Cobalt (Co)
transition-metalSolid
표준 원자량
58.933194 u전자 배치
[Ar] 4s2 3d7녹는점
1494.85 °C끓는점
2926.85 °C밀도
8860 kg/m³산화 상태
−3, −1, 0, +1, +2, +3, +4, +5전기 음성도(Pauling)
1.88제1 이온화 에너지
7.88101 eV발견 연도
1735원자 반지름
135 pm상세 정보
Cobalt is a hard transition metal of group 9, best known for stable high-temperature alloys, magnetic materials, rechargeable battery cathodes, and intensely colored blue pigments. It occurs in nature chiefly as a minor constituent of sulfide and arsenide minerals and is commonly recovered with copper or nickel. Chemically it is dominated by the +2 and +3 oxidation states, with coordination chemistry that includes biologically important corrinoids.
Cobalt is a brittle, hard metal, resembling iron and nickel in appearance. It has a metallic permeability of about two thirds that of iron. Cobalt tends to exist as a mixture of two allotropes over a wide temperature range. The transformation is sluggish and accounts in part for the wide variation in reported data on physical properties of cobalt.
The name derives from the German Kobold for "evil spirits" or "goblins", who were superstitiously thought to cause trouble for miners because the mineral contained arsenic that injured their health and the metallic ores did not yield metals when treated with the normal methods. Cobalt was discovered in 1735 by the Swedish chemist Georg Brandt.
Cobalt was discovered by Georg Brandt, a Swedish chemist, in 1739. Brandt was attempting to prove that the ability of certain minerals to color glass blue was due to an unknown element and not to bismuth, as was commonly believed at the time. Cobalt's primary ores are cobaltite (CoAsS) and erythrite (Co3(AsO4)2). Cobalt is usually recovered as a byproduct of mining and refining nickel, silver, lead, copper and iron.
From the German word Kobald, goblin or evil spirit; also from the Greek cobalos, mine. George Brandt discovered cobalt in 1735.
Pure cobalt is a lustrous, silvery gray metal with a faint bluish cast. It is hard, relatively brittle compared with many structural metals, and ferromagnetic near room temperature. Finely divided cobalt has a much larger reactive surface and can behave differently from compact metal.
Cobalt is used in superalloys for turbine blades and other hot, highly stressed components, where it helps retain strength and resist corrosion. It is a key constituent of some permanent magnets and magnetic recording alloys. Large quantities are used in lithium-ion battery cathode materials, especially layered oxides containing lithium, cobalt, nickel, manganese, or aluminum. Cobalt compounds are also used as catalysts, driers for paints and inks, and blue ceramic and glass colorants. The radioisotope cobalt-60 is used as a gamma-ray source for sterilization, radiography, and radiotherapy.
Although cobalt is used in electroplating to give objects an attractive surface that resists oxidation, it is more widely used to form alloys. Alnico, an alloy consisting of aluminum, nickel and cobalt is used to make powerful permanent magnets. Stellite alloys, which contain cobalt, chromium and tungsten, are used to make high-speed and high temperature cutting tools and dyes. Cobalt is also used to make alloys for jet engines and gas turbines, magnetic steels and some types of stainless steels.
Cobalt-60, a radioactive isotope of cobalt, is an important source of gamma rays and is used to treat some forms of cancer and as a medical tracer. Cobalt-60 has a half-life of 5.27 years and decays into nickel-60 through beta decay.
Cobalt compounds have been used for centuries to color porcelain, glass, pottery, tile and enamel. Some of these compounds are known as: cobalt blue, ceruleum, new blue, smalt, cobalt yellow and cobalt green. In addition to being used as a dye, cobalt is also important to human nutrition as it is an essential part of vitamin B12.
It is alloyed with iron, nickel and other metals to make Alnico, an alloy of unusual magnetic strength with many important uses. Stellite alloys, containing cobalt, chromium, and tungsten, are used for high-speed, heavy-duty, high temperature cutting tools, and for dies.
Cobalt is also used in other magnetic steels and stainless steels, and in alloys used in jet turbines and gas turbine generators. The metal is used in electroplating because of its appearance, hardness, and resistance to oxidation.
Cobalt salts have been used for centuries to produce brilliant and permanent blue colors in porcelain, glass, pottery, tiles, and enamels. It is the principal ingredient in Sevre's and Thenard's blue. A solution of the chloride is used as a sympathetic ink. Cobalt carefully used in the form of the chloride, sulfate, acetate, or nitrate has been found effective in correcting a certain mineral deficiency disease in animals.
Soils should contain 0.13 to 0.30 ppm of cobalt for proper animal nutrition.
Isotopes in Industry
60Co (with a half-life of 5.27 years) is used to irradiate food sources as a method of preserving food (Fig. IUPAC.27.1). The gamma radiation from 60Co kills bacteria and other organisms that cause disease and spoilage of food (see Fig. IUPAC.27.1). The use of radioactive compounds for preserving food is not always viewed positively. Some individuals are concerned that harmful compounds will be produced during the irradiation process. However, there is no evidence to support the claim that irradiation is dangerous for food preservation [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.. Many medical products today are sterilized using gamma rays from a 60Co source. This technique of sterilization is generally much cheaper and more effective than steam-heat sterilization because it is a cold process. For example, it can be performed on packaged items, such as disposable syringes. This sterilization technique is applicable to a wide range of heat-sensitive items, such as powders, ointments, and solutions, as well as biological preparations, such as bone, nerve, skin, etc., used in tissue grafts [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..
60Co is also used in industrial radiography to detect structural flaws in metal parts. The radiation can penetrate metals and the X-ray pattern produced by the radiating material can provide information on its strength, composition, and other properties [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.. Because of the above property, 60Co is also used in leveling devices and thickness gauges used to test welds and castings [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..
Isotopes in Medicine
60Co is a radioactive metal isotope that is used in cancer treatments by radiotherapy. When 60Co undergoes radioactive decay, high-energy gamma rays (energies of 1.17 MeV and 1.33 MeV) are emitted and have been used in brachytherapy to treat various types of cancer. Brachytherapy (brachy is Greek meaning “short distance”) is a method of radiation treatment in which sealed sources are used to deliver a radiation dose at a distance of up to a few centimeters by surface, intracavitary (insertion of the radioactive isotope in a body cavity), or interstitial (between cells) application [75] J. Peterson, M. McDonell, L. Haroun, F. Monette, R. D. Hildebrand, A. Taboas. Radiological and Chemical Fact Sheets to Support Health Risk Analyses for Contaminated Areas, Prepared by Argonne National Laboratory Environmental Science Division in collaboration with U.S. Department of Energy, Richland Operations Office and Chicago Operations Office (2014), Feb. 22; http://www.remm.nlm.gov/ANL_ContaminantFactSheets_All_070418.pdf.. 60Co is used as a source of high-energy ionizing gamma radiation that can be directed to cancer cells from a device outside the body (external radiotherapy).
60Co (and sometimes 57Co and 58Co, with half-lives of 0.75 year and 71 days, respectively) is the key component of the Schilling test, which is a method for determining whether a patient’s body is making and using vitamin B12 properly. The cobalt isotope is used to label cobalt in vitamin B12 to monitor how the body processes this essential vitamin [224] B. R. Krynyckyi, L. S. Zuckier. J. Nucl. Med.36, 1659 (1995)..
57Co delivers the smallest radiation dose of all the cobalt isotopes. As a result, it has been used in the past for imaging and estimating organ size and location and in evaluating tumors of the head and neck [75] J. Peterson, M. McDonell, L. Haroun, F. Monette, R. D. Hildebrand, A. Taboas. Radiological and Chemical Fact Sheets to Support Health Risk Analyses for Contaminated Areas, Prepared by Argonne National Laboratory Environmental Science Division in collaboration with U.S. Department of Energy, Richland Operations Office and Chicago Operations Office (2014), Feb. 22; http://www.remm.nlm.gov/ANL_ContaminantFactSheets_All_070418.pdf., [99] World Nuclear Association. Radioisotopes in Medicine, World Nuclear Association (2014), Feb. 23; http://www.world-nuclear.org/info/inf55.html., [225] Royal Society of Chemistry. Cobalt, Royal Society of Chemistry (2017), Feb. 26; http://www.rsc.org/periodic-table/element/27/cobalt., [226] US Environmental Protection Agency. Cobalt, US Environmental Protection Agency (2017), Feb. 26; https://www.epa.gov/radiation/radionuclide-basics-cobalt-60., [227] Washington State Department of Health. Cobalt-60, Washington State Department of Health (2014), Feb. 26; http://www.doh.wa.gov/Portals/1/Documents/Pubs/320-078_co60_fs.pdf..
Cobalt commonly forms cobalt(II) compounds such as cobalt(II) oxide (CoO), cobalt(II) chloride (CoCl₂), and cobalt(II) sulfate (CoSO₄). Cobalt(III) is strongly stabilized in many coordination compounds, including hexaamminecobalt(III) chloride ([Co(NH₃)₆]Cl₃), and in oxides used in battery electrodes such as lithium cobalt oxide (LiCoO₂). Mixed-valence cobalt oxides include cobalt(II,III) oxide (Co₃O₄). The element also forms carbonyls, notably dicobalt octacarbonyl (Co₂(CO)₈), and complex corrinoid chemistry in vitamin B₁₂ derivatives.
See more information at the Cobalt compound page.
Cobalt is an essential trace element only as part of vitamin B₁₂, but soluble cobalt salts, metal dusts, and some cobalt-containing powders can be harmful by inhalation, ingestion, or skin contact. Industrial exposure may cause respiratory sensitization, dermatitis, and other toxic effects. Cobalt metal powder can present fire or dust hazards. Cobalt-60 is radioactive and hazardous because it emits penetrating gamma radiation; its risks are isotope-specific and depend on activity and shielding.
Exposure to cobalt (metal fumes and dust) should be limited to 0.05 mg/m3 (8-hour time-weighted average 40-hour week).
Cobalt is a trace element in soils, waters, and living systems. It is released naturally by weathering of rocks and minerals and also through mining, smelting, combustion residues, and disposal of cobalt-bearing products. In soils and sediments it can adsorb to iron and manganese oxides or occur in sulfide-rich phases, which affects mobility. It is nutritionally important for organisms that require vitamin B₁₂, but elevated bioavailable concentrations can be toxic.
Cobalt is produced mainly as a by-product of copper and nickel mining, so supply is tied to markets and operations whose primary product is usually another metal. Ores are processed by flotation, leaching, solvent extraction, precipitation, and refining to metal, salts, or battery-grade intermediates. Demand is strongly influenced by rechargeable batteries, superalloys, catalysts, and hard metals. Supply concentration, by-product dependence, and processing capacity make substitution and recycling important. Recycling recovers cobalt from spent batteries, superalloy scrap, and cemented carbides, but collection and chemistry vary by product type.
Cobalt occurs in the minerals cobaltite, smaltite, and erythrite, and is often associated with nickel, silver, lead, copper, and iron ores, from which it is most frequently obtained as a by-product. It is also present in meteorites.
Important ore deposits are found in Zaire, Morocco, and Canada. The U.S. Geological Survey has announced that the bottom of the north central Pacific Ocean may have cobalt-rich deposits at relatively shallow depths in water close to the the Hawaiian Islands and other U.S. Pacific territories.
Cobalt is far less abundant than iron and nickel but is a normal product of stellar nucleosynthesis. Stable cobalt is represented in nature by ⁵⁹Co, while radioactive cobalt isotopes can be produced in supernovae, cosmic-ray interactions, and neutron activation. In meteorites and planetary materials, cobalt tends to follow siderophile and chalcophile behavior, associating with metal and sulfide phases.
- Natural cobalt is essentially monoisotopic, consisting of stable ⁵⁹Co.
- The name comes from miners’ terms for troublesome ores that yielded toxic arsenic fumes.
- Cobalt blue pigments were valued long before cobalt was isolated as a metal.
- Cobalt remains ferromagnetic at temperatures above ordinary ambient conditions.
- Vitamin B₁₂ contains cobalt in a corrin ring, not as free cobalt metal.
이미지
특성
물리적 특성
- 원자 반지름(경험값)
- 135 pm 모든 원소의 원자 반지름(경험값) 비교 →
- 공유 결합 반지름
- 126 pm 모든 원소의 공유 결합 반지름 비교 →
- 반데르발스 반지름
- 192 pm 모든 원소의 반데르발스 반지름 비교 →
- 금속 반지름
- 116 pm 모든 원소의 금속 반지름 비교 →
- 밀도
- 8860 kg/m³ 모든 원소의 밀도 비교 →
- 몰 부피
- 0.0067 L/mol
- STP에서의 상
- 고체 모든 원소의 STP에서의 상 비교 →
- 녹는점
- 1494.85 °C 모든 원소의 녹는점 비교 →
- 끓는점
- 2926.85 °C 모든 원소의 끓는점 비교 →
- 열전도율
- 100 W/(m·K) 모든 원소의 열전도율 비교 →
- 비열
- 0.421 J/(g·K) 모든 원소의 비열 비교 →
- 몰 열용량
- 24.81 J/(mol·K) 모든 원소의 몰 열용량 비교 →
- 결정 구조
- 육방 조밀 충전 모든 원소의 결정 구조 비교 →
화학적 특성
- 전기 음성도(Pauling)
- 1.88 모든 원소의 전기 음성도(Pauling) 비교 →
- 전기 음성도(Allen)
- 1.84
- 전자 친화도
- 0.661 eV
- 제1 이온화 에너지
- 7.88101 eV 모든 원소의 제1 이온화 에너지 비교 →
- 제2 이온화 에너지
- 17.084459 eV 모든 원소의 제2 이온화 에너지 비교 →
- 제3 이온화 에너지
- 33.500115 eV 모든 원소의 제3 이온화 에너지 비교 →
- 제4 이온화 에너지
- 51.270176 eV 모든 원소의 제4 이온화 에너지 비교 →
- 제5 이온화 에너지
- 79.500274 eV 모든 원소의 제5 이온화 에너지 비교 →
- 산화 상태
- −3, −1, 0, +1, +2, +3, +4, +5 모든 원소의 산화 상태 비교 →
- 원자가 전자
- 9 모든 원소의 원자가 전자 비교 →
- 전자 배치
- [Ar] 4s2 3d7
열역학적 특성
- 융해열
- 0.1677981 eV 모든 원소의 융해열 비교 →
- 기화열
- 3.886614 eV 모든 원소의 기화열 비교 →
- 승화열
- 4.40172 eV
- 원자화열
- 4.40172 eV
- 원자화 엔탈피
- 4.422449 eV
핵 특성
- 양성자 수
- 27 모든 원소의 양성자 수 비교 →
- 중성자 수
- 32 모든 원소의 중성자 수 비교 →
- 알려진 동위원소 수
- 32 모든 원소의 알려진 동위원소 수 비교 →
- 안정 동위원소 수
- 1 모든 원소의 안정 동위원소 수 비교 →
- 가장 안정한 동위원소
- Co-59
- 발견 연도
- 1735
존재비
- 존재비(지각)
- 25 mg/kg 모든 원소의 존재비(지각) 비교 →
- 존재비(해양)
- 2 × 10−5 mg/L 모든 원소의 존재비(해양) 비교 →
결정 구조
- 격자 상수 a
- 251 pm
전자 구조
- 전자껍질별 전자 수
- 2, 8, 15, 2 모든 원소의 전자껍질별 전자 수 비교 →
식별자
- CAS 등록 번호
- 7440-48-4 모든 원소의 CAS 등록 번호 비교 →
- 항 기호
- 4F9/2
- InChI
- InChI=1S/Co
- InChI 키
- GUTLYIVDDKVIGB-UHFFFAOYSA-N
전자 배치 측정값
Co: 3d⁷ 4s²[Ar] 3d⁷ 4s²1s² 2s² 2p⁶ 3s² 3p⁶ 3d⁷ 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 |
|---|---|---|---|
| 59 안정 | 58.93319429 ± 0.00000056 | 100.0000% | 안정 |
상 / 상태
이유: 녹는점(1494.85 °C)보다 1469.8 °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 27개 중 10개를 표시합니다. 이온 전하순으로 정렬되었습니다(오름차순).
보유 스펙트럼선 데이터 ?
| 이온 | 전하 | 총 스펙트럼선 수 | 전이 확률 | 준위 표기 |
|---|---|---|---|---|
| Co I | 0 | 420 | 338 | 338 |
| Co II | +1 | 3168 | 2761 | 3168 |
| Co III | +2 | 2064 | 1957 | 2064 |
| Co IV | +3 | 9 | 0 | 0 |
| Co V | +4 | 55 | 0 | 0 |
| Co VIII | +7 | 165 | 150 | 165 |
| Co IX | +8 | 48 | 19 | 48 |
| Co X | +9 | 22 | 5 | 22 |
보유 에너지 준위 데이터 ?
| 이온 | 전하 | 준위 |
|---|---|---|
| Co I | 0 | 330 |
| Co II | +1 | 482 |
| Co III | +2 | 288 |
| Co IV | +3 | 297 |
| Co V | +4 | 268 |
| Co VI | +5 | 180 |
| Co VII | +6 | 65 |
| Co VIII | +7 | 73 |
| Co IX | +8 | 40 |
| Co X | +9 | 31 |
이온 반지름
| 전하 | 배위 | 스핀 | 반지름 |
|---|---|---|---|
| +2 | 4 | high | 57.99999999999999 pm |
| +2 | 5 | 해당 없음 | 67 pm |
| +2 | 6 | low | 65 pm |
| +2 | 6 | high | 74.5 pm |
| +2 | 8 | 해당 없음 | 90 pm |
| +3 | 6 | low | 54.50000000000001 pm |
| +3 | 6 | high | 61 pm |
| +4 | 4 | 해당 없음 | 40 pm |
| +4 | 6 | high | 53 pm |
화합물
동위원소 (1)
Cobalt-60, an artificial isotope, is an important gamma ray source, and is extensively used as a tracer and a radiotherapeutic agent.
| 질량수 | 원자 질량(u) | 천연 존재비 | 반감기 | 붕괴 방식 | |
|---|---|---|---|---|---|
| 59 안정 | 58.93319429 ± 0.00000056 | 100.0000% | 안정 | stable |
스펙트럼선
전체 738개 중 50개를 표시합니다. 기본적으로 세기가 측정된 스펙트럼선만 표시됩니다.
| 파장(nm) | 세기 | 이온화 단계 | 유형 | 전이 | 정확도 | 출처 | |
|---|---|---|---|---|---|---|---|
| 389.4073 nm | 7900 | Co I | emission | 3p6.3d8.(3F).4s a 2F → 3p6.3d8.(3F).4p y 2G* | 측정값 | NIST | |
| 384.5461 nm | 6900 | Co I | emission | 3p6.3d8.(3F).4s a 2F → 3p6.3d8.(3F).4p y 2G* | 측정값 | NIST | |
| 399.5302 nm | 6000 | Co I | emission | 3p6.3d8.(3F).4s a 2F → 3p6.3d8.(3F).4p y 4G* | 측정값 | NIST | |
| 512.92021 nm | 5800 | Co II | emission | 3d7.(4F).4d e 5H → 3d7.(4F<9/2>).4f 2[15/2]* | 측정값 | NIST | |
| 387.3114 nm | 5500 | Co I | emission | 3p6.3d8.(3F).4s b 4F → 3p6.3d7.(4F).4s.4p.(3P*) z 4D* | 측정값 | NIST | |
| 412.1311 nm | 4400 | Co I | emission | 3p6.3d8.(3F).4s a 2F → 3p6.3d7.(4F).4s.4p.(3P*) z 2G* | 측정값 | NIST | |
| 516.315 nm | 4100 | Co II | emission | 3d7.(4F).4d e 3H → 3d7.(4F<7/2>).4f 2[13/2]* | 측정값 | NIST | |
| 521.43464 nm | 3900 | Co II | emission | 3d7.(4F).4d e 5H → 3d7.(4F<9/2>).4f 2[15/2]* | 측정값 | NIST | |
| 505.07089 nm | 3800 | Co II | emission | 3d7.(4F).4d e 5G → 3d7.(4F<9/2>).4f 2[13/2]* | 측정값 | NIST | |
| 517.06829 nm | 3200 | Co II | emission | 3d7.(4F).4d e 5H → 3d7.(4F<7/2>).4f 2[13/2]* | 측정값 | NIST | |
| 387.3955 nm | 2800 | Co I | emission | 3p6.3d8.(3F).4s b 4F → 3p6.3d7.(4F).4s.4p.(3P*) z 4D* | 측정값 | NIST | |
| 411.8767 nm | 2800 | Co I | emission | 3p6.3d8.(3F).4s a 2F → 3p6.3d7.(4F).4s.4p.(3P*) z 2G* | 측정값 | NIST | |
| 519.95128 nm | 2800 | Co II | emission | 3d7.(4F).4d e 3H → 3d7.(4F<5/2>).4f 2[11/2]* | 측정값 | NIST | |
| 513.56812 nm | 2700 | Co II | emission | 3d7.(4F).4d e 5H → 3d7.(4F<5/2>).4f 2[11/2]* | 측정값 | NIST | |
| 509.92115 nm | 2500 | Co II | emission | 3d7.(4F).4d e 3G → 3d7.(4F<7/2>).4f 2[11/2]* | 측정값 | NIST | |
| 523.11044 nm | 2300 | Co II | emission | 3d7.(4F).4d e 3H → 3d7.(4F<3/2>).4f 2[9/2]* | 측정값 | NIST | |
| 496.41682 nm | 2200 | Co II | emission | 3d7.(4F).4d f 5F → 3d7.(4F<9/2>).4f 2[11/2]* | 측정값 | NIST | |
| 505.7416 nm | 1700 | Co II | emission | 3d7.(4F).4d e 5G → 3d7.(4F<9/2>).4f 2[11/2]* | 측정값 | NIST | |
| 393.5959 nm | 1500 | Co I | emission | 3p6.3d8.(3F).4s a 2F → 3p6.3d8.(3F).4p y 4F* | 측정값 | NIST | |
| 384.2046 nm | 1400 | Co I | emission | 3p6.3d8.(3F).4s a 2F → 3p6.3d7.(4F).4s.4p.(3P*) z 2D* | 측정값 | NIST | |
| 509.52694 nm | 1400 | Co II | emission | 3d7.(4F).4d e 3G → 3d7.(4F<5/2>).4f 2[9/2]* | 측정값 | NIST | |
| 510.75362 nm | 1400 | Co II | emission | 3d7.(4F).4d e 5G → 3d7.(4F<7/2>).4f 2[9/2]* | 측정값 | NIST | |
| 506.70997 nm | 1200 | Co II | emission | 3d7.(4F).4d e 5P → 3d7.(4F<9/2>).4f 2[3/2]* | 측정값 | NIST | |
| 396.31 nm | 1100 | Co II | emission | 3d7.(4F).5p 5F* → 3d7.(4F).6d 5G | 측정값 | NIST | |
| 496.23566 nm | 1100 | Co II | emission | 3d7.(4F).4d f 5F → 3d7.(4F<9/2>).4f 2[9/2]* | 측정값 | NIST | |
| 517.6949 nm | 1100 | Co II | emission | 3d7.(4F).4d e 5G → 3d7.(4F<9/2>).4f 2[13/2]* | 측정값 | NIST | |
| 657.13038 nm | 1100 | Co II | emission | 3d7.(4F).5p 5G* → 3d7.(4F).5d 5H | 측정값 | NIST | |
| 657.62238 nm | 1100 | Co II | emission | 3d7.(4F).5p 3G* → 3d7.(4F).5d 3H | 측정값 | NIST | |
| 502.59107 nm | 990 | Co II | emission | 3d7.(4F).4d e 5D → 3d7.(4F<7/2>).4f 2[11/2]* | 측정값 | NIST | |
| 399.79 nm | 970 | Co I | emission | 3p6.3d8.(3F).4s a 2F → 3p6.3d8.(3F).4p * | 측정값 | NIST | |
| 512.9972 nm | 960 | Co II | emission | 3d7.(4F).4d e 3G → 3d7.(4F<3/2>).4f 2[9/2]* | 측정값 | NIST | |
| 743.9418 nm | 960 | Co II | emission | 3d7.(4F).5p 5D* → 3d7.(4F).6s 5F | 측정값 | NIST | |
| 637.37856 nm | 920 | Co II | emission | 3d7.(4F).5p 5F* → 3d7.(4F).5d 5G | 측정값 | NIST | |
| 495.82966 nm | 900 | Co II | emission | 3d7.(4F).4d f 5F → 3d7.(4F<9/2>).4f 2[11/2]* | 측정값 | NIST | |
| 502.25161 nm | 900 | Co II | emission | 3d7.(4F).4d e 3D → 3d7.(4F<3/2>).4f 2[7/2]* | 측정값 | NIST | |
| 642.58717 nm | 900 | Co II | emission | 3d7.(4F).5p 5F* → 3d7.(4F).5d 5F | 측정값 | NIST | |
| 510.45696 nm | 890 | Co II | emission | 3d7.(4F).4d e 5D → 3d7.(4F<5/2>).4f 2[9/2]* | 측정값 | NIST | |
| 502.36685 nm | 860 | Co II | emission | 3d7.(4F).4d f 5F → 3d7.(4F<9/2>).4f 2[9/2]* | 측정값 | NIST | |
| 620.5716 nm | 860 | Co II | emission | 3d7.(4F).5p 5D* → 3d7.(4F).5d 5F | 측정값 | NIST | |
| 409.2384 nm | 830 | Co I | emission | 3p6.3d8.(3F).4s a 2F → 3p6.3d7.(4F).4s.4p.(3P*) z 2F* | 측정값 | NIST | |
| 508.31892 nm | 780 | Co II | emission | 3d7.(4F).4d e 5D → 3d7.(4F<3/2>).4f 2[5/2]* | 측정값 | NIST | |
| 502.6664 nm | 680 | Co II | emission | 3d7.(4F).4d e 5G → 3d7.(4F<5/2>).4f 2[7/2]* | 측정값 | NIST | |
| 517.75201 nm | 680 | Co II | emission | 3d7.(4F).4d e 3H → 3d7.(4F<7/2>).4f 2[11/2]* | 측정값 | NIST | |
| 662.16287 nm | 680 | Co II | emission | 3d7.(4F).5p 3G* → 3d7.(4F).5d 3H | 측정값 | NIST | |
| 495.25711 nm | 670 | Co II | emission | 3d7.(4F).4d e 5G → 3d7.(4F<5/2>).4f 2[9/2]* | 측정값 | NIST | |
| 500.77152 nm | 640 | Co II | emission | 3d7.(4F).4d f 5F → 3d7.(4F<9/2>).4f 2[5/2]* | 측정값 | NIST | |
| 510.63945 nm | 640 | Co II | emission | 3d7.(4F).4d e 5D → 3d7.(4F<3/2>).4f 2[5/2]* | 측정값 | NIST | |
| 499.59719 nm | 600 | Co II | emission | 3d7.(4F).4d e 5H → 3d7.(4F<7/2>).4f 2[13/2]* | 측정값 | NIST | |
| 509.2051 nm | 600 | Co II | emission | 3d7.(4F).4d e 5D → 3d7.(4F<3/2>).4f 2[3/2]* | 측정값 | NIST | |
| 510.07741 nm | 600 | Co II | emission | 3d7.(4F).4d e 3G → 3d7.(4F<7/2>).4f 2[9/2]* | 측정값 | NIST |
확장 특성
공유 결합 반지름(확장)
- 공유 결합 반지름(Pyykkö)
- 111 pm
- 공유 결합 반지름(Pyykkö, 이중 결합)
- 103 pm
- 공유 결합 반지름(Pyykkö, 삼중 결합)
- 96 pm
- 공유 결합 반지름(Bragg)
- 137 pm
반데르발스 반지름
- Batsanov
- 200 pm
- Alvarez
- 240 pm
- UFF
- 287.2 pm
- MM3
- 223 pm
원자 및 금속 반지름
- 원자 반지름(Rahm)
- 233 pm
- 금속 반지름(C12)
- 125 pm
번호 척도
- Mendeleev
- 63
- Pettifor
- 64
- Glawe
- 70
전기 음성도 척도
- Ghosh
- 0
- Miedema
- 5
- Gunnarsson–Lundqvist
- 6
- Robles–Bartolotti
- 5
분극률 및 분산
- 쌍극자 분극률
- 55 a.u.
- 쌍극자 분극률(불확도)
- 4 a.u.
- C₆
- 408 Ha·Bohr6
- C₆ (Gould–Bučko)
- 461 Ha·Bohr6
화학 친화력
- 양성자 친화도
- 742.7 kJ/mol
- 기체상 염기성
- 719.8 kJ/mol
미데마 매개변수
- 미데마 몰 부피
- 6.7 cm3/mol
- 미데마 전자 밀도
- 5
공급 위험 및 경제성
- 생산 집중도
- 67
- 상대적 공급 위험
- 8
- 매장량 분포
- 45
- 정치적 안정성(최대 생산국)
- 3
- 정치적 안정성(최대 매장국)
- 3
상전이 및 동소체
| 녹는점 | 1768.15 K |
| 끓는점 | 3200.15 K |
산화 상태 분류
심화 참고 데이터
차폐 상수 (7)
| n | 오비탈 | σ |
|---|---|---|
| 1 | s | 0.6332 |
| 2 | p | 3.9076 |
| 2 | s | 7.595 |
| 3 | d | 15.1446 |
| 3 | p | 13.5654 |
| 3 | s | 12.6777 |
| 4 | s | 21.4236 |
결정 반지름 상세 정보 (9)
| 전하 | CN | 스핀 | rcrystal (pm) | 기원 |
|---|---|---|---|---|
| 2 | IV | HS | 72 | |
| 2 | V | 81 | calculated, | |
| 2 | VI | LS | 79 | from r^3 vs V plots, |
| 2 | VI | HS | 88.5 | from r^3 vs V plots, |
| 2 | VIII | 104 | ||
| 3 | VI | LS | 68.5 | from r^3 vs V plots, |
| 3 | VI | HS | 75 | |
| 4 | IV | 54 | ||
| 4 | VI | HS | 67 | from r^3 vs V plots, |
동위원소 붕괴 방식 (57)
| 동위원소 | 모드 | 세기 |
|---|---|---|
| 47 | p | — |
| 48 | p | — |
| 49 | p | — |
| 50 | B+ | 100% |
| 50 | B+p | 70.5% |
| 50 | 2p | — |
| 51 | B+ | 100% |
| 51 | B+p | 3.8% |
| 52 | B+ | 100% |
| 52 | B+p | — |
X선 산란 인자 (504)
| 에너지 (eV) | f₁ | f₂ |
|---|---|---|
| 10 | — | 1.42071 |
| 10.1617 | — | 1.45925 |
| 10.3261 | — | 1.49884 |
| 10.4931 | — | 1.53949 |
| 10.6628 | — | 1.58125 |
| 10.8353 | — | 1.62415 |
| 11.0106 | — | 1.6682 |
| 11.1886 | — | 1.71345 |
| 11.3696 | — | 1.75993 |
| 11.5535 | — | 1.80767 |
추가 데이터
Estimated Crustal Abundance
The estimated element abundance in the earth's crust.
2.5×101 milligrams per kilogram
참고 문헌 (1)
Estimated Oceanic Abundance
The estimated element abundance in the earth's oceans.
2×10-5 milligrams per liter
참고 문헌 (1)
Sources
Sources of this element.
Cobalt occurs in the minerals cobaltite, smaltite, and erythrite, and is often associated with nickel, silver, lead, copper, and iron ores, from which it is most frequently obtained as a by-product. It is also present in meteorites.
Important ore deposits are found in Zaire, Morocco, and Canada. The U.S. Geological Survey has announced that the bottom of the north central Pacific Ocean may have cobalt-rich deposits at relatively shallow depths in water close to the the Hawaiian Islands and other U.S. Pacific territories.
참고 문헌 (1)
- [6] Cobalt https://periodic.lanl.gov/27.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 Cobalt.
The element property data was retrieved from publications.