunotherapy for the treatment of small, soft tumors and for imaging purposes (Fig. IUPAC.71.1) [501].

Fig. IUPAC.71.1: Bone scan (on left) and ¹⁷⁷Lu scan (on right) done 10 days apart on a patient with prostate cancer (PC), which metastasized to his bones, and who is being treated with the experimental drug ¹⁷⁷lutetium-labeled J591 (¹⁷⁷Lu-J591). The primary areas of uptake of this drug in the body are in PC metastases, which appear as small dark spots in both sets of scans, and in the liver (the large dark spot in the ¹⁷⁷Lu scans). The location and number of metastases is clearer in the ¹⁷⁷Lu scan than in the bone scan. (Image Source: Bander, Milowsky, Nanus, Kostakoglu, Vallabhajosula and Goldsmith, 2005, © American Society of Clinical Oncology. All rights reserved.) [501].

[501] N. H. Bander, M. I. Milowsky, D. M. Nanus, L. Kostakoglu, S. Vallabhajosula, S. J. Goldsmith. J. Clin. Oncol.23, 4591 (2005).

Isotope Mass and Abundance

Isotope Atomic Mass (uncertainty) [u] Abundance (uncertainty)
175Lu 174.940 777(8) 0.974 14(5)
176Lu 175.942 692(8) 0.025 86(5)
Isotope Atomic Mass (uncertainty) [u] Abundance (uncertainty)
175Lu 174.9407752(20) 0.97401(13)
176Lu 175.9426897(20) 0.02599(13)

Atomic Mass, Half Life, and Decay

Nuclide Atomic Mass and Uncertainty [u] Half Life and Uncertainty Discovery Year Decay Modes, Intensities and Uncertainties [%]
150Lu 149.973407 ± 0.000322 [Estimated] 45 ms ± 3 1993 p≈100%; β+ ?
150Lum 149.973407 ± 0.000322 [Estimated] 40 us ± 7 1998 p=100%
151Lu 150.967471 ± 0.000322 [Estimated] 78.4 ms ± 0.9 1982 p=?; β+=?
151Lum 150.967471 ± 0.000322 [Estimated] 16.0 us ± 0.5 1998 p=100%
152Lu 151.964120 ± 0.00021 [Estimated] 650 ms ± 70 1987 β+=100%; β+p=15±0.7%
153Lu 152.958802248 ± 0.00016105 900 ms ± 200 1989 α=?; β+ ?; p=0%
153Lum 152.958802248 ± 0.00016105 1 s [Estimated] 1997 α ?; β+ ?; IT ?; p=0%
153Lun 152.958802248 ± 0.00016105 >100 ns 1993 IT=100%
153Lup 152.958802248 ± 0.00016105 15 us ± 3 1993 IT=100%
154Lu 153.957416 ± 0.000216 [Estimated] 1 s [Estimated] 1981 β+ ?; α ?
154Lum 153.957416 ± 0.000216 [Estimated] 1.12 s ± 0.08 1981 β+≈100%; β+p=?; β+α=?; α ?
154Lun 153.957416 ± 0.000216 [Estimated] 35 us ± 3 1990 IT=100%
155Lu 154.954326005 ± 0.00002066 68 ms ± 2 1965 α=90±0.2%; β+=10±0.2%
155Lum 154.954326005 ± 0.00002066 138 ms ± 9 1967 α=76±1.6%; β+=24±1.6%
155Lun 154.954326005 ± 0.00002066 2.69 ms ± 0.03 1981 α≈100%; IT ?
156Lu 155.953086606 ± 0.000058102 494 ms ± 12 1965 α=100%; β+ ?
156Lum 155.953086606 ± 0.000058102 198 ms ± 2 1979 α≈100%; β+ ?
156Lun 155.953086606 ± 0.000058102 179 ns ± 4 2018 IT=100%
157Lu 156.950144807 ± 0.000012961 7.7 s ± 2.0 1977 β+ ?; α=?
157Lum 156.950144807 ± 0.000012961 4.79 s ± 0.12 1972 β+=92.3±1.9%; α=7.7±1.9%
158Lu 157.949315620 ± 0.000016236 10.6 s ± 0.3 1979 β+=99.09±2%; α=0.91±2%
159Lu 158.946635615 ± 0.000040433 12.1 s ± 1.0 1980 β+≈100%; α= ?
159Lum 158.946635615 ± 0.000040433 10 s [Estimated] β+ ?; IT ?; α ?
160Lu 159.946033000 ± 0.000061 36.1 s ± 0.3 1979 β+=100%; α ?
160Lum 159.946033000 ± 0.000061 40 s ± 1 1980 β+≈100%; α ?
161Lu 160.943572000 ± 0.00003 77 s ± 2 1973 β+=100%
161Lum 160.943572000 ± 0.00003 7.3 ms ± 0.4 1973 IT≈100%; β+ ?
162Lu 161.943282776 ± 0.000080554 1.37 m ± 0.02 1978 β+=100%
162Lum 161.943282776 ± 0.000080554 1.5 m 1980 β+≈100%; IT ?
162Lun 161.943282776 ± 0.000080554 1.9 m 1980 β+ ?; IT ?
163Lu 162.941179000 ± 0.00003 3.97 m ± 0.13 1979 β+=100%
164Lu 163.941339000 ± 0.00003 3.14 m ± 0.03 1977 β+=100%
165Lu 164.939406758 ± 0.00002849 10.74 m ± 0.10 1973 β+=100%
166Lu 165.939859000 ± 0.000032 2.65 m ± 0.10 1969 β+=100%
166Lum 165.939859000 ± 0.000032 1.41 m ± 0.10 1974 β+=58±0.5%; IT=42±0.5%
166Lun 165.939859000 ± 0.000032 2.12 m ± 0.10 1974 β+=90±0.6%; IT ?
167Lu 166.938243000 ± 0.00004 51.5 m ± 1.0 1958 β+=100%
167Lum 166.938243000 ± 0.00004 >1 m 1998 IT ?; β+ ?
168Lu 167.938729798 ± 0.000040766 5.5 m ± 0.1 1960 β+=100%
168Lum 167.938729798 ± 0.000040766 6.7 m ± 0.4 1960 β+≈100%; IT ?
169Lu 168.937645845 ± 0.000003226 34.06 h ± 0.05 1955 β+=100%
169Lum 168.937645845 ± 0.000003226 160 s ± 10 1965 IT=100%
170Lu 169.938479230 ± 0.000018081 2.012 d ± 0.030 1951 β+=100%
170Lum 169.938479230 ± 0.000018081 670 ms ± 100 1965 IT=100%
171Lu 170.937918591 ± 0.000001999 8.247 d ± 0.023 1951 β+=100%
171Lum 170.937918591 ± 0.000001999 79 s ± 2 1965 IT=100%
172Lu 171.939091320 ± 0.000002507 6.70 d ± 0.03 1951 β+=100%
172Lum 171.939091320 ± 0.000002507 3.7 m ± 0.5 1962 IT=100%; β+ ?
172Lun 171.939091320 ± 0.000002507 332 ns ± 20 1965 IT=100%
172Lup 171.939091320 ± 0.000002507 440 us ± 12 1965 IT=100%
172Luq 171.939091320 ± 0.000002507 150 ns 1974 IT=100%
173Lu 172.938935722 ± 0.000001682 1.37 y ± 0.01 1951 ε=100%
173Lum 172.938935722 ± 0.000001682 74.2 us ± 1.0 1962 IT=100%
174Lu 173.940342840 ± 0.000001682 3.31 y ± 0.05 1951 β+=100%
174Lum 173.940342840 ± 0.000001682 142 d ± 2 1960 IT=99.38±0.2%; ε=0.62±0.2%
174Lun 173.940342840 ± 0.000001682 395 ns ± 15 1980 IT=100%
174Lup 173.940342840 ± 0.000001682 145 ns ± 3 1980 IT=100%
174Luq 173.940342840 ± 0.000001682 194 ns ± 24 2009 IT=100%
174Lur 173.940342840 ± 0.000001682 97 ns ± 10 2009 IT=100%
174Lux 173.940342840 ± 0.000001682 242 ns ± 19 2009 IT=100%
175Lu 174.940777211 ± 0.000001295 Stable 1934 IS=97.401±1.3%
175Lum 174.940777211 ± 0.000001295 1.49 us ± 0.07 1965 IT=100%
175Lun 174.940777211 ± 0.000001295 984 us ± 30 1998 IT=100%
176Lu 175.942691711 ± 0.000001301 37.01 Gy ± 0.17 1935 IS=2.599±1.3%; β-=100%; β+=0.45±2.6%
176Lum 175.942691711 ± 0.000001301 3.664 h ± 0.019 1935 β-≈100%; ε=0.095±1.6%
176Lun 175.942691711 ± 0.000001301 312 ns ± 69 2000 IT=100%
176Lup 175.942691711 ± 0.000001301 40 us ± 3 2000 IT=100%
177Lu 176.943763570 ± 0.00000131 6.6443 d ± 0.0009 1945 β-=100%
177Lum 176.943763570 ± 0.00000131 130.1 ns ± 2.4 1949 IT=100%
177Lun 176.943763570 ± 0.00000131 155 us ± 7 1965 IT=100%
177Lup 176.943763570 ± 0.00000131 160.4 d ± 0.3 1962 β-=77.30±0.8%; IT=22.70±0.8%
177Luq 176.943763570 ± 0.00000131 625 ns ± 62 2004 IT=100%
177Lur 176.943763570 ± 0.00000131 6 us ± 2 2003 IT=100%
178Lu 177.945960065 ± 0.000002416 28.4 m ± 0.2 1957 β-=100%
178Lum 177.945960065 ± 0.000002416 23.1 m ± 0.3 1951 β-=100%
179Lu 178.947332985 ± 0.000005528 4.59 h ± 0.06 1961 β-=100%
179Lum 178.947332985 ± 0.000005528 3.1 ms ± 0.9 1982 IT=100%
180Lu 179.949890744 ± 0.000075926 5.7 m ± 0.1 1971 β-=100%
180Lum 179.949890744 ± 0.000075926 ~1 s 1995 IT ?; β- ?
180Lun 179.949890744 ± 0.000075926 >1 ms 2001 IT=100%
181Lu 180.951908000 ± 0.000135 3.5 m ± 0.3 1982 β-=100%
182Lu 181.955158 ± 0.000215 [Estimated] 2.0 m ± 0.2 1982 β-=100%
183Lu 182.957363000 ± 0.000086 58 s ± 4 1983 β-=100%
184Lu 183.961030 ± 0.000215 [Estimated] 20 s ± 3 1989 β-=100%
185Lu 184.963542 ± 0.000322 [Estimated] 20 s >300ns [Estimated] 2009 β- ?
186Lu 185.967450 ± 0.000429 [Estimated] 6 s >300ns [Estimated] 2012 β- ?; β-n ?
187Lu 186.970188 ± 0.000429 [Estimated] 7 s >300ns [Estimated] 2012 β- ?
188Lu 187.974428 ± 0.000429 [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
    Lutetium

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