Cesium (Cs)
alkali-metalSolid
표준 원자량
132.905452 u전자 배치
[Xe] 6s1녹는점
28.44 °C끓는점
670.85 °C밀도
1930 kg/m³산화 상태
−1, +1전기 음성도(Pauling)
0.79제1 이온화 에너지
3.893906 eV발견 연도
1860원자 반지름
260 pm상세 정보
Cesium is a soft alkali metal with very low ionization energy and an unusually low melting point for a metal. It occurs naturally as the single stable isotope ¹³³Cs, chiefly in rare granitic pegmatite minerals. Chemically it is the heaviest stable group 1 element and forms almost exclusively Cs⁺ salts. Its best-known technological role is in the definition of the second, based on the microwave transition of the ¹³³Cs atom.
The metal is characterized by a spectrum containing two bright lines in the blue along with several others in the red, yellow, and green wavelengths. It is silvery white, soft, and ductile. It is the most electropositive and most alkaline element.
Cesium, gallium, and mercury are the only three metals that are liquid at room temperature. Cesium reacts explosively with cold water, and reacts with ice at temperatures above -116C. Cesium hydroxide, the strongest base known, attacks glass.
The name derives from the Latin caesius for "sky blue", which was the colour of the caesium line in the spectroscope. Caesium was discovered by the German chemist Robert Wilhelm Bunsen and the German physicist Gustav Robert Kirchhoff in 1860. It was first isolated by the German chemist Carl Setterberg in 1882.
Cesium was discovered by Robert Wilhelm Bunsen and Gustav Robert Kirchhoff, German chemists, in 1860 through the spectroscopic analysis of Durkheim mineral water. They named cesium after the blue lines they observed in its spectrum. Today, cesium is primarily obtained from the mineral pollucite (CsAlSi2O6). Obtaining pure cesium is difficult since cesium ores are frequently contaminated with rubidium, an element that is chemically similar to cesium. To obtain pure cesium, cesium and rubidium ores are crushed and heated with sodium metal to 650°C, forming an alloy that can then be separated with a process known as fractional distillation. Metallic cesium is too reactive to easily handle and is usually sold in the form of cesium azide (CsN3). Cesium is recovered from cesium azide by heating it.
From the Latin word caesius, sky blue. Cesium was discovered spectroscopically in 1860 by Bunsen and Kirchhoff in mineral water from Durkheim.
Pure cesium is a pale gold, silvery metal that is solid near ordinary room temperature but melts at about 28.5 °C. It is extremely soft and must be kept under dry inert gas, vacuum, or mineral oil because fresh surfaces tarnish and react rapidly with air or moisture.
Cesium vapor is used in atomic clocks and frequency standards, where ¹³³Cs provides a reproducible microwave reference. Cesium compounds are used in specialty photoemissive and scintillation materials, in some radiation detectors, and in high-density cesium formate brines for demanding oil and gas drilling operations. Radioactive ¹³⁷Cs has been used in industrial gauges, calibration sources, and radiotherapy, although many applications now use alternatives where security or disposal is difficult.
Cesium has the second lowest melting point of all metallic elements, which limits its uses. Cesium readily combines with oxygen and is used as a getter, a material that combines with and removes trace gases from vacuum tubes. Cesium is also used in atomic clocks, in photoelectric cells and as a catalyst in the hydrogenation of certain organic compounds. Since it is easily ionized and has a high mass, cesium ions may one day be used as a propellant in ion engines on spacecraft.
Cesium reacts violently with water and ice, forming cesium hydroxide (CsOH). Cesium hydroxide is the strongest base known and will attack glass. Cesium chloride (CsCl) and cesium nitrate (CsNO3) are cesium's most common compounds and are primarily used in the production of other chemicals.
Because of it has great affinity for oxygen, the metal is used as a "getter" in electron tubes. It is also used in photoelectric cells, as well as a catalyst in the hydrogenation of certain organic compounds.
The metal has recently found application in ion propulsion systems. Cesium is used in atomic clocks, which are accurate to 5 s in 300 years. Its chief compounds are the chloride and the nitrate.
Isotopes in Biology
137Cs (with a half-life of 30 years) can be used as a tracer in fungal mycelia (an extensive matrix of underground hyphae (stems of growth from a fungus)) to monitor the immobilization of this radioactive caesium isotope. After the nuclear reactor accident at Chernobyl, large quantities of 137Cs were released as fission products into the environment. Areas with large fungal populations and fungal mycelia seemed to immobilize the 137Cs isotope, which limited the spread of the radioactive isotope [399] S. N. Gray, J. Dighton, S. Olsson, D. H. Jennings. New Phytol.129, 449 (1995)., [400] J. Dighton, G. M. Clint, J. Poskitt. Mycol. Res.95, 1052 (1991)..
Isotopes in Earth/Planetary Science
River floodplains are an important site for storing suspended sediments and contaminants transferred from upstream catchments. 137Cs measurements of floodplain sediments provide a technique for estimating overbank sediment deposition, and it can provide information on spatial patterns of sediment deposition (Fig. IUPAC.55.1) [401] R. H. Gardner, W. W. Hargrove, D. A. Levine, S. M. Pearson, K. A. Rose. Spatial Analysis of Cesium in Sediments of Watts Bar Reservoir, Oak Ridge National Laboratory (2014), Feb. 27; http://research.esd.ornl.gov/CRERP/WATTSBAR/INDEX.HTM., [402] C. R. Olsen, I. L. Larson, P. D. Lowry, C. R. Moriones, C. J. Ford, K. C. Dearstone, R. R. Turner, B. L. Kimmel, C. C. Brandt. Transport and Accumulation of Cesium-137 and Mercury in the Clinch River and Watts Bar Reservoir system, ORNL/ER-7, Oak Ridge National Laboratory, Oak Ridge, TN (1992)., [403] D. E. Walling, Q. He. Catena29, 263 (1997)..
Isotopes in Geochronology
Nuclear fission of 235U (or other fissionable materials) yields 137Cs as a product. Although 137Cs is not naturally present in the environment, it can be collected from nuclear reactor processing and then used as an environmental tracer. 137Cs adheres tightly to porous sediments and will follow the movement of the sediment. By exposing sediments to 137Cs and allowing this combination to move dynamically, gamma ray spectrometry can then be used to measure the activity of 137Cs and monitor the movement of the radioactive sediments [404] W. G. Winn. J. Radioanal. Nucl. Chem.195, 345 (1995)., [405] A. V. Chesnokov, A. P. Govorun, F. V. N., O. P. Ivanov, V. I. Liksonov, V. N. Potapov, S. B. Shcherbak, S. V. Smirnov, L. I. Urutskoev. Nucl. Instrm. Methods Phys. Res. Section A: Accelerators, Spectrometers, Detectors and Associated Equipment.420, 336 (1999)., [406] A. Albrecht, R. Reiser, A. Lück, J. M. A. Stoll, W. Giger. Environ. Sci. Technol.32, 1882 (1998)..
137Cs dating of sediments not older than 60 years is useful in natural and artificial lakes and other environments because of its widespread production and release during atmospheric nuclear weapons testing, which began in the late 1940s, plus subsequent releases, such as during the accident at the Chernobyl nuclear reactor in April 1986. The 137Cs concentration profile in a sediment core can be matched with the historical record of 137Cs release to determine the approximate age profile of the sediment [406] A. Albrecht, R. Reiser, A. Lück, J. M. A. Stoll, W. Giger. Environ. Sci. Technol.32, 1882 (1998)., [407] M. S. Humphries, A. Kindness, W. N. Ellery, J. C. Hughes, C. R. Benitez-Nelson. Geomorphology119, 88 (2010)..
Isotopes in Industry
High-energy gamma rays from 137Cs serve as food irradiation devices to remove bacteria and other harmful microorganisms (living single celled organisms such as virus, algae and fungus) from food. Although 137Cs is not used commercially for large-scale food irradiation, it has been proposed that it can be used this way. Gamma rays from the radioactive 137Cs destroy the DNA of organisms to enable foods to last longer (i.e. irradiation of fruits and vegetables stops the ripening process) and be contamination free [408] D. W. Hayer. J. Food Quality13, 147 (1990)., [409] United States General Accounting Office. Food Irradiation: Available Research Indicates that Benefits Outweigh the Risks, GAO/RCED-00-217, GAO (2000)..
Cesium chemistry is dominated by the +1 oxidation state and by large, highly soluble salts. Cesium chloride (CsCl), cesium nitrate (CsNO₃), cesium carbonate (Cs₂CO₃), and cesium sulfate (Cs₂SO₄) are common laboratory compounds. Cesium hydroxide (CsOH) is a very strong base, and cesium fluoride (CsF) is valued as a fluoride source in some syntheses. The element forms oxides and superoxides, including cesium superoxide (CsO₂), when exposed to oxygen under suitable conditions.
See more information at the Cesium compound page.
Metallic cesium is highly reactive and can ignite or explode on contact with water, forming cesium hydroxide (CsOH) and hydrogen (H₂). Soluble cesium salts can be taken up by the body in ways broadly similar to potassium, so toxic or radioactive isotopes require strict control. ¹³⁷Cs is a significant gamma-emitting contamination hazard because it is mobile in many environments and has a half-life of about 30 years.
Natural cesium is a trace constituent of crustal rocks and is enriched in some pegmatites. In soils and sediments, Cs⁺ can be strongly fixed by clay minerals, especially at selective exchange sites, but mobility increases in low-clay or organic-rich settings. Fallout-derived ¹³⁷Cs is useful as an environmental tracer, while accidental releases can contaminate food chains through uptake by plants and animals.
Cesium is produced in small quantities compared with major industrial metals. The principal ore mineral is pollucite, a hydrated cesium aluminosilicate found in rare pegmatite deposits. Processing commonly converts ore to soluble cesium salts, from which metal or specialty compounds can be prepared. Demand is concentrated in specialized uses, so supply is shaped more by a few deposits, inventory management, and technical purity than by broad commodity trading. Recycling is limited, except for controlled recovery of sealed radioactive sources and some specialty materials.
Cesium, an alkali metal, occurs in lepidolite, pollucte (a hydrated silicate of aluminum and cesium), and in other sources. One of the world's richest sources of cesium is located at Bernic Lake, Manitoba. The deposits are estimated to contain 300,000 tons of pollucite, averaging 20% cesium.
It can be isolated by elecytrolysis of the fused cyanide and by a number of other methods. Very pure, gas-free cesium can be prepared by thermal decomposition of cesium azide.
Cesium is a rare element in cosmic terms. Its stable isotope ¹³³Cs is produced mainly by slow neutron-capture processes in evolved stars, with contributions from other neutron-rich nucleosynthesis pathways. In planetary materials it behaves as an incompatible, lithophile alkali element, tending to concentrate in late-stage melts rather than in common rock-forming minerals.
- Cesium is one of the few metals that can melt in a warm hand, though handling it that way would be dangerous.
- The official SI second is defined using a hyperfine transition of neutral ¹³³Cs.
- Pollucite is important because cesium has few concentrated ore minerals.
- Cesium salts often make dense solutions because the Cs⁺ ion is very heavy.
- The name comes from the blue spectral lines observed when the element was discovered.
이미지
특성
물리적 특성
- 원자 반지름(경험값)
- 260 pm 모든 원소의 원자 반지름(경험값) 비교 →
- 공유 결합 반지름
- 244 pm 모든 원소의 공유 결합 반지름 비교 →
- 반데르발스 반지름
- 343 pm 모든 원소의 반데르발스 반지름 비교 →
- 금속 반지름
- 235 pm 모든 원소의 금속 반지름 비교 →
- 밀도
- 1930 kg/m³ 모든 원소의 밀도 비교 →
- 몰 부피
- 0.07 L/mol
- STP에서의 상
- 고체 모든 원소의 STP에서의 상 비교 →
- 녹는점
- 28.44 °C 모든 원소의 녹는점 비교 →
- 끓는점
- 670.85 °C 모든 원소의 끓는점 비교 →
- 열전도율
- 35.9 W/(m·K) 모든 원소의 열전도율 비교 →
- 비열
- 0.242 J/(g·K) 모든 원소의 비열 비교 →
- 몰 열용량
- 32.21 J/(mol·K) 모든 원소의 몰 열용량 비교 →
- 결정 구조
- 체심 입방 모든 원소의 결정 구조 비교 →
화학적 특성
- 전기 음성도(Pauling)
- 0.79 모든 원소의 전기 음성도(Pauling) 비교 →
- 전기 음성도(Allen)
- 0.659
- 전자 친화도
- 0.4716 eV
- 제1 이온화 에너지
- 3.893906 eV 모든 원소의 제1 이온화 에너지 비교 →
- 제2 이온화 에너지
- 23.15753 eV 모든 원소의 제2 이온화 에너지 비교 →
- 제3 이온화 에너지
- 33.195114 eV 모든 원소의 제3 이온화 에너지 비교 →
- 제4 이온화 에너지
- 43.000148 eV 모든 원소의 제4 이온화 에너지 비교 →
- 제5 이온화 에너지
- 56.000193 eV 모든 원소의 제5 이온화 에너지 비교 →
- 산화 상태
- −1, +1 모든 원소의 산화 상태 비교 →
- 원자가 전자
- 1 모든 원소의 원자가 전자 비교 →
- 전자 배치
- [Xe] 6s1
열역학적 특성
- 임계점(온도)
- 1665 °C
- 임계점(압력)
- 9.4e+6 Pa
- 융해열
- 0.0216614 eV 모든 원소의 융해열 비교 →
- 기화열
- 0.67367985 eV 모든 원소의 기화열 비교 →
- 승화열
- 0.79286936 eV
- 원자화열
- 0.79286936 eV
- 원자화 엔탈피
- 0.79286936 eV
핵 특성
- 양성자 수
- 55 모든 원소의 양성자 수 비교 →
- 중성자 수
- 78 모든 원소의 중성자 수 비교 →
- 알려진 동위원소 수
- 42 모든 원소의 알려진 동위원소 수 비교 →
- 안정 동위원소 수
- 1 모든 원소의 안정 동위원소 수 비교 →
- 가장 안정한 동위원소
- Cs-133
- 발견 연도
- 1860
존재비
- 존재비(지각)
- 3 mg/kg 모든 원소의 존재비(지각) 비교 →
- 존재비(해양)
- 3 × 10−4 mg/L 모든 원소의 존재비(해양) 비교 →
결정 구조
- 격자 상수 a
- 605 pm
전자 구조
- 전자껍질별 전자 수
- 2, 8, 18, 18, 8, 1 모든 원소의 전자껍질별 전자 수 비교 →
식별자
- CAS 등록 번호
- 7440-46-2 모든 원소의 CAS 등록 번호 비교 →
- 항 기호
- 2S1/2
- InChI
- InChI=1S/Cs
- InChI 키
- TVFDJXOCXUVLDH-UHFFFAOYSA-N
전자 배치 측정값
Cs: 6s¹[Xe] 6s¹1s² 2s² 2p⁶ 3s² 3p⁶ 3d¹⁰ 4s² 4p⁶ 4d¹⁰ 5s² 5p⁶ 6s¹원자 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 |
|---|---|---|---|
| 133 안정 | 132.905451961 ± 0.000000008 | 100.0000% | 안정 |
상 / 상태
이유: 녹는점(28.44 °C)보다 3.4 °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
심화
원자 스펙트럼
전체 55개 중 10개를 표시합니다. 이온 전하순으로 정렬되었습니다(오름차순).
보유 스펙트럼선 데이터 ?
| 이온 | 전하 | 총 스펙트럼선 수 | 전이 확률 | 준위 표기 |
|---|---|---|---|---|
| Cs I | 0 | 230 | 42 | 228 |
| Cs II | +1 | 1757 | 2 | 1737 |
| Cs III | +2 | 1010 | 1010 | 1010 |
| Cs IV | +3 | 207 | 0 | 207 |
| Cs V | +4 | 143 | 0 | 143 |
| Cs VI | +5 | 67 | 0 | 67 |
| Cs VII | +6 | 185 | 0 | 185 |
| Cs VIII | +7 | 111 | 13 | 111 |
| Cs IX | +8 | 50 | 16 | 50 |
| Cs X | +9 | 86 | 86 | 86 |
보유 에너지 준위 데이터 ?
| 이온 | 전하 | 준위 |
|---|---|---|
| Cs I | 0 | 179 |
| Cs II | +1 | 316 |
| Cs III | +2 | 174 |
| Cs IV | +3 | 116 |
| Cs V | +4 | 50 |
| Cs VI | +5 | 32 |
| Cs VII | +6 | 79 |
| Cs VIII | +7 | 55 |
| Cs IX | +8 | 69 |
| Cs X | +9 | 79 |
이온 반지름
| 전하 | 배위 | 스핀 | 반지름 |
|---|---|---|---|
| +1 | 6 | 해당 없음 | 167 pm |
| +1 | 8 | 해당 없음 | 174 pm |
| +1 | 9 | 해당 없음 | 178 pm |
| +1 | 10 | 해당 없음 | 181 pm |
| +1 | 11 | 해당 없음 | 185 pm |
| +1 | 12 | 해당 없음 | 188 pm |
화합물
동위원소 (1)
Cesium has more isotopes than any element32with masses ranging from 114 to 145.
| 질량수 | 원자 질량(u) | 천연 존재비 | 반감기 | 붕괴 방식 | |
|---|---|---|---|---|---|
| 133 안정 | 132.905451961 ± 0.000000008 | 100.0000% | 안정 | stable |
스펙트럼선
전체 728개 중 50개를 표시합니다. 기본적으로 세기가 측정된 스펙트럼선만 표시됩니다.
| 파장(nm) | 세기 | 이온화 단계 | 유형 | 전이 | 정확도 | 출처 | |
|---|---|---|---|---|---|---|---|
| 460.37908 nm | 10000000 | Cs II | emission | 5p5.(2P*<3/2>).6s 2[3/2]* → 5p5.(2P*<3/2>).6p 2[5/2] | 측정값 | NIST | |
| 522.70372 nm | 7500000 | Cs II | emission | 5p5.(2P*<3/2>).6s 2[3/2]* → 5p5.(2P*<3/2>).6p 2[1/2] | 측정값 | NIST | |
| 592.56312 nm | 5100000 | Cs II | emission | 5p5.(2P*<3/2>).5d 2[7/2]* → 5p5.(2P*<3/2>).6p 2[5/2] | 측정값 | NIST | |
| 556.3024 nm | 3900000 | Cs II | emission | 5p5.(2P*<3/2>).5d 2[3/2]* → 5p5.(2P*<3/2>).6p 2[3/2] | 측정값 | NIST | |
| 495.28523 nm | 3700000 | Cs II | emission | 5p5.(2P*<3/2>).5d 2[1/2]* → 5p5.(2P*<3/2>).6p 2[5/2] | 측정값 | NIST | |
| 695.54998 nm | 3700000 | Cs II | emission | 5p5.(2P*<3/2>).5d 2[7/2]* → 5p5.(2P*<3/2>).6p 2[5/2] | 측정값 | NIST | |
| 524.93849 nm | 2900000 | Cs II | emission | 5p5.(2P*<3/2>).6s 2[3/2]* → 5p5.(2P*<3/2>).6p 2[3/2] | 측정값 | NIST | |
| 504.38026 nm | 2700000 | Cs II | emission | 5p5.(2P*<3/2>).6s 2[3/2]* → 5p5.(2P*<3/2>).6p 2[3/2] | 측정값 | NIST | |
| 483.01864 nm | 2500000 | Cs II | emission | 5p5.(2P*<3/2>).6s 2[3/2]* → 5p5.(2P*<3/2>).6p 2[5/2] | 측정값 | NIST | |
| 583.11404 nm | 2400000 | Cs II | emission | 5p5.(2P*<3/2>).6s 2[3/2]* → 5p5.(2P*<3/2>).6p 2[5/2] | 측정값 | NIST | |
| 537.09876 nm | 2200000 | Cs II | emission | 5p5.(2P*<3/2>).5d 2[1/2]* → 5p5.(2P*<3/2>).6p 2[1/2] | 측정값 | NIST | |
| 452.67416 nm | 2000000 | Cs II | emission | 5p5.(2P*<3/2>).5d 2[1/2]* → 5p5.(2P*<3/2>).6p 2[3/2] | 측정값 | NIST | |
| 487.00392 nm | 1900000 | Cs II | emission | 5p5.(2P*<1/2>).6s 2[1/2]* → 5p5.(2P*<1/2>).6p 2[3/2] | 측정값 | NIST | |
| 427.71303 nm | 1800000 | Cs II | emission | 5p5.(2P*<3/2>).6s 2[3/2]* → 5p5.(2P*<3/2>).6p 2[3/2] | 측정값 | NIST | |
| 697.96684 nm | 1600000 | Cs II | emission | 5p5.(2P*<3/2>).5d 2[5/2]* → 5p5.(2P*<3/2>).6p 2[3/2] | 측정값 | NIST | |
| 426.470255 nm | 1400000 | Cs II | emission | 5p5.(2P*<3/2>).6p 2[5/2] → 5p5.(2P*<3/2>).6d 2[7/2]* | 측정값 | NIST | |
| 721.9603 nm | 1400000 | Cs III | emission | 5s2.5p5 2P* → 5s2.5p5 2P* | 측정값 | NIST | |
| 714.95415 nm | 1300000 | Cs II | emission | 5p5.(2P*<1/2>).5d 2[5/2]* → 5p5.(2P*<1/2>).6p 2[3/2] | 측정값 | NIST | |
| 450.15517 nm | 1200000 | Cs II | emission | 5p5.(2P*<3/2>).6s 2[3/2]* → 5p5.(2P*<3/2>).6p 2[1/2] | 측정값 | NIST | |
| 527.40539 nm | 1100000 | Cs II | emission | 5p5.(2P*<3/2>).5d 2[1/2]* → 5p5.(2P*<3/2>).6p 2[1/2] | 측정값 | NIST | |
| 534.91319 nm | 1000000 | Cs II | emission | 5p5.(2P*<1/2>).6s 2[1/2]* → 5p5.(2P*<1/2>).6p 2[3/2] | 측정값 | NIST | |
| 653.6445 nm | 1000000 | Cs II | emission | 5p5.(2P*<3/2>).5d 2[3/2]* → 5p5.(2P*<3/2>).6p 2[5/2] | 측정값 | NIST | |
| 612.86072 nm | 980000 | Cs II | emission | 5p5.(2P*<3/2>).5d 2[3/2]* → 5p5.(2P*<3/2>).6p 2[5/2] | 측정값 | NIST | |
| 672.44659 nm | 960000 | Cs II | emission | 5p5.(2P*<1/2>).5d 2[5/2]* → 5p5.(2P*<1/2>).6p 2[3/2] | 측정값 | NIST | |
| 664.65663 nm | 880000 | Cs II | emission | 5p5.(2P*<1/2>).5d 2[3/2]* → 5p5.(2P*<1/2>).6p 2[1/2] | 측정값 | NIST | |
| 400.65447 nm | 860000 | Cs III | emission | 5s2.5p4.(3P<2>).6s 2[2] → 5s2.5p4.(3P<2>).6p 2[3]* | 측정값 | NIST | |
| 649.55329 nm | 830000 | Cs II | emission | 5p5.(2P*<3/2>).5d 2[7/2]* → 5p5.(2P*<3/2>).6p 2[5/2] | 측정값 | NIST | |
| 497.25963 nm | 820000 | Cs II | emission | 5p5.(2P*<3/2>).6p 2[5/2] → 5p5.(2P*<3/2>).7s 2[3/2]* | 측정값 | NIST | |
| 403.985602 nm | 800000 | Cs II | emission | 5p5.(2P*<3/2>).6p 2[5/2] → 5p5.(2P*<3/2>).6d 2[7/2]* | 측정값 | NIST | |
| 436.329875 nm | 760000 | Cs II | emission | 5p5.(2P*<3/2>).6p 2[3/2] → 5p5.(2P*<3/2>).6d 2[5/2]* | 측정값 | NIST | |
| 388.83763 nm | 740000 | Cs III | emission | 5s2.5p4.(3P<1>).5d 2[3] → 5s2.5p4.(3P<2>).6p 2[3]* | 측정값 | NIST | |
| 441.02226 nm | 720000 | Cs III | emission | 5s2.5p4.(3P<2>).5d 2[3] → 5s2.5p4.(3P<2>).6p 2[2]* | 측정값 | NIST | |
| 450.67197 nm | 720000 | Cs III | emission | 5s2.5p4.(3P<2>).5d 2[3] → 5s2.5p4.(3P<2>).6p 2[2]* | 측정값 | NIST | |
| 476.36362 nm | 700000 | Cs II | emission | 5p5.(2P*<1/2>).6s 2[1/2]* → 5p5.(2P*<1/2>).6p 2[1/2] | 측정값 | NIST | |
| 520.95813 nm | 650000 | Cs II | emission | 5p5.(2P*<1/2>).6s 2[1/2]* → 5p5.(2P*<1/2>).6p 2[3/2] | 측정값 | NIST | |
| 392.55957 nm | 620000 | Cs III | emission | 5s2.5p4.(3P<2>).5d 2[3] → 5s2.5p4.(3P<2>).6p 2[3]* | 측정값 | NIST | |
| 442.56759 nm | 560000 | Cs III | emission | 5s2.5p4.(3P<2>).6s 2[2] → 5s2.5p4.(3P<2>).6p 2[2]* | 측정값 | NIST | |
| 428.837507 nm | 510000 | Cs II | emission | 5p5.(2P*<3/2>).6p 2[3/2] → 5p5.(2P*<3/2>).6d 2[5/2]* | 측정값 | NIST | |
| 488.00516 nm | 490000 | Cs II | emission | 5p5.(2P*<1/2>).6s 2[1/2]* → 5p5.(2P*<1/2>).6p 2[1/2] | 측정값 | NIST | |
| 581.41641 nm | 450000 | Cs II | emission | 5p5.(2P*<3/2>).5d 2[3/2]* → 5p5.(2P*<3/2>).6p 2[3/2] | 측정값 | NIST | |
| 395.95055 nm | 420000 | Cs II | emission | 5p5.(2P*<3/2>).5d 2[1/2]* → 5p5.(2P*<3/2>).6p 2[1/2] | 측정값 | NIST | |
| 461.61693 nm | 420000 | Cs II | emission | 5p5.(2P*<1/2>).6s 2[1/2]* → 5p5.(2P*<1/2>).6p 2[1/2] | 측정값 | NIST | |
| 453.896566 nm | 410000 | Cs II | emission | 5p5.(2P*<3/2>).6p 2[3/2] → 5p5.(2P*<3/2>).6d 2[3/2]* | 측정값 | NIST | |
| 440.525568 nm | 390000 | Cs II | emission | 5p5.(2P*<3/2>).6p 2[1/2] → 5p5.(2P*<3/2>).7s 2[3/2]* | 측정값 | NIST | |
| 437.30356 nm | 370000 | Cs II | emission | 5p5.(2P*<3/2>).5d 2[1/2]* → 5p5.(2P*<3/2>).6p 2[3/2] | 측정값 | NIST | |
| 452.28578 nm | 350000 | Cs III | emission | 5s2.5p4.(3P<2>).6s 2[2] → 5s2.5p4.(3P<2>).6p 2[2]* | 측정값 | NIST | |
| 389.698641 nm | 340000 | Cs II | emission | 5p5.(2P*<3/2>).6p 2[1/2] → 5p5.(2P*<3/2>).6d 2[1/2]* | 측정값 | NIST | |
| 404.34262 nm | 310000 | Cs III | emission | 5s2.5p4.(1D<2>).6s 2[2] → 5s2.5p4.(1D<2>).6p 2[3]* | 측정값 | NIST | |
| 645.6318 nm | 310000 | Cs III | emission | 5s2.5p4.(3P<2>).7p 2[3]* → 5s2.5p4.(3P<2>).7d 2[4] | 측정값 | NIST | |
| 607.9854 nm | 300000 | Cs III | emission | 5s2.5p4.(3P<2>).5f 2[2]* → 5s2.5p4.(3P<2>).5g 2[3] | 측정값 | NIST |
확장 특성
공유 결합 반지름(확장)
- 공유 결합 반지름(Pyykkö)
- 232 pm
- 공유 결합 반지름(Pyykkö, 이중 결합)
- 209 pm
- 공유 결합 반지름(Bragg)
- 237 pm
반데르발스 반지름
- Truhlar
- 343 pm
- Batsanov
- 300 pm
- Alvarez
- 348 pm
- UFF
- 451.7 pm
- MM3
- 344 pm
원자 및 금속 반지름
- 원자 반지름(Rahm)
- 249 pm
- 금속 반지름(C12)
- 267 pm
번호 척도
- Mendeleev
- 5
- Pettifor
- 8
- Glawe
- 8
전기 음성도 척도
- Ghosh
- 0
- Miedema
- 2
- Gunnarsson–Lundqvist
- 2
- Robles–Bartolotti
- 1
분극률 및 분산
- 쌍극자 분극률
- 400.9 a.u.
- 쌍극자 분극률(불확도)
- 0.7 a.u.
- C₆ (Gould–Bučko)
- 6660 Ha·Bohr6
미데마 매개변수
- 미데마 몰 부피
- 69.23 cm3/mol
- 미데마 전자 밀도
- 0
상전이 및 동소체
| 녹는점 | 301.65 K |
| 끓는점 | 944.15 K |
| 임계점(온도) | 1938.15 K |
| 임계점(압력) | 9.4 MPa |
산화 상태 분류
심화 참고 데이터
차폐 상수 (12)
| n | 오비탈 | σ |
|---|---|---|
| 1 | s | 1.0957 |
| 2 | p | 4.1804 |
| 2 | s | 14.4884 |
| 3 | d | 14.0194 |
| 3 | p | 18.4222 |
| 3 | s | 18.6226 |
| 4 | d | 32.1616 |
| 4 | p | 29.1424 |
| 4 | s | 27.9576 |
| 5 | p | 41.349 |
결정 반지름 상세 정보 (6)
| 전하 | CN | 스핀 | rcrystal (pm) | 기원 |
|---|---|---|---|---|
| 1 | VI | 181 | ||
| 1 | VIII | 188 | ||
| 1 | IX | 192 | ||
| 1 | X | 195 | ||
| 1 | XI | 199 | ||
| 1 | XII | 202 |
동위원소 붕괴 방식 (74)
| 동위원소 | 모드 | 세기 |
|---|---|---|
| 111 | p | — |
| 112 | p | 100% |
| 112 | A | 0.3% |
| 113 | p | 100% |
| 114 | B+ | 100% |
| 114 | A | 0% |
| 114 | B+p | 8.7% |
| 114 | B+A | 0.2% |
| 115 | B+ | 100% |
| 115 | B+p | 0.1% |
X선 산란 인자 (508)
| 에너지 (eV) | f₁ | f₂ |
|---|---|---|
| 10 | — | 0.04294 |
| 10.1617 | — | 0.04199 |
| 10.3261 | — | 0.04106 |
| 10.4931 | — | 0.04015 |
| 10.6628 | — | 0.03925 |
| 10.8353 | — | 0.03838 |
| 11.0106 | — | 0.04186 |
| 11.1886 | — | 0.04987 |
| 11.3696 | — | 0.06291 |
| 11.5535 | — | 0.06823 |
추가 데이터
Estimated Crustal Abundance
The estimated element abundance in the earth's crust.
3 milligrams per kilogram
참고 문헌 (1)
Estimated Oceanic Abundance
The estimated element abundance in the earth's oceans.
3×10-4 milligrams per liter
참고 문헌 (1)
Sources
Sources of this element.
Cesium, an alkali metal, occurs in lepidolite, pollucte (a hydrated silicate of aluminum and cesium), and in other sources. One of the world's richest sources of cesium is located at Bernic Lake, Manitoba. The deposits are estimated to contain 300,000 tons of pollucite, averaging 20% cesium.
It can be isolated by elecytrolysis of the fused cyanide and by a number of other methods. Very pure, gas-free cesium can be prepared by thermal decomposition of cesium azide.
참고 문헌 (1)
- [6] Cesium https://periodic.lanl.gov/55.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 Cesium.
The element property data was retrieved from publications.