Ruthenium (Ru)
transition-metalSolid
표준 원자량
101.07 u전자 배치
[Kr] 5s1 4d7녹는점
2333.85 °C끓는점
4149.85 °C밀도
1.21e+4 kg/m³산화 상태
−4, −2, +1, +2, +3, +4, +5, +6, +7, +8전기 음성도(Pauling)
2.2제1 이온화 에너지
7.3605 eV발견 연도
1828원자 반지름
130 pm상세 정보
Ruthenium is a hard, platinum-group transition metal with atomic number 44. It is rare in the crust and is recovered chiefly with platinum and nickel-copper sulfide ores. Chemically it is notable for a wide range of oxidation states, especially +2, +3, +4, +6, and +8, and for forming many coordination and organometallic compounds. Metallic ruthenium improves hardness and corrosion resistance in some platinum and palladium alloys, while its oxides and complexes are important in catalysis and electrochemistry.
Ruthenium is a hard, white metal and has four crystal modifications. It does not tarnish at room temperatures, but oxidizes explosively. It is attacked by halogens, hydroxides, etc. Ruthenium can be plated by electrodeposition or by thermal decomposition methods. The metal is one of the most effective hardeners for platinum and palladium, and is alloyed with these metals to make electrical contacts for severe wear resistance. A ruthenium-molybdenum alloy is said to be superconductive at 10.6 K. The corrosion resistance of titanium is improved a hundredfold by addition of 0.1% ruthenium. It is a versatile catalyst. Hydrogen sulfide can be split catalytically by light using an aqueous suspension of CdS particles loaded with ruthenium dioxide. It is thought this may have application to removal of H2S from oil refining and other industrial processes. Compounds in at least eight oxidation states have been found, but of these, the +2, +3, and +4 states are the most common. Ruthenium tetroxide, like osmium tetroxide, is highly toxic. In addition, it may explode. Ruthenium compounds show a marked resemblance to those of cadmium.
The name derives from the Latin ruthenia for the old name of Russia. It was discovered in a crude platinum ore by the Russian chemist Gottfried Wilhelm Osann in 1828. Osann thought that he had found three new metals in the sample, pluranium, ruthenium, and polinium. In 1844, Russian chemist Karl Karlovich Klaus was able to show that Osann's mistake was due to the impurity of the sample, and Klaus was able to isolate the ruthenium metal.
Ruthenium was discovered by Karl Karlovich Klaus, a Russian chemist, in 1844 while analyzing the residue of a sample of platinum ore obtained from the Ural mountains. Apparently, Jedrzej Sniadecki, a Polish chemist, had produced ruthenium in 1807 but he withdrew his claim of discovery after other scientists failed to replicate his results. Ruthenium tends to occur along with deposits of platinum and is primarily obtained as a byproduct of mining and refining platinum. Ruthenium is also obtained as a byproduct of the nickel mining operation in the Sudbury region of Ontario, Canada.
From the Latin word Ruthenia, Russia. In 1827, Berzelius and Osann examined the residues left after dissolving crude platinum from the Ural mountains in aqua regia. While Berzelius found no unusual metals, Osann thought he found three new metals, one of which he named ruthenium. In 1844 Klaus, generally recognized as the discoverer, showed that Osann's ruthenium oxide was very impure and that it contained a new metal. Klaus obtained 6 g of ruthenium from the portion of crude platinum that is insoluble in aqua regia.
Pure ruthenium is a silvery gray, lustrous metal. It is hard and brittle at ordinary temperatures, has a high melting point, and resists attack by air, water, and many acids. Finely divided metal has a much larger reactive surface than compact metal.
Small additions of ruthenium harden platinum and palladium alloys used for wear-resistant electrical contacts, jewelry alloys, and some laboratory or industrial components. Ruthenium-containing materials are used in thick-film resistors and pastes for electronic circuits. Ruthenium dioxide, RuO₂, is an electrically conducting oxide used in electrochemical electrodes and as a catalyst component. Ruthenium complexes are also used as homogeneous catalysts, including catalysts for olefin metathesis and transfer hydrogenation. The radioisotope ¹⁰⁶Ru has been used in ophthalmic brachytherapy sources.
Ruthenium is primarily used as an alloying agent. Adding 0.1% ruthenium to titanium makes titanium 100 times more resistant to corrosion. Small amounts of ruthenium are added to platinum and palladium to strengthen them. These alloys are used in jewelry and in electrical contacts that must resist wear.
Isotopes in Earth/Planetary Science
100Ru is the product of a rare (and hence very long-lived) nuclear decay process from the double beta decay of 100Mo. A careful measurement of the half-life for this decay, which is 7.1×1018 years, can be used to place an upper limit on the mass of the electron neutrino, which is a neutral and weakly interacting subatomic particle first postulated by Wolfgang Pauli in 1930 [326] M. J. Hornish, L. De Braeckeleer, A. S. Barabash, V. I. Umatov. Phys. Rev. C74, 044314 (2006)..
Ruthenium and molybdenum share many similarities. They both have seven isotopes (96, 98, 99, 100, 101, 102, and 104 for ruthenium and 92, 94, 95, 96, 97, 98, and 100 for molybdenum), and their isotopes are formed by the same nucleosynthesisp-processes, r-processes, and s-processes, namely, p, r, s and r, s only, s and r, s and r, and r, respectively. The molybdenum and ruthenium isotopic composition of most meteorites lie along a mixing line (Fig. IUPAC.44.1). The ruthenium and molybdenum of silicates in the Earth also lie on this line, which supports the hypothesis that the Earth accreted homogeneously. That is, the feeding zone of the Earth did not change substantially over time as both the bulk of the Earth and the late veneer accreted from material having the same ruthenium-molybdenum isotopic reservoir [327] N. Dauphas, A. M. Davis, B. Marty, L. Reisberg. Earth Planet. Sci. Lett.226, 465 (2004)..
Isotopes in Medicine
106Ru plaque brachytherapy has been used for eye preservation and tumor control of uveal (the middle layer of the wall of the eye) melanoma [333] L. Tarmann, W. Wackernagel, A. Avian, C. Mayer, M. Schneider, P. Winkler, G. Langmann. Br. J. Ophthalmol.99, 1644 (2015).. The half-life of 106Ru is 373 days.
Isotopes Used as a Source of Radioactive Isotope(s)
96Ru is used to produce radioisotopes 94Ru (with a half-life of 52 min) and 95Ru (with half-life of about 1.64 h) via the reactions 96Ru (n, 3n) 94Ru and 96Ru (n, 2n) 95Ru, respectively (Fig. IUPAC.44.2) [334] A. R. Ketring, G. J. Ehrhardt, M. F. Embree, T. T. Tyler, J. A. Gawenis, S. S. Jurisson, H. P. Engelbrecht, C. J. Smith, C. S. Cutler. Alasbimn J.5 (19), (2003)., [335] J. W. Arblaster. Platinum Met. Rev.55, 124 (2011).. 104Ru is used to produce the radioisotope 105Rh (with a half-life of about 35 h) via the reaction 104Ru (p, γ) 105Rh. 105Rh has been used in the treatment of bone pain [334] A. R. Ketring, G. J. Ehrhardt, M. F. Embree, T. T. Tyler, J. A. Gawenis, S. S. Jurisson, H. P. Engelbrecht, C. J. Smith, C. S. Cutler. Alasbimn J.5 (19), (2003)..
Ruthenium chemistry spans many oxidation states, with +2, +3, and +4 common in coordination compounds and oxides. Ruthenium(III) chloride, RuCl₃, is a common precursor for laboratory synthesis, although commercial material may be hydrated or non-stoichiometric. Ruthenium dioxide, RuO₂, is a stable, conductive oxide with rutile-type structure. Ruthenium tetroxide, RuO₄, contains ruthenium in the +8 state and is a volatile, powerful oxidant. Organometallic ruthenium compounds include arene complexes and carbene complexes used in catalysis.
See more information at the Ruthenium compound page.
Bulk ruthenium metal is relatively inert, but dusts and powders can be fire or inhalation hazards in industrial handling. Soluble ruthenium salts and many complexes should be treated as toxic unless specifically characterized. Ruthenium tetroxide, RuO₄, is especially hazardous because it is volatile, strongly oxidizing, and damaging to tissue. Radioactive isotopes such as ¹⁰⁶Ru present isotope-specific radiation and contamination risks, particularly if dispersed as fine particles or volatile species.
Ruthenium occurs naturally at very low concentrations, mainly associated with platinum-group minerals and sulfide ore systems rather than as a major independent mineral resource. In surface environments it is generally immobile as metal or insoluble oxide, but soluble complexes can behave differently under oxidizing or complexing conditions. Anthropogenic releases are normally small and localized, except in special cases involving mining, refining, industrial catalysts, or nuclear fission products.
Ruthenium is produced as a by-product during refining of platinum-group metal concentrates and, to a lesser extent, nickel-copper sulfide ores. Supply is therefore tied to the mining and refining of other metals rather than to primary ruthenium mining. Demand is modest compared with platinum, palladium, and rhodium, but specialized uses in electronics, catalysts, electrochemical materials, and alloys can require high purity. Recycling occurs from some spent catalysts, electronic materials, and precious-metal alloys, although recovery depends strongly on concentration and process economics.
A member of the platinum group, ruthenium occurs native with other members of the group in ores found in the Ural mountains and in North and South America. It is also found along with other platinum metals in small but commercial quantities in pentlandite in the Sudbury, Ontario nickel-mining region, and in the pyroxinite deposits of South Africa.
Ruthenium is a heavy element formed mainly by neutron-capture nucleosynthesis in earlier generations of stars. It is far less abundant cosmically than iron-group elements, but it is present in meteorites and planetary materials at trace levels. Its association with other platinum-group elements reflects both nucleosynthetic origin and geochemical partitioning into metal-rich and sulfide-rich phases.
- Ruthenium was named from Ruthenia, a historical Latin name associated with parts of Eastern Europe.
- It is one of the least abundant stable platinum-group metals in Earth’s crust.
- Ruthenium tetroxide, RuO₄, is volatile despite being an oxide of a heavy metal.
- The metal can form a passive oxide surface that contributes to corrosion resistance.
- Some commercial RuCl₃ is not a simple anhydrous compound but a mixture of hydrated chloride species.
- Ruthenium catalysts are central to many well-known olefin metathesis reactions.
이미지
특성
물리적 특성
- 원자 반지름(경험값)
- 130 pm 모든 원소의 원자 반지름(경험값) 비교 →
- 공유 결합 반지름
- 146 pm 모든 원소의 공유 결합 반지름 비교 →
- 반데르발스 반지름
- 207 pm 모든 원소의 반데르발스 반지름 비교 →
- 금속 반지름
- 125 pm 모든 원소의 금속 반지름 비교 →
- 밀도
- 1.21 × 104 kg/m³ 모든 원소의 밀도 비교 →
- 몰 부피
- 0.0083 L/mol
- STP에서의 상
- 고체 모든 원소의 STP에서의 상 비교 →
- 녹는점
- 2333.85 °C 모든 원소의 녹는점 비교 →
- 끓는점
- 4149.85 °C 모든 원소의 끓는점 비교 →
- 열전도율
- 117 W/(m·K) 모든 원소의 열전도율 비교 →
- 비열
- 0.238 J/(g·K) 모든 원소의 비열 비교 →
- 몰 열용량
- 24.06 J/(mol·K) 모든 원소의 몰 열용량 비교 →
- 결정 구조
- 육방 조밀 충전 모든 원소의 결정 구조 비교 →
화학적 특성
- 전기 음성도(Pauling)
- 2.2 모든 원소의 전기 음성도(Pauling) 비교 →
- 전기 음성도(Allen)
- 1.54
- 전자 친화도
- 1.05 eV
- 제1 이온화 에너지
- 7.3605 eV 모든 원소의 제1 이온화 에너지 비교 →
- 제2 이온화 에너지
- 16.760058 eV 모든 원소의 제2 이온화 에너지 비교 →
- 제3 이온화 에너지
- 28.470098 eV 모든 원소의 제3 이온화 에너지 비교 →
- 제4 이온화 에너지
- 45.000155 eV 모든 원소의 제4 이온화 에너지 비교 →
- 제5 이온화 에너지
- 59.000203 eV 모든 원소의 제5 이온화 에너지 비교 →
- 산화 상태
- −4, −2, +1, +2, +3, +4, +5, +6, +7, +8 모든 원소의 산화 상태 비교 →
- 원자가 전자
- 8 모든 원소의 원자가 전자 비교 →
- 전자 배치
- [Kr] 5s1 4d7
열역학적 특성
- 융해열
- 0.24874333 eV 모든 원소의 융해열 비교 →
- 기화열
- 6.166762 eV 모든 원소의 기화열 비교 →
- 승화열
- 6.736798 eV
- 원자화열
- 6.736798 eV
- 원자화 엔탈피
- 6.743017 eV
핵 특성
- 양성자 수
- 44 모든 원소의 양성자 수 비교 →
- 중성자 수
- 58 모든 원소의 중성자 수 비교 →
- 알려진 동위원소 수
- 41 모든 원소의 알려진 동위원소 수 비교 →
- 안정 동위원소 수
- 6 모든 원소의 안정 동위원소 수 비교 →
- 가장 안정한 동위원소
- Ru-102
- 발견 연도
- 1828
존재비
- 존재비(지각)
- 0.001 mg/kg 모든 원소의 존재비(지각) 비교 →
- 존재비(해양)
- 7 × 10−7 mg/L 모든 원소의 존재비(해양) 비교 →
결정 구조
- 격자 상수 a
- 270 pm
전자 구조
- 전자껍질별 전자 수
- 2, 8, 18, 15, 1 모든 원소의 전자껍질별 전자 수 비교 →
식별자
- CAS 등록 번호
- 7440-18-8 모든 원소의 CAS 등록 번호 비교 →
- 항 기호
- 5F5
- InChI
- InChI=1S/Ru
- InChI 키
- KJTLSVCANCCWHF-UHFFFAOYSA-N
전자 배치 측정값
Ru: 4d⁷ 5s¹[Kr] 4d⁷ 5s¹1s² 2s² 2p⁶ 3s² 3p⁶ 3d¹⁰ 4s² 4p⁶ 4d⁷ 5s¹원자 모형
동위원소에 따라 중성자 수, 질량, 안정성은 달라지지만, 중성 원자의 전자 배치는 달라지지 않습니다.
개략적인 원자 모형이며 실제 비율과 다릅니다.
원자 지문
방출 / 흡수 스펙트럼
동위원소 분포
| 질량수 | 원자 질량(u) | 천연 존재비 | 반감기 |
|---|---|---|---|
| 98 안정 | 97.9052868 ± 0.0000069 | 1.8700% | 안정 |
| 99 안정 | 98.9059341 ± 0.0000011 | 12.7600% | 안정 |
| 100 안정 | 99.9042143 ± 0.0000011 | 12.6000% | 안정 |
| 101 안정 | 100.9055769 ± 0.0000012 | 17.0600% | 안정 |
| 102 안정 | 101.9043441 ± 0.0000012 | 31.5500% | 안정 |
| 104 안정 | 103.9054275 ± 0.0000028 | 18.6200% | 안정 |
상 / 상태
이유: 녹는점(2333.85 °C)보다 2308.8 °C 낮음
개략도이며 실제 비율과 다름
상전이점
전이 에너지
녹는점에서 1 mol을 녹이는 데 필요한 에너지
끓는점에서 1 mol을 기화시키는 데 필요한 에너지
승화점에서 1 mol을 승화시키는 데 필요한 에너지
밀도
표준 조건에서
표준 조건에서
원자 스펙트럼
전체 44개 중 10개를 표시합니다. 이온 전하순으로 정렬되었습니다(오름차순).
보유 에너지 준위 데이터 ?
| 이온 | 전하 | 준위 |
|---|---|---|
| Ru I | 0 | 329 |
| Ru II | +1 | 235 |
| Ru III | +2 | 26 |
| Ru IV | +3 | 2 |
| Ru V | +4 | 2 |
| Ru VI | +5 | 2 |
| Ru VII | +6 | 2 |
| Ru VIII | +7 | 2 |
| Ru IX | +8 | 2 |
| Ru X | +9 | 2 |
이온 반지름
| 전하 | 배위 | 스핀 | 반지름 |
|---|---|---|---|
| +3 | 6 | 해당 없음 | 68 pm |
| +4 | 6 | 해당 없음 | 62 pm |
| +5 | 6 | 해당 없음 | 56.49999999999999 pm |
| +7 | 4 | 해당 없음 | 38 pm |
| +8 | 4 | 해당 없음 | 36 pm |
화합물
동위원소 (6)
| 질량수 | 원자 질량(u) | 천연 존재비 | 반감기 | 붕괴 방식 | |
|---|---|---|---|---|---|
| 98 안정 | 97.9052868 ± 0.0000069 | 1.8700% ± 0.0300% | 안정 | stable | |
| 99 안정 | 98.9059341 ± 0.0000011 | 12.7600% ± 0.1400% | 안정 | stable | |
| 100 안정 | 99.9042143 ± 0.0000011 | 12.6000% ± 0.0700% | 안정 | stable | |
| 101 안정 | 100.9055769 ± 0.0000012 | 17.0600% ± 0.0200% | 안정 | stable | |
| 102 안정 | 101.9043441 ± 0.0000012 | 31.5500% ± 0.1400% | 안정 | stable | |
| 104 안정 | 103.9054275 ± 0.0000028 | 18.6200% ± 0.2700% | 안정 | stable |
확장 특성
공유 결합 반지름(확장)
- 공유 결합 반지름(Pyykkö)
- 125 pm
- 공유 결합 반지름(Pyykkö, 이중 결합)
- 114 pm
- 공유 결합 반지름(Pyykkö, 삼중 결합)
- 103 pm
반데르발스 반지름
- Batsanov
- 205 pm
- Alvarez
- 246 pm
- UFF
- 296.3 pm
- MM3
- 234 pm
원자 및 금속 반지름
- 원자 반지름(Rahm)
- 237 pm
- 금속 반지름(C12)
- 134 pm
번호 척도
- Mendeleev
- 60
- Pettifor
- 63
- Glawe
- 61
전기 음성도 척도
- Ghosh
- 0
- Miedema
- 5
- Gunnarsson–Lundqvist
- 4
- Robles–Bartolotti
- 3
분극률 및 분산
- 쌍극자 분극률
- 72 a.u.
- 쌍극자 분극률(불확도)
- 10 a.u.
- C₆ (Gould–Bučko)
- 809 Ha·Bohr6
화학 친화력
- 양성자 친화도
- 774 kJ/mol
- 기체상 염기성
- 751.4 kJ/mol
미데마 매개변수
- 미데마 몰 부피
- 8.2 cm3/mol
- 미데마 전자 밀도
- 6
공급 위험 및 경제성
- 생산 집중도
- 60
- 상대적 공급 위험
- 8
- 매장량 분포
- 95
- 정치적 안정성(최대 생산국)
- 44
- 정치적 안정성(최대 매장국)
- 44
상전이 및 동소체
| 녹는점 | 2606.15 K |
| 끓는점 | 4420.15 K |
산화 상태 분류
심화 참고 데이터
차폐 상수 (10)
| n | 오비탈 | σ |
|---|---|---|
| 1 | s | 0.9077 |
| 2 | p | 4.0492 |
| 2 | s | 11.6202 |
| 3 | d | 14.6411 |
| 3 | p | 16.7789 |
| 3 | s | 16.3988 |
| 4 | d | 31.1872 |
| 4 | p | 27.5652 |
| 4 | s | 26.344 |
| 5 | s | 37.5155 |
결정 반지름 상세 정보 (5)
| 전하 | CN | 스핀 | rcrystal (pm) | 기원 |
|---|---|---|---|---|
| 3 | VI | 82 | ||
| 4 | VI | 76 | from r^3 vs V plots, from metallic oxides, | |
| 5 | VI | 70.5 | estimated, from r^3 vs V plots, | |
| 7 | IV | 52 | ||
| 8 | IV | 50 |
동위원소 붕괴 방식 (62)
| 동위원소 | 모드 | 세기 |
|---|---|---|
| 85 | B+ | — |
| 85 | B+p | — |
| 85 | p | — |
| 86 | B+ | — |
| 86 | B+p | — |
| 87 | B+ | — |
| 87 | B+p | — |
| 88 | B+ | 100% |
| 88 | B+p | 3.6% |
| 89 | B+ | 100% |
X선 산란 인자 (615)
| 에너지 (eV) | f₁ | f₂ |
|---|---|---|
| 10 | — | 1.51919 |
| 10.1617 | — | 1.51438 |
| 10.3261 | — | 1.51486 |
| 10.4931 | — | 1.54335 |
| 10.6628 | — | 1.57238 |
| 10.8353 | — | 1.60195 |
| 11.0105 | — | 1.63207 |
| 11.1886 | — | 1.66277 |
| 11.3696 | — | 1.7032 |
| 11.5535 | — | 1.79614 |
추가 데이터
Estimated Crustal Abundance
The estimated element abundance in the earth's crust.
1×10-3 milligrams per kilogram
참고 문헌 (1)
- [5] Ruthenium https://education.jlab.org/itselemental/ele044.html
Estimated Oceanic Abundance
The estimated element abundance in the earth's oceans.
7×10-7 milligrams per liter
참고 문헌 (1)
- [5] Ruthenium https://education.jlab.org/itselemental/ele044.html
Sources
Sources of this element.
A member of the platinum group, ruthenium occurs native with other members of the group in ores found in the Ural mountains and in North and South America. It is also found along with other platinum metals in small but commercial quantities in pentlandite in the Sudbury, Ontario nickel-mining region, and in the pyroxinite deposits of South Africa.
참고 문헌 (1)
- [6] Ruthenium https://periodic.lanl.gov/44.shtml
Production
Production of this element (from raw materials or other compounds containing the element).
The metal is isolated commercially by a complex chemical process, the final stage of which is the hydrogen reduction of ammonium ruthenium chloride, which yields a powder. The powder is consolidated by powder metallurgy techniques or by argon-arc welding.
참고 문헌 (1)
- [6] Ruthenium https://periodic.lanl.gov/44.shtml
참고 문헌
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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 Ruthenium.
The element property data was retrieved from publications.