Roentgenium (Rg)
transition-metalExpected to be a Solid
표준 원자량
281 u전자 배치
[Rn] 7s2 5f14 6d9 (예측값)녹는점
해당 없음끓는점
해당 없음밀도
2.87e+4 kg/m³산화 상태
−1, +1, +3, +5전기 음성도(Pauling)
해당 없음제1 이온화 에너지
해당 없음발견 연도
1994원자 반지름
138 pm상세 정보
Roentgenium is a synthetic transactinide element in group 11, below gold. It has been made only one atom at a time in heavy-ion fusion experiments, and all confirmed isotopes are highly radioactive and short-lived. Its chemistry has not been established experimentally in bulk or solution. Relativistic calculations generally place it among the coinage metals, but with properties that may differ appreciably from lighter homologues.
Roentgenium does not occur naturally in the Earth’s crust. Roentgenium was first synthesized by an international team of scientists from the GSI in Darmstadt, Germany, the Joint Institute for Nuclear Research (JINR) in Dubna, Russia, the Comenius University in Bratislava, Slovakia, and the University of Jyväskylä, Finland at the GSI Helmholtz Center for Heavy Ion Research in Darmstadt, Germany in 1994, using the nuclear reaction 209Bi (64Ni, n) 272Rg. The credit for the first synthesis was confirmed in 2003. The element was named after Wilhelm Conrad Roentgen (Fig. IUPAC.111.1), who discovered X-rays in 1895 [660], [661], [662]. Roentgenium has no known isotopic applications aside from scientific research.
Roentgenium is named after Wilhelm Conrad Röntgen.
Roentgenium was first produced by Peter Armbruster, Gottfried Münzenber and their team working at the Gesellschaft für Schwerionenforschung in Darmstadt, Germany in late 1994. They bombarded atoms of bismuth-209 with ions of nickel-64 with a device known as a linear accelerator. This produced three atoms of roentgenium-272, an isotope with a half-life of about 1.5 milliseconds (0.0015 seconds), and a free neutron. Roentgenium's most stable isotope, roentgenium-281, has a half-life of about 26 seconds and decays through spontaneous fission.
Discovered by Gesellschaft Schwerionenforschung (GSI) in Darmstadt, in 1994. Reasearch group of S. Hofmann, V. Ninov, F.P. Hessberger, P. Armbruster, H. Folger, G. Munzenberg, H.J. Schott, and others.
No macroscopic sample of roentgenium has ever been prepared, so its appearance is unknown. A bulk metal, if it could exist long enough, is expected from theory to be dense and metallic, but color, surface behavior, and ordinary physical constants have not been measured.
Roentgenium has no practical, commercial, medical, or industrial use. Its only use is in nuclear research, where individual atoms and their decay chains help test models of heavy-element formation, nuclear stability, and alpha decay. Experiments involving roentgenium also support the identification of neighboring superheavy nuclei, but the element is not available as a material for devices, tracers, or chemical applications.
Since only a few atoms of roentgenium have ever been produced, it currently has no uses outside of basic scientific research.
No confirmed roentgenium compound has been isolated or characterized. The element is expected to show group 11 chemistry in some respects, but strong relativistic effects make detailed predictions uncertain. The +1 and +3 oxidation states are commonly discussed in theoretical work, with possible analogies to gold compounds such as gold(III) chloride, AuCl₃, rather than to the more stable simple chemistry of copper or silver. Proposed species such as roentgenium fluorides or chlorides remain predictions, not observed substances.
See more information at the Roentgenium compound page.
The safety properties of roentgenium are governed by radioactivity rather than ordinary chemical toxicity. Known isotopes decay rapidly, mainly through alpha decay and spontaneous fission pathways within decay chains. The quantities produced are far below a macroscopic hazard under normal laboratory containment, but any experiment requires specialized radiological controls for heavy-ion target materials, recoil products, and short-lived radioactive daughters.
Roentgenium has no confirmed natural occurrence and no environmental cycle. Any atoms produced in a laboratory decay before they could disperse or participate in ordinary geochemical processes. Environmental relevance is therefore limited to controlled accelerator facilities and to the management of irradiated targets, catcher foils, and associated radioactive residues from superheavy-element experiments.
Roentgenium is not a commodity and has no market price, supply chain, or recycling practice. Production requires a heavy-ion accelerator, rare target materials, and long experiments with extremely low atom yields. The element is identified through decay correlations rather than collected as a product. Economic considerations are those of publicly or institutionally funded nuclear-physics research, including accelerator time, target preparation, detector systems, and radiological handling.
Made by bombarding bismuth-209 with nickel-60.
Roentgenium is not expected to be a persistent cosmic element because its known isotopes are too unstable. If nuclei with 111 protons are formed transiently in extreme nucleosynthetic environments, they would decay quickly unless an unknown much longer-lived isotope exists. No roentgenium has been detected in stars, meteorites, planets, or terrestrial minerals.
- Roentgenium was named in honor of Wilhelm Conrad Röntgen, discoverer of X-rays.
- Its identification relies on linking a few decay events to known daughter nuclei.
- The longest-lived confirmed isotopes still have half-lives far too short for chemical stockpiles.
- Roentgenium lies in the same periodic-table group as copper, silver, and gold.
- Chemical experiments have not yet established a measured oxidation state for roentgenium.
이미지
특성
물리적 특성
- 원자 반지름(경험값)
- 138 pm 모든 원소의 원자 반지름(경험값) 비교 →
- 밀도
- 2.87 × 104 kg/m³ 모든 원소의 밀도 비교 →
화학적 특성
- 전자 친화도
- 1.6 eV
- 산화 상태
- −1, +1, +3, +5 모든 원소의 산화 상태 비교 →
- 원자가 전자
- 2 모든 원소의 원자가 전자 비교 →
- 전자 배치
- [Rn] 7s2 5f14 6d9 (예측값)
열역학적 특성
해당 없음
핵 특성
- 양성자 수
- 111 모든 원소의 양성자 수 비교 →
- 중성자 수
- 171 모든 원소의 중성자 수 비교 →
- 알려진 동위원소 수
- 15 모든 원소의 알려진 동위원소 수 비교 →
- 안정 동위원소 수
- 0 모든 원소의 안정 동위원소 수 비교 →
- 질량수(가장 안정한 동위원소)
- 282
- 가장 안정한 동위원소
- Rg-282
- 발견 연도
- 1994
존재비
해당 없음
결정 구조
해당 없음
전자 구조
- 전자껍질별 전자 수
- 14, 9, 2 모든 원소의 전자껍질별 전자 수 비교 →
식별자
- CAS 등록 번호
- 54386-24-2 모든 원소의 CAS 등록 번호 비교 →
- InChI
- InChI=1S/Rg
- InChI 키
- LJROPTGWFUZRDB-UHFFFAOYSA-N
전자 배치 예측값
——이 이온의 전자 배치 데이터가 없습니다.
원자 모형
동위원소에 따라 중성자 수, 질량, 안정성은 달라지지만, 중성 원자의 전자 배치는 달라지지 않습니다.
해당 없음
개략적인 원자 모형이며 실제 비율과 다릅니다.
원자 지문
방출 / 흡수 스펙트럼
동위원소 분포
안정 동위원소가 없습니다.
| 질량수 | 원자 질량(u) | 천연 존재비 | 반감기 |
|---|---|---|---|
| 279 방사성 | 279.16272 ± 0.00051 | 해당 없음 | 170 ms |
| 282 방사성 | 282.16912 ± 0.00072 | 해당 없음 | 130 초 |
| 285 방사성 | 285.175771 ± 0.000644 | 해당 없음 | 30 초 |
| 274 방사성 | 274.15525 ± 0.00019 | 해당 없음 | 20 ms |
| 281 방사성 | 281.16636 ± 0.00089 | 해당 없음 | 19 초 |
상 / 상태
상/상태 데이터 없음
상/상태 데이터 없음
화합물
동위원소 (5)
| 질량수 | 원자 질량(u) | 천연 존재비 | 반감기 | 붕괴 방식 | |
|---|---|---|---|---|---|
| 279 방사성 | 279.16272 ± 0.00051 | 해당 없음 | 170 ms | α =100% | |
| 282 방사성 | 282.16912 ± 0.00072 | 해당 없음 | 130 초 | α =100% | |
| 285 방사성 | 285.175771 ± 0.000644 | 해당 없음 | 30 초 | α ?SF ? | |
| 274 방사성 | 274.15525 ± 0.00019 | 해당 없음 | 20 ms | α ≈100% | |
| 281 방사성 | 281.16636 ± 0.00089 | 해당 없음 | 19 초 | SF =87±0.8%α =13±0.8% |
확장 특성
공유 결합 반지름(확장)
- 공유 결합 반지름(Pyykkö)
- 121 pm
- 공유 결합 반지름(Pyykkö, 이중 결합)
- 116 pm
- 공유 결합 반지름(Pyykkö, 삼중 결합)
- 118 pm
번호 척도
- Mendeleev
- 74
분극률 및 분산
- 쌍극자 분극률
- 32 a.u.
- 쌍극자 분극률(불확도)
- 6 a.u.
산화 상태 분류
심화 참고 데이터
동위원소 붕괴 방식 (22)
| 동위원소 | 모드 | 세기 |
|---|---|---|
| 272 | A | 100% |
| 273 | A | — |
| 274 | A | 100% |
| 275 | A | — |
| 276 | A | — |
| 276 | SF | — |
| 277 | A | — |
| 277 | SF | — |
| 278 | A | 100% |
| 279 | A | 100% |
추가 데이터
Estimated Crustal Abundance
The estimated element abundance in the earth's crust.
Not Applicable
참고 문헌 (1)
- [5] Roentgenium https://education.jlab.org/itselemental/ele111.html
Estimated Oceanic Abundance
The estimated element abundance in the earth's oceans.
Not Applicable
참고 문헌 (1)
- [5] Roentgenium https://education.jlab.org/itselemental/ele111.html
참고 문헌
(8)
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.
This section provides all form of data related to element Roentgenium.