Lutetium (Lu)
lanthanideSolid
標準原子量
174.9668 u電子配置
[Xe] 6s2 4f14 5d1融点
1662.85 °C沸点
3401.85 °C密度
9840 kg/m³酸化数
0, +1, +2, +3電気陰性度(Pauling)
1.27第1イオン化エネルギー
5.425871 eV発見年
1907原子半径
175 pm詳細
Lutetium is a dense, silvery lanthanide and the last element of the 4f series. In chemistry it is almost exclusively trivalent, with a filled 4f shell in Lu³⁺ and a relatively small ionic radius compared with other lanthanides. It occurs with the rare-earth elements in minerals such as monazite and xenotime, but is one of the least abundant lanthanides. Its main technological value lies in specialized scintillators, catalysts, and medical radioisotopes rather than in bulk structural use.
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.
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.
Pure lutetium is a bright silvery metal that tarnishes slowly in air. It is relatively hard and dense for a lanthanide, and can be cut or machined as a reactive metal under suitable conditions. Macroscopic metal is available, but usually only in small quantities because separation is costly.
The largest practical uses of lutetium are specialized. Lutetium oxyorthosilicate, Lu₂SiO₅, and related cerium-doped crystals are important scintillators in positron emission tomography and other radiation detectors. Lutetium compounds are used as catalysts or catalyst supports in some petroleum refining and organic reactions. The radioisotope ¹⁷⁷Lu is used in targeted radiopharmaceutical therapy, where its beta emission and accompanying gamma rays are useful for treatment and imaging dosimetry. Metallic lutetium itself has few direct applications.
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.
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] C. Rappel, D. Schaumloöffel. Anal. Chem.81, 385 (2009).. 175Lu has been used as a yield tracer in inductively coupled plasma mass spectrometry (ICP-MS) determination of plutonium in urine [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] N. H. Bander, M. I. Milowsky, D. M. Nanus, L. Kostakoglu, S. Vallabhajosula, S. J. Goldsmith. J. Clin. Oncol.23, 4591 (2005)..
Lutetium chemistry is dominated by the +3 oxidation state. Common compounds include lutetium oxide, Lu₂O₃, a refractory sesquioxide; lutetium chloride, LuCl₃; lutetium fluoride, LuF₃; and lutetium nitrate, Lu(NO₃)₃. Lu³⁺ forms colorless or weakly colored salts because the 4f shell is filled and gives little visible absorption. Organometallic and coordination compounds are known, including cyclopentadienyl complexes, but they are mainly used in research or as specialized catalysts. Stable lower oxidation states are not characteristic under ordinary conditions.
See more information at the Lutetium compound page.
Lutetium metal dust can present fire and irritation hazards typical of reactive rare-earth metals. Soluble lutetium salts should be handled as toxic laboratory chemicals, although lutetium has no known biological role and its ordinary compounds are not among the most acutely hazardous rare-earth salts. The main isotope-specific hazard is radiological: ¹⁷⁷Lu and other radioactive isotopes require shielding, contamination control, and regulated handling. Stable natural lutetium is not significantly radioactive for practical purposes, despite containing long-lived ¹⁷⁶Lu.
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.
Lutetium is dispersed in the crust with other heavy rare-earth elements and is concentrated only weakly by normal geological processes. It is released from minerals mainly through weathering or mining and processing of rare-earth ores. In natural waters Lu³⁺ is strongly complexed, adsorbed to particles, or incorporated into sediments, so dissolved concentrations are very low. It has no recognized biological function, and ecological effects are chiefly a concern near rare-earth mining, refining, or waste streams.
Lutetium is obtained as a minor component during separation of mixed rare-earth concentrates, especially from xenotime, ion-adsorption clays, and some monazite-derived streams. Its supply is constrained less by absolute geological scarcity than by the difficulty of separating adjacent lanthanides with very similar chemistry and by the limited volume of heavy rare-earth processing. Demand is modest but high-value, led by scintillator materials, research chemicals, catalysts, and medical isotope production chains. Recycling is limited and mostly tied to recovery from specialized crystals or process residues rather than broad consumer products.
Found with ytterbium in gadolinite and xenotime. Usually obtained from monazite sand which is ofter 50% rare earth by weight and 0.003% lutetium.
Lutetium is a rare heavy element in cosmic terms. Its stable isotope ¹⁷⁵Lu and long-lived ¹⁷⁶Lu are produced by neutron-capture processes in evolved stars and supernova-related environments, with details depending on s-process and r-process histories. In planetary materials it follows lithophile rare-earth behavior and is useful in isotope geochemistry, especially through the ¹⁷⁶Lu–¹⁷⁶Hf decay system.
- Lutetium was the last naturally occurring lanthanide to be identified as a separate element.
- The name derives from Lutetia, the Latin name for Paris.
- Lu³⁺ is the smallest common trivalent lanthanide ion.
- Natural lutetium is mostly ¹⁷⁵Lu, with a small fraction of long-lived ¹⁷⁶Lu.
- The ¹⁷⁶Lu–¹⁷⁶Hf system is used to date rocks and study mantle evolution.
- Lutetium is often placed under yttrium in periodic tables, but its group placement has been historically debated.
画像
性質
物理的性質
- 原子半径(経験値)
- 175 pm 全元素の原子半径(経験値)を比較 →
- 共有結合半径
- 187 pm 全元素の共有結合半径を比較 →
- ファンデルワールス半径
- 221 pm 全元素のファンデルワールス半径を比較 →
- 密度
- 9840 kg/m³ 全元素の密度を比較 →
- モル体積
- 0.0178 L/mol
- 標準温度・圧力(STP)での相
- 固体 全元素の標準温度・圧力(STP)での相を比較 →
- 融点
- 1662.85 °C 全元素の融点を比較 →
- 沸点
- 3401.85 °C 全元素の沸点を比較 →
- 比熱容量
- 0.154 J/(g·K) 全元素の比熱容量を比較 →
- モル熱容量
- 26.86 J/(mol·K) 全元素のモル熱容量を比較 →
- 結晶構造
- 六方最密充填構造 全元素の結晶構造を比較 →
化学的性質
- 電気陰性度(Pauling)
- 1.27 全元素の電気陰性度(Pauling)を比較 →
- 電気陰性度(Allen)
- 1.09
- 電子親和力
- 0.346 eV
- 第1イオン化エネルギー
- 5.425871 eV 全元素の第1イオン化エネルギーを比較 →
- 第2イオン化エネルギー
- 14.130049 eV 全元素の第2イオン化エネルギーを比較 →
- 第3イオン化エネルギー
- 20.959472 eV 全元素の第3イオン化エネルギーを比較 →
- 第4イオン化エネルギー
- 45.249156 eV 全元素の第4イオン化エネルギーを比較 →
- 第5イオン化エネルギー
- 66.80023 eV 全元素の第5イオン化エネルギーを比較 →
- 酸化数
- 0, +1, +2, +3 全元素の酸化数を比較 →
- 価電子
- 3 全元素の価電子を比較 →
- 電子配置
- [Xe] 6s2 4f14 5d1
熱力学的性質
- 融解熱
- 0.18759393 eV 全元素の融解熱を比較 →
- 蒸発熱
- 3.679328 eV 全元素の蒸発熱を比較 →
- 昇華熱
- 4.435923 eV
- 原子化熱
- 4.435923 eV
- 原子化エンタルピー
- 4.431777 eV
原子核
- 陽子数
- 71 全元素の陽子数を比較 →
- 中性子数
- 104 全元素の中性子数を比較 →
- 既知の同位体
- 39 全元素の既知の同位体を比較 →
- 安定同位体
- 1 全元素の安定同位体を比較 →
- 最も安定な同位体
- Lu-175
- 発見年
- 1907
存在度
- 存在度(地殻)
- 0.8 mg/kg 全元素の存在度(地殻)を比較 →
- 存在度(海洋)
- 1.5 × 10−7 mg/L 全元素の存在度(海洋)を比較 →
結晶構造
- 格子定数a
- 351 pm
電子構造
- 各電子殻の電子数
- 2, 8, 18, 32, 9, 2 全元素の各電子殻の電子数を比較 →
識別子
- CAS登録番号
- 7439-94-3 全元素のCAS登録番号を比較 →
- 項記号
- 2D3/2
- InChI
- InChI=1S/Lu
- InChI Key
- OHSVLFRHMCKCQY-UHFFFAOYSA-N
電子配置 測定値
Lu: 4f¹⁴ 5d¹ 6s²[Xe] 4f¹⁴ 5d¹ 6s²1s² 2s² 2p⁶ 3s² 3p⁶ 3d¹⁰ 4s² 4p⁶ 4d¹⁰ 5s² 5p⁶ 4f¹⁴ 5d¹ 6s²原子モデル
同位体によって中性子数、質量、安定性は変わりますが、中性原子の電子配置は変わりません。
模式的な原子モデルです。実際の縮尺とは異なります。
原子の指紋
発光/吸収スペクトル
同位体分布
| 質量数 | 原子質量(u) | 天然存在比 | 半減期 |
|---|---|---|---|
| 175 安定 | 174.9407752 ± 0.000002 | 97.4010% | 安定 |
相/状態
理由: 融点(1662.85 °C)より1637.8 °C低い
模式図、実際の縮尺とは異なります
相転移点
相転移エネルギー
融点で1 molを融解させるのに必要なエネルギー
沸点で1 molを蒸発させるのに必要なエネルギー
昇華点で1 molを昇華させるのに必要なエネルギー
密度
標準条件下
標準条件下
原子スペクトル
全71件中10件を表示しています。 イオンの電荷の昇順で並べています。
スペクトル線データの収録状況 ?
| イオン | 電荷 | スペクトル線の総数 | 遷移確率 | 準位の表記 |
|---|---|---|---|---|
| Lu I | 0 | 133 | 44 | 108 |
| Lu II | +1 | 79 | 9 | 17 |
| Lu III | +2 | 64 | 0 | 0 |
| Lu IV | +3 | 100 | 0 | 0 |
| Lu V | +4 | 64 | 0 | 0 |
準位データの収録状況 ?
| イオン | 電荷 | 準位 |
|---|---|---|
| Lu I | 0 | 234 |
| Lu II | +1 | 40 |
| Lu III | +2 | 29 |
| Lu IV | +3 | 62 |
| Lu V | +4 | 40 |
| Lu VI | +5 | 2 |
| Lu VII | +6 | 2 |
| Lu VIII | +7 | 2 |
| Lu IX | +8 | 2 |
| Lu X | +9 | 2 |
イオン半径
| 電荷 | 配位 | スピン | 半径 |
|---|---|---|---|
| +3 | 6 | データなし | 86.1 pm |
| +3 | 8 | データなし | 97.7 pm |
| +3 | 9 | データなし | 103.2 pm |
化合物
同位体 (1)
| 質量数 | 原子質量(u) | 天然存在比 | 半減期 | 崩壊形式 | |
|---|---|---|---|---|---|
| 175 安定 | 174.9407752 ± 0.000002 | 97.4010% ± 0.0130% | 安定 | stable |
詳細な性質
共有結合半径(詳細)
- 共有結合半径(Pyykkö)
- 162 pm
- 共有結合半径(Pyykkö、二重結合)
- 131 pm
- 共有結合半径(Pyykkö、三重結合)
- 131 pm
ファンデルワールス半径
- Alvarez
- 274 pm
- UFF
- 364 pm
- MM3
- 265 pm
原子半径と金属半径
- 原子半径(Rahm)
- 270 pm
番号付けの尺度
- Mendeleev
- 41
- Pettifor
- 21
- Glawe
- 19
電気陰性度の尺度
- Ghosh
- 0
- Miedema
- 3
- Gunnarsson–Lundqvist
- 3
- Robles–Bartolotti
- 2
分極率と分散
- 双極子分極率
- 137 a.u.
- 双極子分極率(不確かさ)
- 7 a.u.
- C₆ (Gould–Bučko)
- 2020 Ha·Bohr6
化学親和力
- プロトン親和力
- 992 kJ/mol
- 気相塩基性
- 970.6 kJ/mol
ミーデマパラメータ
- ミーデマモル体積
- 17.77 cm3/mol
- ミーデマ電子密度
- 2
供給リスクと経済性
- 生産集中度
- 97
- 相対供給リスク
- 10
- 埋蔵量の分布
- 50
- 政治的安定性(最大生産国)
- 24
- 政治的安定性(最大埋蔵国)
- 24
相転移と同素体
| 融点 | 1936.15 K |
| 沸点 | 3675.15 K |
酸化数の分類
専門参考データ
遮蔽定数 (14)
| n | 軌道 | σ |
|---|---|---|
| 1 | s | 1.3805 |
| 2 | p | 4.389 |
| 2 | s | 18.5502 |
| 3 | d | 13.5812 |
| 3 | p | 20.8337 |
| 3 | s | 21.4655 |
| 4 | d | 35.7108 |
| 4 | f | 40.0688 |
| 4 | p | 33.8096 |
| 4 | s | 32.7308 |
結晶半径の詳細 (3)
| 電荷 | CN | スピン | rcrystal (pm) | 由来 |
|---|---|---|---|---|
| 3 | VI | 100.1 | from r^3 vs V plots, | |
| 3 | VIII | 111.7 | from r^3 vs V plots, | |
| 3 | IX | 117.2 | from r^3 vs V plots, |
同位体の崩壊形式 (53)
| 同位体 | モード | 強度 |
|---|---|---|
| 150 | p | 100% |
| 150 | B+ | — |
| 151 | p | — |
| 151 | B+ | — |
| 152 | B+ | 100% |
| 152 | B+p | 15% |
| 153 | A | — |
| 153 | B+ | — |
| 153 | p | 0% |
| 154 | B+ | — |
X線散乱因子 (514)
| エネルギー (eV) | f₁ | f₂ |
|---|---|---|
| 10 | — | 1.67493 |
| 10.1617 | — | 1.63824 |
| 10.3261 | — | 1.60236 |
| 10.4931 | — | 1.56726 |
| 10.6628 | — | 1.53293 |
| 10.8353 | — | 1.49935 |
| 11.0106 | — | 1.46651 |
| 11.1886 | — | 1.43538 |
| 11.3696 | — | 1.42424 |
| 11.5535 | — | 1.41319 |
追加データ
Estimated Crustal Abundance
The estimated element abundance in the earth's crust.
8×10-1 milligrams per kilogram
参考文献 (1)
- [5] Lutetium https://education.jlab.org/itselemental/ele071.html
Estimated Oceanic Abundance
The estimated element abundance in the earth's oceans.
1.5×10-7 milligrams per liter
参考文献 (1)
- [5] Lutetium https://education.jlab.org/itselemental/ele071.html
参考文献
(9)
Data deposited in or computed by PubChem
The half-life and atomic mass data was provided by the Atomic Mass Data Center at the International Atomic Energy Agency.
Element data are cited from the Atomic weights of the elements (an IUPAC Technical Report). The IUPAC periodic table of elements can be found at https://iupac.org/what-we-do/periodic-table-of-elements/. Additional information can be found within IUPAC publication doi:10.1515/pac-2015-0703 Copyright © 2020 International Union of Pure and Applied Chemistry.
The information are cited from Pure Appl. Chem. 2018; 90(12): 1833-2092, https://doi.org/10.1515/pac-2015-0703.
Thomas Jefferson National Accelerator Facility (Jefferson Lab) is one of 17 national laboratories funded by the U.S. Department of Energy. The lab's primary mission is to conduct basic research of the atom's nucleus using the lab's unique particle accelerator, known as the Continuous Electron Beam Accelerator Facility (CEBAF). For more information visit https://www.jlab.org/
The periodic table at the LANL (Los Alamos National Laboratory) contains basic element information together with the history, source, properties, use, handling and more. The provenance data may be found from the link under the source name.
The periodic table contains NIST's critically-evaluated data on atomic properties of the elements. The provenance data that include data for atomic spectroscopy, X-ray and gamma ray, radiation dosimetry, nuclear physics, and condensed matter physics may be found from the link under the source name. Ref: https://www.nist.gov/pml/atomic-spectra-database
This section provides all form of data related to element Lutetium.
The element property data was retrieved from publications.

