Lutetium (Lu)
lanthanideSolid
मानक परमाणु भार
174.9668 uइलेक्ट्रॉन विन्यास
[Xe] 6s2 4f14 5d1गलनांक
1662.85 °Cक्वथनांक
3401.85 °Cघनत्व
9840 kg/m³ऑक्सीकरण अवस्थाएँ
0, +1, +2, +3विद्युतऋणात्मकता (पॉलिंग)
1.27आयनन ऊर्जा (प्रथम)
5.425871 eVखोज का वर्ष
1907परमाणु त्रिज्या
175 pmविवरण
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.
चित्र
गुण
भौतिक
- परमाणु त्रिज्या (आनुभविक)
- 175 pm सभी तत्वों की परमाणु त्रिज्या (आनुभविक) की तुलना करें →
- सहसंयोजक त्रिज्या
- 187 pm सभी तत्वों की सहसंयोजक त्रिज्या की तुलना करें →
- वान डर वाल्स त्रिज्या
- 221 pm सभी तत्वों की वान डर वाल्स त्रिज्या की तुलना करें →
- घनत्व
- 9840 kg/m³ सभी तत्वों की घनत्व की तुलना करें →
- मोलर आयतन
- 0.0178 L/mol
- STP पर प्रावस्था
- ठोस सभी तत्वों की STP पर प्रावस्था की तुलना करें →
- गलनांक
- 1662.85 °C सभी तत्वों की गलनांक की तुलना करें →
- क्वथनांक
- 3401.85 °C सभी तत्वों की क्वथनांक की तुलना करें →
- विशिष्ट ऊष्मा धारिता
- 0.154 J/(g·K) सभी तत्वों की विशिष्ट ऊष्मा धारिता की तुलना करें →
- मोलर ऊष्मा धारिता
- 26.86 J/(mol·K) सभी तत्वों की मोलर ऊष्मा धारिता की तुलना करें →
- क्रिस्टल संरचना
- षट्कोणीय सघन संकुलित सभी तत्वों की क्रिस्टल संरचना की तुलना करें →
रासायनिक
- विद्युतऋणात्मकता (पॉलिंग)
- 1.27 सभी तत्वों की विद्युतऋणात्मकता (पॉलिंग) की तुलना करें →
- विद्युतऋणात्मकता (ऐलन)
- 1.09
- इलेक्ट्रॉन बंधुता
- 0.346 eV
- आयनन ऊर्जा (प्रथम)
- 5.425871 eV सभी तत्वों की आयनन ऊर्जा (प्रथम) की तुलना करें →
- आयनन ऊर्जा (द्वितीय)
- 14.130049 eV सभी तत्वों की आयनन ऊर्जा (द्वितीय) की तुलना करें →
- आयनन ऊर्जा (तृतीय)
- 20.959472 eV सभी तत्वों की आयनन ऊर्जा (तृतीय) की तुलना करें →
- आयनन ऊर्जा (चतुर्थ)
- 45.249156 eV सभी तत्वों की आयनन ऊर्जा (चतुर्थ) की तुलना करें →
- आयनन ऊर्जा (पंचम)
- 66.80023 eV सभी तत्वों की आयनन ऊर्जा (पंचम) की तुलना करें →
- ऑक्सीकरण अवस्थाएँ
- 0, +1, +2, +3 सभी तत्वों की ऑक्सीकरण अवस्थाएँ की तुलना करें →
- संयोजकता इलेक्ट्रॉन
- 3 सभी तत्वों की संयोजकता इलेक्ट्रॉन की तुलना करें →
- इलेक्ट्रॉन विन्यास
- [Xe] 6s2 4f14 5d1
ऊष्मागतिक
- गलन ऊष्मा
- 0.18759393 eV सभी तत्वों की गलन ऊष्मा की तुलना करें →
- वाष्पन ऊष्मा
- 3.679328 eV सभी तत्वों की वाष्पन ऊष्मा की तुलना करें →
- ऊर्ध्वपातन ऊष्मा
- 4.435923 eV
- परमाणुकरण ऊष्मा
- 4.435923 eV
- परमाणुकरण एन्थैल्पी
- 4.431777 eV
नाभिकीय
- प्रोटॉन
- 71 सभी तत्वों की प्रोटॉन की तुलना करें →
- न्यूट्रॉन
- 104 सभी तत्वों की न्यूट्रॉन की तुलना करें →
- ज्ञात समस्थानिक
- 39 सभी तत्वों की ज्ञात समस्थानिक की तुलना करें →
- स्थिर समस्थानिक
- 1 सभी तत्वों की स्थिर समस्थानिक की तुलना करें →
- सबसे स्थिर समस्थानिक
- Lu-175
- खोज का वर्ष
- 1907
प्रचुरता
- प्रचुरता (भूपर्पटी)
- 0.8 mg/kg सभी तत्वों की प्रचुरता (भूपर्पटी) की तुलना करें →
- प्रचुरता (महासागर)
- 1.5 × 10−7 mg/L सभी तत्वों की प्रचुरता (महासागर) की तुलना करें →
क्रिस्टल संरचना
- जालक स्थिरांक a
- 351 pm
इलेक्ट्रॉनिक संरचना
- प्रति कोश इलेक्ट्रॉन
- 2, 8, 18, 32, 9, 2 सभी तत्वों की प्रति कोश इलेक्ट्रॉन की तुलना करें →
पहचानकर्ता
- CAS संख्या
- 7439-94-3 सभी तत्वों की CAS संख्या की तुलना करें →
- टर्म प्रतीक
- 2D3/2
- InChI
- InChI=1S/Lu
- InChI कुंजी
- OHSVLFRHMCKCQY-UHFFFAOYSA-N
इलेक्ट्रॉन विन्यास मापित
Lu: 4f¹⁴ 5d¹ 6s²[Xe] 4f¹⁴ 5d¹ 6s²1s² 2s² 2p⁶ 3s² 3p⁶ 3d¹⁰ 4s² 4p⁶ 4d¹⁰ 5s² 5p⁶ 4f¹⁴ 5d¹ 6s²परमाणु मॉडल
समस्थानिक न्यूट्रॉन की संख्या, द्रव्यमान और स्थिरता बदलते हैं — उदासीन परमाणु का इलेक्ट्रॉन विन्यास नहीं।
सांकेतिक परमाणु मॉडल, वास्तविक अनुपात में नहीं।
परमाणु पहचान-चिह्न
उत्सर्जन / अवशोषण स्पेक्ट्रम
समस्थानिक वितरण
| द्रव्यमान संख्या | परमाणु द्रव्यमान (u) | प्राकृतिक प्रचुरता | अर्धायु |
|---|---|---|---|
| 175 स्थिर | 174.9407752 ± 0.000002 | 97.4010% | स्थिर |
प्रावस्था / अवस्था
कारण: गलनांक (1662.85 °C) से 1637.8 °C कम
सांकेतिक, वास्तविक अनुपात में नहीं
प्रावस्था संक्रमण बिंदु
संक्रमण ऊर्जाएँ
गलनांक पर 1 mol को पिघलाने के लिए आवश्यक ऊर्जा
क्वथनांक पर 1 mol को वाष्पित करने के लिए आवश्यक ऊर्जा
ऊर्ध्वपातनांक पर 1 mol के ऊर्ध्वपातन के लिए आवश्यक ऊर्जा
घनत्व
मानक परिस्थितियों में
मानक परिस्थितियों में
परमाणु स्पेक्ट्रम
71 में से 10 दिखाए जा रहे हैं। आयन के आवेश के अनुसार आरोही क्रम में व्यवस्थित।
उपलब्ध स्पेक्ट्रमी रेखा डेटा ?
| आयन | आवेश | कुल रेखाएँ | संक्रमण प्रायिकताएँ | स्तर पदनाम |
|---|---|---|---|---|
| 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 |
उपलब्ध ऊर्जा स्तर डेटा ?
| आयन | आवेश | स्तर |
|---|---|---|
| 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 |
आयनिक त्रिज्याएँ
| आवेश | उपसहसंयोजन | प्रचक्रण | त्रिज्या |
|---|---|---|---|
| +3 | 6 | उपलब्ध नहीं | 86.1 pm |
| +3 | 8 | उपलब्ध नहीं | 97.7 pm |
| +3 | 9 | उपलब्ध नहीं | 103.2 pm |
यौगिक
समस्थानिक (1)
| द्रव्यमान संख्या | परमाणु द्रव्यमान (u) | प्राकृतिक प्रचुरता | अर्धायु | क्षय का प्रकार | |
|---|---|---|---|---|---|
| 175 स्थिर | 174.9407752 ± 0.000002 | 97.4010% ± 0.0130% | स्थिर | stable |
विस्तृत गुण
सहसंयोजक त्रिज्याएँ (विस्तृत)
- सहसंयोजक त्रिज्या (प्यूक्को)
- 162 pm
- सहसंयोजक त्रिज्या (प्यूक्को, द्विबंध)
- 131 pm
- सहसंयोजक त्रिज्या (प्यूक्को, त्रिबंध)
- 131 pm
वान डर वाल्स त्रिज्याएँ
- Alvarez
- 274 pm
- UFF
- 364 pm
- MM3
- 265 pm
परमाणु और धात्विक त्रिज्याएँ
- परमाणु त्रिज्या (राह्म)
- 270 pm
संख्यांकन मापक्रम
- Mendeleev
- 41
- Pettifor
- 21
- Glawe
- 19
विद्युतऋणात्मकता मापक्रम
- Ghosh
- 0
- Miedema
- 3
- Gunnarsson–Lundqvist
- 3
- Robles–Bartolotti
- 2
ध्रुवणीयता और परिक्षेपण
- द्विध्रुव ध्रुवणीयता
- 137 a.u.
- द्विध्रुव ध्रुवणीयता (अनिश्चितता)
- 7 a.u.
- C₆ (Gould–Bučko)
- 2020 Ha·Bohr6
रासायनिक बंधुता
- प्रोटॉन बंधुता
- 992 kJ/mol
- गैसीय क्षारकता
- 970.6 kJ/mol
मीडेमा प्राचल
- मीडेमा मोलर आयतन
- 17.77 cm3/mol
- मीडेमा इलेक्ट्रॉन घनत्व
- 2
आपूर्ति जोखिम और अर्थशास्त्र
- उत्पादन संकेंद्रण
- 97
- सापेक्ष आपूर्ति जोखिम
- 10
- भंडार वितरण
- 50
- राजनीतिक स्थिरता (प्रमुख उत्पादक)
- 24
- राजनीतिक स्थिरता (सबसे अधिक भंडार वाला देश)
- 24
प्रावस्था संक्रमण और अपररूप
| गलनांक | 1936.15 K |
| क्वथनांक | 3675.15 K |
ऑक्सीकरण अवस्था की श्रेणियाँ
उन्नत संदर्भ डेटा
परिरक्षण स्थिरांक (14)
| n | कक्षक | 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 |
क्रिस्टल त्रिज्याओं का विवरण (3)
| आवेश | CN | प्रचक्रण | rcrystal (pm) | उत्पत्ति |
|---|---|---|---|---|
| 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, |
समस्थानिक क्षय के प्रकार (53)
| समस्थानिक | मोड | तीव्रता |
|---|---|---|
| 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+ | — |
एक्स-रे प्रकीर्णन गुणक (514)
| ऊर्जा (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 |
अतिरिक्त डेटा
Estimated Crustal Abundance
The estimated element abundance in the earth's crust.
8×10-1 milligrams per kilogram
संदर्भ (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
संदर्भ (1)
- [5] Lutetium https://education.jlab.org/itselemental/ele071.html
संदर्भ
(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.

