Nickel (Ni)
transition-metalSolid
표준 원자량
58.6934 u전자 배치
[Ar] 4s2 3d8녹는점
1454.85 °C끓는점
2912.85 °C밀도
8912 kg/m³산화 상태
−2, −1, 0, +1, +2, +3, +4전기 음성도(Pauling)
1.91제1 이온화 에너지
7.639878 eV발견 연도
1751원자 반지름
135 pm상세 정보
Nickel is a silvery transition metal of group 10, valued for corrosion resistance, strength at high temperature, and its ability to form useful alloys. It is ferromagnetic near room temperature and commonly occurs in the +2 oxidation state, although several other states are known in coordination chemistry. Natural nickel is mostly found in sulfide and laterite ores, and it is a key metal for stainless steels, superalloys, plating, catalysts, and rechargeable batteries.
Nickel is silvery white and takes on a high polish. It is hard, malleable, ductile, somewhat ferromagnetic, and a fair conductor of heat and electricity. It belongs to the iron-cobalt group of metals and is chiefly valuable for the alloys it forms.
The name derives from the German Nickel for "deceptive little spirit" because miners called mineral niccolite (NiAs) by the name Kupfernickel (false copper) because it resembled copper ores in appearance, but no copper was found in the ore. It was discovered by the Swedish metallurgist Axel-Frederik Cronstedt in 1751.
Nickel was discovered by the Swedish chemist Axel Fredrik Cronstedt in the mineral niccolite (NiAs) in 1751. Today, most nickel is obtained from the mineral pentlandite (NiS·2FeS). Most of the world's supply of nickel is mined in the Sudbury region of Ontario, Canada. It is believed that this large deposit of nickel ore is a result of an ancient meteor impact.
From the German word Nickel (Satan), and from kupfernickel, Old Nick's copper. Cronstedt discovered nickel in 1751 in kupfernickel (niccolite).
Pure nickel is a lustrous, silvery-white metal with a faint golden tinge. It is hard, ductile, and malleable, and it can take a high polish. Compact nickel resists attack by air and water under ordinary conditions because a thin protective surface film forms.
The largest use of nickel is in alloys, especially stainless steels, where it improves toughness, corrosion resistance, and formability. Nickel-base superalloys are used in turbine blades and other high-temperature parts. The metal is also used for electroplating, coinage alloys, catalysts such as Raney nickel, and electrical contacts. Nickel compounds and nickel metal are important in batteries, including nickel-cadmium, nickel-metal hydride, and many lithium-ion cathode chemistries.
Nickel is a hard, corrosion resistant metal. It can be electroplated onto other metals to form a protective coating. Finely divided nickel is used as a catalyst for the hydrogenation of vegetable oils. Adding nickel to glass gives it a green color. A single kilogram of nickel can be drawn into 300 kilometers of wire. Nickel is also used to manufacture some types of coins and batteries.
Nickel is alloyed with other metals to improve their strength and resistance to corrosion. Nickel is alloyed with steel to make armor plate, vaults and machine parts. It is alloyed with copper to make pipes that are used in desalination plants. Very powerful permanent magnets, known as Alnico magnets, can be made from an alloy of aluminum, nickel, cobalt and iron.
It is extensively used for making stainless steel and other corrosion-resistant alloys such as Invar(R), Monel(R), Inconel(R), and the Hastelloys(R). Tubing made of copper-nickel alloy is extensively used in making desalination plants for converting sea water into fresh water.
Nickel, used extensively to make coins and nickel steel for armor plates and burglar-proof vaults, and is also a component in Nichrome(R), Permalloy(R), and constantan.
Nickel gives glass a greenish color. Nickel plating is often used to provide a protective coating for other metals, and finely divided nickel is a catalyst for hydrogenating vegetable oils. It is also used in ceramics, in the manufacture of Alnico magnets, and in the Edison(R) storage battery.
Isotopes in Earth/Planetary Science
Because molecules, atoms, and ions of the stable isotopes of nickel possess slightly different physical and chemical properties, they commonly will be fractionated during physical, chemical, and biological processes, giving rise to variations in isotopic abundances and in atomic weights. There are measureable variations in the isotopic abundances of nickel in terrestrial silicate rocks (Fig. IUPAC.28.1) [228] B. Gueguen, O. Rouxel, E. Ponzevera, A. Bekker, Y. Fouquet. Geostand. Geoanal. Res.37, 297 (2013)..
Isotopes in Geochronology
Anomalies in 60Ni abundance caused by decay of now extinct 60Fe have been used to study the early history of our Solar System (see section 4.26.2). 59Ni is a cosmogenic radionuclide with a half-life of 7.6×104 years. Decay of 59Ni has been used to assess the terrestrial age of meteorites and to determine abundances of extraterrestrial dust in ice and sediment [230] G. F. Herzog, C. Schnabel, S. Xue, J. Masarik, R. G. Cresswell, M. L. D. Tada. Meteorit. Planet. Sci.33, A66 (1998)..
Isotopes in Industry
63Ni (with a half-life of 99 years) is produced from stable 62Ni and is a beta-emitting radionuclide that serves as an electron source together with 55Fe in electron-capture detectors. Electron-capture detectors are used as thickness gauges or as detectors for organic analytes in gas chromatography (Fig. IUPAC.28.2) [108] World Nuclear Association. Radioisotopes in Industry: Industrial Uses of Radioisotopes, World Nuclear Association (2014), Feb. 24; http://www.world-nuclear.org/info/inf56.html.. 63Ni is also used to ionize substances in ion mobility spectrometry–the basis of the instrument used in airports to screen passengers for drugs and bombs [231] J. R. Verkouteren, J. L. Staymates. Forensic Sci. Int.206, 190 (2011).. 63Ni is also used as a fluorescence-inducing source in elemental analysis by X-ray fluorescence spectroscopy and in miniaturized long-lived nuclear batteries [108] World Nuclear Association. Radioisotopes in Industry: Industrial Uses of Radioisotopes, World Nuclear Association (2014), Feb. 24; http://www.world-nuclear.org/info/inf56.html.. Until the mid-1980s, nuclear batteries were used in pacemakers, but then they were replaced by long-lasting lithium batteries [232] B. Ulmen, P. D. Desai, S. Moghaddam, G. H. Miley, R. I. Masel. J. Radioanal. Nucl. Chem.282, 601 (2009)..
Isotopes Used as a Source of Radioactive Isotope(s)
61Ni is used as a radiation target for production of the radioactive isotope 61Cu (with a half-life of 3.3 h), which emits positrons for positron emission tomography (PET) applications using the 61Ni (p, n) 61Cu reaction. 64Ni is used as a radiation target for production of 64Cu (with a half-life of 12.7 h), which is used in radioimmunotherapy by attaching it to an antibody for delivery of cytotoxic radiation (toxic to living cells) to a target cell via the 64Ni (p, n) 64Cu reaction [235] National Research Council. Isotopes for Medicine and the Life Sciences, p. 38, The National Academies Press, Washington, DC (1995).. 60Ni is used for the production of 57Co (with a half-life of 0.75 year), which is used as a reference source for gamma cameras that are used in nuclear medicinevia the 60Ni (p, 4He) 57Co reaction [235] National Research Council. Isotopes for Medicine and the Life Sciences, p. 38, The National Academies Press, Washington, DC (1995)..
Nickel chemistry is dominated by Ni²⁺, which forms many salts and coordination complexes. Nickel(II) oxide, NiO, is a green to black solid used in ceramics, catalysts, and battery materials. Nickel(II) sulfate, NiSO₄, is important in electroplating and hydrometallurgy. Nickel carbonyl, Ni(CO)₄, is a volatile zerovalent compound central to the Mond refining process and notable for its high toxicity. Nickel also forms sulfides, halides, organonickel complexes, and mixed oxides used as battery cathode precursors.
See more information at the Nickel compound page.
Nickel metal is not highly toxic as a solid, but nickel dusts, fumes, and soluble nickel salts can cause allergic contact dermatitis and respiratory sensitization. Some nickel compounds are classified as carcinogenic, especially with inhalation exposure in refining or processing environments. Nickel carbonyl, Ni(CO)₄, is acutely poisonous and readily absorbed by inhalation. Fine nickel powder can be a fire or explosion hazard.
Exposure to nickel metal and soluble compounds (as Ni) should not exceed 0.05 mg/cm3 (8-hour time-weighted average per 40-hour work week). Nickel sulfide fume and dust is recognized as being potentially carcinogenic.
Nickel is naturally present in rocks, soils, waters, and biological systems at low concentrations. Weathering releases Ni²⁺ and nickel-bearing particles, while industrial sources include mining, smelting, fuel combustion, waste disposal, and corrosion of alloys. Its mobility depends strongly on pH, organic matter, sulfide availability, and adsorption to iron and manganese oxides. Nickel is an essential trace nutrient for some microorganisms and plants, but elevated concentrations can be toxic.
Nickel is produced mainly from sulfide ores and lateritic ores. Sulfide concentrates are commonly smelted and refined, while laterites require energy-intensive pyrometallurgical or hydrometallurgical processing. Demand is strongly tied to stainless steel production and increasingly to battery materials, although cathode chemistry choices can change nickel intensity. Recycling from stainless steel scrap, superalloys, and batteries is economically important. Supply is influenced by ore type, energy cost, refining capacity, environmental controls, and the distribution of suitable deposits.
Nickel is found as a constituent in most meteorites and often serves as one of the criteria for distinguishing a meteorite from other minerals. Iron meteorites, or siderites, may contain iron alloyed with from 5 percent to nearly 20 percent nickel. Nickel is obtained commercially from pentlandite and pyrrhotite of the Sudbury region of Ontario, a district that produces about 30 percent of the world's supply of nickel.
Other deposits are found in New Caledonia, Australia, Cuba, Indonesia, and elsewhere.
Nickel is a relatively abundant iron-peak element made in late stellar burning and supernova nucleosynthesis. Radioactive ⁵⁶Ni, produced in explosive events, decays through ⁵⁶Co to ⁵⁶Fe and helps power the light curves of many supernovae. In planets, nickel partitions strongly with iron, so much of Earth’s nickel is thought to reside in the core, while accessible crustal nickel is concentrated by magmatic and weathering processes.
- Nickel was named from a troublesome copper ore that miners associated with a mischievous spirit.
- The kilogram was once defined by an alloy containing 90 percent platinum and 10 percent nickel.
- Nickel is one of the few elements ferromagnetic at ordinary temperatures.
- Raney nickel is a porous catalyst made by leaching aluminium from a nickel-aluminium alloy.
- Many meteorites contain iron-nickel metal rather than nickel as separate mineral grains.
이미지
특성
물리적 특성
- 원자 반지름(경험값)
- 135 pm 모든 원소의 원자 반지름(경험값) 비교 →
- 공유 결합 반지름
- 124 pm 모든 원소의 공유 결합 반지름 비교 →
- 반데르발스 반지름
- 163 pm 모든 원소의 반데르발스 반지름 비교 →
- 금속 반지름
- 115 pm 모든 원소의 금속 반지름 비교 →
- 밀도
- 8912 kg/m³ 모든 원소의 밀도 비교 →
- 몰 부피
- 0.0066 L/mol
- STP에서의 상
- 고체 모든 원소의 STP에서의 상 비교 →
- 녹는점
- 1454.85 °C 모든 원소의 녹는점 비교 →
- 끓는점
- 2912.85 °C 모든 원소의 끓는점 비교 →
- 열전도율
- 90.9 W/(m·K) 모든 원소의 열전도율 비교 →
- 비열
- 0.444 J/(g·K) 모든 원소의 비열 비교 →
- 몰 열용량
- 26.07 J/(mol·K) 모든 원소의 몰 열용량 비교 →
- 결정 구조
- 면심 입방 모든 원소의 결정 구조 비교 →
화학적 특성
- 전기 음성도(Pauling)
- 1.91 모든 원소의 전기 음성도(Pauling) 비교 →
- 전기 음성도(Allen)
- 1.88
- 전자 친화도
- 1.156 eV
- 제1 이온화 에너지
- 7.639878 eV 모든 원소의 제1 이온화 에너지 비교 →
- 제2 이온화 에너지
- 18.168901 eV 모든 원소의 제2 이온화 에너지 비교 →
- 제3 이온화 에너지
- 35.187121 eV 모든 원소의 제3 이온화 에너지 비교 →
- 제4 이온화 에너지
- 54.920189 eV 모든 원소의 제4 이온화 에너지 비교 →
- 제5 이온화 에너지
- 76.060262 eV 모든 원소의 제5 이온화 에너지 비교 →
- 산화 상태
- −2, −1, 0, +1, +2, +3, +4 모든 원소의 산화 상태 비교 →
- 원자가 전자
- 10 모든 원소의 원자가 전자 비교 →
- 전자 배치
- [Ar] 4s2 3d8
열역학적 특성
- 융해열
- 0.18116806 eV 모든 원소의 융해열 비교 →
- 기화열
- 3.838939 eV 모든 원소의 기화열 비교 →
- 승화열
- 4.457688 eV
- 원자화열
- 4.457688 eV
- 원자화 엔탈피
- 4.457688 eV
핵 특성
- 양성자 수
- 28 모든 원소의 양성자 수 비교 →
- 중성자 수
- 32 모든 원소의 중성자 수 비교 →
- 알려진 동위원소 수
- 35 모든 원소의 알려진 동위원소 수 비교 →
- 안정 동위원소 수
- 4 모든 원소의 안정 동위원소 수 비교 →
- 가장 안정한 동위원소
- Ni-60
- 발견 연도
- 1751
존재비
- 존재비(지각)
- 84 mg/kg 모든 원소의 존재비(지각) 비교 →
- 존재비(해양)
- 5.6 × 10−4 mg/L 모든 원소의 존재비(해양) 비교 →
결정 구조
- 격자 상수 a
- 352 pm
전자 구조
- 전자껍질별 전자 수
- 2, 8, 16, 2 모든 원소의 전자껍질별 전자 수 비교 →
식별자
- CAS 등록 번호
- 7440-02-0 모든 원소의 CAS 등록 번호 비교 →
- 항 기호
- 3F4
- InChI
- InChI=1S/Ni
- InChI 키
- PXHVJJICTQNCMI-UHFFFAOYSA-N
전자 배치 측정값
Ni: 3d⁸ 4s²[Ar] 3d⁸ 4s²1s² 2s² 2p⁶ 3s² 3p⁶ 3d⁸ 4s²원자 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 |
|---|---|---|---|
| 60 안정 | 59.93078588 ± 0.00000052 | 26.2230% | 안정 |
| 61 안정 | 60.93105557 ± 0.00000052 | 1.1399% | 안정 |
| 62 안정 | 61.92834537 ± 0.00000055 | 3.6346% | 안정 |
| 64 안정 | 63.92796682 ± 0.00000058 | 0.9255% | 안정 |
상 / 상태
이유: 녹는점(1454.85 °C)보다 1429.8 °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 28개 중 10개를 표시합니다. 이온 전하순으로 정렬되었습니다(오름차순).
보유 스펙트럼선 데이터 ?
| 이온 | 전하 | 총 스펙트럼선 수 | 전이 확률 | 준위 표기 |
|---|---|---|---|---|
| Ni I | 0 | 576 | 522 | 522 |
| Ni II | +1 | 249 | 208 | 208 |
| Ni III | +2 | 128 | 50 | 50 |
| Ni IV | +3 | 216 | 169 | 169 |
| Ni V | +4 | 1582 | 1566 | 1582 |
| Ni VII | +6 | 24 | 24 | 24 |
| Ni IX | +8 | 38 | 20 | 38 |
| Ni X | +9 | 41 | 0 | 41 |
보유 에너지 준위 데이터 ?
| 이온 | 전하 | 준위 |
|---|---|---|
| Ni I | 0 | 288 |
| Ni II | +1 | 719 |
| Ni III | +2 | 345 |
| Ni IV | +3 | 236 |
| Ni V | +4 | 324 |
| Ni VI | +5 | 273 |
| Ni VII | +6 | 45 |
| Ni VIII | +7 | 44 |
| Ni IX | +8 | 31 |
| Ni X | +9 | 34 |
이온 반지름
| 전하 | 배위 | 스핀 | 반지름 |
|---|---|---|---|
| +2 | 4 | 해당 없음 | 55.00000000000001 pm |
| +2 | 4 | 해당 없음 | 49 pm |
| +2 | 5 | 해당 없음 | 63 pm |
| +2 | 6 | 해당 없음 | 69 pm |
| +3 | 6 | low | 56.00000000000001 pm |
| +3 | 6 | high | 60 pm |
| +4 | 6 | low | 48 pm |
화합물
동위원소 (4)
The sulfate and the oxides are important compounds. Natural nickel is a mixture of five stable isotopes; nine other unstable isotopes are known.
| 질량수 | 원자 질량(u) | 천연 존재비 | 반감기 | 붕괴 방식 | |
|---|---|---|---|---|---|
| 60 안정 | 59.93078588 ± 0.00000052 | 26.2230% ± 0.0150% | 안정 | stable | |
| 61 안정 | 60.93105557 ± 0.00000052 | 1.1399% ± 0.0013% | 안정 | stable | |
| 62 안정 | 61.92834537 ± 0.00000055 | 3.6346% ± 0.0040% | 안정 | stable | |
| 64 안정 | 63.92796682 ± 0.00000058 | 0.9255% ± 0.0019% | 안정 | stable |
스펙트럼선
전체 433개 중 50개를 표시합니다. 기본적으로 세기가 측정된 스펙트럼선만 표시됩니다.
| 파장(nm) | 세기 | 이온화 단계 | 유형 | 전이 | 정확도 | 출처 | |
|---|---|---|---|---|---|---|---|
| 385.82968 nm | 1200 | Ni I | emission | 3d9.(2D).4s 1D → 3d9.(2D).4p 3F* | 측정값 | NIST | |
| 380.71402 nm | 700 | Ni I | emission | 3d9.(2D).4s 1D → 3d9.(2D).4p * | 측정값 | NIST | |
| 547.6904 nm | 180 | Ni I | emission | 3d10 1S → 3d9.(2D).4p 1P* | 측정값 | NIST | |
| 383.16908 nm | 110 | Ni I | emission | 3d9.(2D).4s 1D → 3d9.(2D).4p 3P* | 측정값 | NIST | |
| 397.35547 nm | 110 | Ni I | emission | 3d9.(2D).4s 1D → 3d9.(2D).4p 3P* | 측정값 | NIST | |
| 440.1541 nm | 110 | Ni I | emission | 3d8.(3F).4s.4p.(3P*) 5D* → 3d8.4s.(4F).5s 5F | 측정값 | NIST | |
| 471.4417 nm | 110 | Ni I | emission | 3d8.(3F).4s.4p.(3P*) 5G* → 3d8.4s.(4F).5s 5F | 측정값 | NIST | |
| 503.5362 nm | 100 | Ni I | emission | 3d9.(2D).4p 3F* → 3d9.(2D<5/2>).4d 2[9/2] | 측정값 | NIST | |
| 508.0533 nm | 100 | Ni I | emission | 3d9.(2D).4p 3F* → 3d9.(2D<5/2>).4d 2[9/2] | 측정값 | NIST | |
| 464.8652 nm | 75 | Ni I | emission | 3d8.(3F).4s.4p.(3P*) 5G* → 3d8.4s.(4F).5s 5F | 측정값 | NIST | |
| 460.4987 nm | 65 | Ni I | emission | 3d8.(3F).4s.4p.(3P*) 5G* → 3d8.4s.(4F).5s 5F | 측정값 | NIST | |
| 508.111 nm | 65 | Ni I | emission | 3d9.(2D).4p 1F* → 3d9.(2D<3/2>).4d 2[7/2] | 측정값 | NIST | |
| 447.0477 nm | 55 | Ni I | emission | 3d8.(3F).4s.4p.(3P*) 5D* → 3d8.4s.(4F).5s 5F | 측정값 | NIST | |
| 501.7576 nm | 50 | Ni I | emission | 3d8.(3F).4s.4p.(3P*) 5F* → 3d8.4s.(4F).5s 5F | 측정값 | NIST | |
| 478.6535 nm | 45 | Ni I | emission | 3d8.(3F).4s.4p.(3P*) 5G* → 3d8.4s.(4F).5s 5F | 측정값 | NIST | |
| 485.5411 nm | 45 | Ni I | emission | 3d9.(2D).4p 3P* → 3d9.(2D<5/2>).4d 2[3/2] | 측정값 | NIST | |
| 498.0173 nm | 45 | Ni I | emission | 3d8.(3F).4s.4p.(3P*) 5F* → 3d9.(2D<5/2>).4d 2[9/2] | 측정값 | NIST | |
| 490.4412 nm | 40 | Ni I | emission | 3d9.(2D).4p 3P* → 3d9.(2D<5/2>).4d 2[1/2] | 측정값 | NIST | |
| 475.6515 nm | 30 | Ni I | emission | 3d8.(3F).4s.4p.(3P*) 5G* → 3d8.4s.(4F).5s 5F | 측정값 | NIST | |
| 712.2197 nm | 26 | Ni I | emission | 3d9.(2D).4p 3P* → 3d9.(2D<5/2>).5s 2[5/2] | 측정값 | NIST | |
| 468.6213 nm | 23 | Ni I | emission | 3d8.(3F).4s.4p.(3P*) 5G* → 3d8.4s.(4F).5s 5F | 측정값 | NIST | |
| 513.7074 nm | 23 | Ni I | emission | 3d8.(1D).4s2 1D → 3d9.(2D).4p 1P* | 측정값 | NIST | |
| 570.9545 nm | 23 | Ni I | emission | 3d8.(1D).4s2 1D → 3d9.(2D).4p 1F* | 측정값 | NIST | |
| 742.2275 nm | 23 | Ni I | emission | 3d9.(2D).4p 3F* → 3d9.(2D<5/2>).5s 2[5/2] | 측정값 | NIST | |
| 471.5762 nm | 22 | Ni I | emission | 3d8.(3F).4s.4p.(3P*) 5G* → 3d8.4s.(4F).5s 5F | 측정값 | NIST | |
| 480.6993 nm | 22 | Ni I | emission | 3d9.(2D).4p * → 3d8.4s.(4F).5s 3F | 측정값 | NIST | |
| 491.8364 nm | 22 | Ni I | emission | 3d8.(3F).4s.4p.(3P*) 3G* → 3d8.4s.(4F).5s 3F | 측정값 | NIST | |
| 676.7772 nm | 22 | Ni I | emission | 3d10 1S → 3d9.(2D).4p 3P* | 측정값 | NIST | |
| 511.5392 nm | 21 | Ni I | emission | 3d8.(3F).4s.4p.(3P*) 3G* → 3d8.4s.(4F).5s 3F | 측정값 | NIST | |
| 483.1176 nm | 19 | Ni I | emission | 3d8.(3F).4s.4p.(3P*) 5F* → 3d8.4s.(4F).5s 5F | 측정값 | NIST | |
| 446.2455 nm | 18 | Ni I | emission | 3d8.(3F).4s.4p.(3P*) 5D* → 3d8.4s.(4F).5s 5F | 측정값 | NIST | |
| 460.0359 nm | 18 | Ni I | emission | 3d8.(3F).4s.4p.(3P*) 5G* → 3d8.4s.(4F).5s 5F | 측정값 | NIST | |
| 460.6221 nm | 18 | Ni I | emission | 3d8.(3F).4s.4p.(3P*) 5G* → 3d9.(2D<3/2>).4d 2[3/2] | 측정값 | NIST | |
| 501.2443 nm | 18 | Ni I | emission | 3d8.(3F).4s.4p.(3P*) 5F* → 3d8.4s.(4F).5s 5F | 측정값 | NIST | |
| 493.5831 nm | 16 | Ni I | emission | 3d8.(3F).4s.4p.(3P*) 3G* → 3d8.4s.(4F).5s 3F | 측정값 | NIST | |
| 504.8847 nm | 16 | Ni I | emission | 3d9.(2D).4p 1F* → 3d9.(2D<3/2>).4d 2[5/2] | 측정값 | NIST | |
| 575.4656 nm | 16 | Ni I | emission | 3d8.(3P).4s2 3P → 3d9.(2D).4p 1P* | 측정값 | NIST | |
| 664.363 nm | 16 | Ni I | emission | 3d8.(1D).4s2 1D → 3d9.(2D).4p 3P* | 측정값 | NIST | |
| 739.3676 nm | 16 | Ni I | emission | 3d8.(3F).4s2 3F → 3d8.(1D).4s2 1D | 측정값 | NIST | |
| 517.656 nm | 13 | Ni I | emission | 3d9.(2D).4p 1D* → 3d9.(2D<3/2>).4d 2[3/2] | 측정값 | NIST | |
| 559.2262 nm | 13 | Ni I | emission | 3d8.(3P).4s2 3P → 3d8.(3F).4s.4p.(3P*) 3D* | 측정값 | NIST | |
| 625.6355 nm | 13 | Ni I | emission | 3d8.(1D).4s2 1D → 3d9.(2D).4p 3P* | 측정값 | NIST | |
| 568.2199 nm | 12 | Ni I | emission | 3d8.(3F).4s.4p.(3P*) 3F* → 3d9.(2D<3/2>).4d 2[7/2] | 측정값 | NIST | |
| 571.1888 nm | 10 | Ni I | emission | 3d8.(3P).4s2 3P → 3d8.(3F).4s.4p.(3P*) 3F* | 측정값 | NIST | |
| 589.2872 nm | 10 | Ni I | emission | 3d8.(3P).4s2 3P → 3d9.(2D).4p 1P* | 측정값 | NIST | |
| 610.8116 nm | 10 | Ni I | emission | 3d8.(1D).4s2 1D → 3d9.(2D).4p 3D* | 측정값 | NIST | |
| 617.6811 nm | 10 | Ni I | emission | 3d8.(3F).4s.4p.(3P*) 3F* → 3d9.(2D<5/2>).4d 2[9/2] | 측정값 | NIST | |
| 631.4659 nm | 10 | Ni I | emission | 3d8.(3P).4s2 3P → 3d9.(2D).4p 1D* | 측정값 | NIST | |
| 691.4559 nm | 10 | Ni I | emission | 3d8.(3P).4s2 3P → 3d9.(2D).4p 3P* | 측정값 | NIST | |
| 558.7858 nm | 9 | Ni I | emission | 3d8.(3P).4s2 3P → 3d8.(3F).4s.4p.(3P*) 3D* | 측정값 | NIST |
확장 특성
공유 결합 반지름(확장)
- 공유 결합 반지름(Pyykkö)
- 110 pm
- 공유 결합 반지름(Pyykkö, 이중 결합)
- 101 pm
- 공유 결합 반지름(Pyykkö, 삼중 결합)
- 101 pm
- 공유 결합 반지름(Bragg)
- 135 pm
반데르발스 반지름
- Batsanov
- 200 pm
- Alvarez
- 240 pm
- UFF
- 283.4 pm
- MM3
- 222 pm
원자 및 금속 반지름
- 원자 반지름(Rahm)
- 229 pm
- 금속 반지름(C12)
- 124 pm
번호 척도
- Mendeleev
- 67
- Pettifor
- 67
- Glawe
- 69
전기 음성도 척도
- Ghosh
- 0
- Miedema
- 5
- Gunnarsson–Lundqvist
- 6
- Robles–Bartolotti
- 5
분극률 및 분산
- 쌍극자 분극률
- 49 a.u.
- 쌍극자 분극률(불확도)
- 3 a.u.
- C₆
- 373 Ha·Bohr6
- C₆ (Gould–Bučko)
- 393 Ha·Bohr6
화학 친화력
- 양성자 친화도
- 737 kJ/mol
- 기체상 염기성
- 714.1 kJ/mol
미데마 매개변수
- 미데마 몰 부피
- 6.6 cm3/mol
- 미데마 전자 밀도
- 5
공급 위험 및 경제성
- 생산 집중도
- 17
- 상대적 공급 위험
- 6
- 매장량 분포
- 36
- 정치적 안정성(최대 생산국)
- 18
- 정치적 안정성(최대 매장국)
- 75
상전이 및 동소체
| 녹는점 | 1728.15 K |
| 끓는점 | 3186.15 K |
산화 상태 분류
심화 참고 데이터
차폐 상수 (7)
| n | 오비탈 | σ |
|---|---|---|
| 1 | s | 0.6474 |
| 2 | p | 3.9048 |
| 2 | s | 7.7874 |
| 3 | d | 15.4705 |
| 3 | p | 13.915 |
| 3 | s | 13.039 |
| 4 | s | 22.2892 |
결정 반지름 상세 정보 (7)
| 전하 | CN | 스핀 | rcrystal (pm) | 기원 |
|---|---|---|---|---|
| 2 | IV | 69 | ||
| 2 | IVSQ | 63 | ||
| 2 | V | 77 | estimated, | |
| 2 | VI | 83 | from r^3 vs V plots, | |
| 3 | VI | LS | 70 | from r^3 vs V plots, |
| 3 | VI | HS | 74 | estimated, |
| 4 | VI | LS | 62 | from r^3 vs V plots, |
동위원소 붕괴 방식 (54)
| 동위원소 | 모드 | 세기 |
|---|---|---|
| 48 | 2p | 70% |
| 48 | B+ | 30% |
| 48 | B+p | — |
| 49 | B+ | 100% |
| 49 | B+p | 83.4% |
| 50 | B+ | 100% |
| 50 | B+p | 73% |
| 50 | 2p | 14% |
| 51 | B+ | 100% |
| 51 | B+p | 87.2% |
X선 산란 인자 (504)
| 에너지 (eV) | f₁ | f₂ |
|---|---|---|
| 10 | — | 1.37727 |
| 10.1617 | — | 1.38064 |
| 10.3261 | — | 1.38401 |
| 10.4931 | — | 1.3874 |
| 10.6628 | — | 1.39079 |
| 10.8353 | — | 1.39419 |
| 11.0106 | — | 1.39982 |
| 11.1886 | — | 1.44104 |
| 11.3696 | — | 1.48347 |
| 11.5535 | — | 1.52716 |
추가 데이터
Estimated Crustal Abundance
The estimated element abundance in the earth's crust.
8.4×101 milligrams per kilogram
참고 문헌 (1)
Estimated Oceanic Abundance
The estimated element abundance in the earth's oceans.
5.6×10-4 milligrams per liter
참고 문헌 (1)
Sources
Sources of this element.
Nickel is found as a constituent in most meteorites and often serves as one of the criteria for distinguishing a meteorite from other minerals. Iron meteorites, or siderites, may contain iron alloyed with from 5 percent to nearly 20 percent nickel. Nickel is obtained commercially from pentlandite and pyrrhotite of the Sudbury region of Ontario, a district that produces about 30 percent of the world's supply of nickel.
Other deposits are found in New Caledonia, Australia, Cuba, Indonesia, and elsewhere.
참고 문헌 (1)
- [6] Nickel https://periodic.lanl.gov/28.shtml
참고 문헌
(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 Nickel.
The element property data was retrieved from publications.