Strontium (Sr)
alkaline-earth-metalSolid
표준 원자량
87.62 u전자 배치
[Kr] 5s2녹는점
776.85 °C끓는점
1381.85 °C밀도
2640 kg/m³산화 상태
+1, +2전기 음성도(Pauling)
0.95제1 이온화 에너지
5.694867 eV발견 연도
1792원자 반지름
200 pm상세 정보
Strontium is an alkaline earth metal below calcium and above barium in group 2. Natural strontium is stable and occurs mainly as the minerals celestine and strontianite rather than as the free metal. Its chemistry is dominated by the Sr²⁺ ion, which closely resembles Ca²⁺ but is larger and more readily forms insoluble sulfate and carbonate salts. Strontium is best known technologically for red pyrotechnic colors, ferrite magnets, glass additives, and the radioactive isotope ⁹⁰Sr.
Strontium is softer than calcium and decomposes in water more vigorously. It does not absorb nitrogen below 380°C. It should be kept under kerosene to prevent oxidation. Freshly cut strontium has a silvery appearance, but rapidly turns a yellowish color with the formation of the oxide. The finely divided metal ignites spontaneously in air. Volatile strontium salts impart a beautiful crimson color to flames, and these salts are used in pyrotechnics and in the production of flares. Natural strontium is a mixture of four stable isotopes.
The name derives from Strontian, a town in Scotland. The mineral strontianite is found in mines in Strontian. The element was discovered in 1792 by the Scottish chemist and physician Thomas Charles Hope, who observed the brilliant red flame colour of strontium. It was first isolated by the English chemist Humphry Davy in 1808.
Strontium was discovered by Adair Crawford, an Irish chemist, in 1790 while studying the mineral witherite (BaCO3). When he mixed witherite with hydrochloric acid (HCl) he did not get the results he expected. He assumed that his sample of witherite was contaminated with an unknown mineral, a mineral he named strontianite (SrCO3). Strontium was first isolated by Sir Humphry Davy, an English chemist, in 1808 through the electrolysis of a mixture of strontium chloride (SrCl2) and mercuric oxide (HgO). Today, strontium is obtained from two of its most common ores, celestite (SrSO4) and strontianite (SrCO3), by treating them with hydrochloric acid, forming strontium chloride. The strontium chloride, usually mixed with potassium chloride (KCl), is then melted and electrolyzed, forming strontium and chlorine gas (Cl2).
Named after Strontian, a town in Scotland. Isolated by Davey by electrolysis in 1808, however, Adair Crawford recognized a new mineral (strontianite) as differing from other barium minerals in 1790.
Pure strontium is a soft, silvery metal when freshly cut, but it rapidly develops a yellowish or gray oxide-nitride surface film in air. It is less dense and less hard than many structural metals and is normally stored under oil or in sealed containers to limit reaction with moisture and oxygen.
Strontium nitrate, Sr(NO₃)₂, and related salts are used to produce intense red colors in fireworks, signal flares, and tracer compositions. Strontium carbonate, SrCO₃, is a feedstock for ceramic glazes, ferrite magnets, and specialty glass. Strontium ferrite materials are common permanent magnets in speakers, motors, and magnetic strips. ⁸⁷Sr/⁸⁶Sr ratios are used in geology, archaeology, and provenance studies. ⁹⁰Sr has been used in radioisotope power sources and industrial gauges, but its use is restricted by radiological hazards.
Most of the strontium produced today is used in the manufacture of color television picture tubes. It is also used to refine zinc and is combined with iron to make magnets.
Two strontium compounds, strontium carbonate (SrCO3) and strontium nitrate (Sr(NO3)2), burn with a bright, red flame and are used in fireworks and signal flares. Strontium carbonate is also used to make certain kinds of glass and is the base material for making most other strontium compounds.
Strontium-90, a radioactive isotope of strontium, is a common product of nuclear explosions. It has a half-life of about 28.8 years and decays into yttrium-90 through beta decay. Strontium-90 is especially deadly since it has a relatively long half-life, is strongly radioactive and is absorbed by the body, where it accumulates in the skeletal system. The radiation affects the production of new blood cells, which eventually leads to death.
In addition to the medical imaging application described in the image caption above, strontium has found use in producing ferrite magnets and in refining zinc. Strontium titanate is an interesting optical material as it has an extremely high refractive index and an optical dispersion greater than that of diamond. It has been used as a gemstone, but is very soft. It does not occur naturally.
Isotopes in Earth/Planetary Science
Stable isotopic fractionation of strontium is small because the relative differences between the masses of strontium stable isotopes are small (mass numbers are 86, 87, and 88 for the most abundant stable isotopes). Also, strontium is not subject to reduction-oxidation reactions in normal terrestrial environments, which would cause isotopic fractionation to be more evident. Nevertheless, current studies are exploring potential applications of stable strontium isotopic fractionation; for example, it has been used as a proxy for temperature during coral growth and for insights into the diets of ancient populations [295] A. Rüggeberg, J. Fietzke, V. Liebetrau, A. Eisenhauer, W. C. Dullo, A. Freiwald. Earth Planet. Sci. Lett.269, 570 (2008)., [296] K. J. Knudson, H. M. Williams, J. E. Buikstra, P. D. Tomczak, G. W. Gordon, A. D. Anbar. J. Archaeolog. Sci.37, 2352 (2010)..
The relative abundance of natural radiogenic 87Sr in seawater is related to the relative rates of processes that add or remove strontium in the ocean (seafloor spreading, mid-ocean-ridge hydrothermal activity, and continental weathering). Over geologic time, these processes have fluctuated and the isotope-amount ratio n(87Sr)/n(86Sr) has changed systematically. By measuring the n(87Sr)/n(86Sr) ratio in marine fossils of known age, it is possible to identify when such environmental changes occurred. Conversely, it is possible to estimate the ages of marine deposits by comparing measured n(87Sr)/n(86Sr) ratios with the global time chart; this process is known as strontium isotope stratigraphy [297] J. M. McArthur, R. J. Howarth, T. R. Bailey. J. Geol.109, 155 (2001)..
Isotopes in Forensic Science and Anthropology
The isotope-amount ratio n(87Sr)/n(86Sr) is highly variable in rocks, minerals, soils, and waters, and it can be transmitted to plants (Fig. IUPAC.38.1), animals, and manufactured materials. Measurements of n(87Sr)/n(86Sr) ratios are used for forensic applications in food authentication (determining where food came from), archaeology, crime-scene investigation, and human migration [298] B. L. Beard, C. M. Johnson. J. Forensic Sci.45, 1049 (2000)., [299] K. M. Frei, R. Frei. Appl. Geochem.26, 326 (2011)..
Isotopes in Geochronology
The 87Rb- 87Sr dating technique utilizes the fact that 87Sr is a product of radioactive 87Rb decay (half-life of 4.97×1010 years) and is a useful tool for determining ages of rocks and minerals spanning the age of the Earth (Fig. IUPAC.38.2) [301] G. Faure. Principles of Isotope Geology, 2nd Edition. p. 608. Wiley, New York (1986)..
Strontium almost always forms compounds in the +2 oxidation state. Strontium oxide, SrO, is a strongly basic oxide that reacts with water to form strontium hydroxide, Sr(OH)₂. Strontium carbonate, SrCO₃, and strontium sulfate, SrSO₄, are sparingly soluble and control much of its mineral behavior. Strontium chloride, SrCl₂, and strontium nitrate, Sr(NO₃)₂, are soluble salts used as chemical intermediates. Strontium titanate, SrTiO₃, is a high-refractive-index ceramic and an important substrate material in oxide electronics research.
Strontium is found chiefly as celestite and strontianite. The metal can be prepared by electrolysis of the fused chloride mixed with potassium chloride, or is made by reducing strontium oxide with aluminum in a vacuum at a temperature at which strontium distills off. Three allotropic forms of the metal exist, with transition points at 235 and 540°C.
See more information at the Strontium compound page.
Metallic strontium reacts with water and acids to release hydrogen, H₂, and can ignite as filings or powder. Soluble strontium salts have moderate chemical toxicity and can disturb calcium metabolism at high exposure. The main radiological concern is ⁹⁰Sr, a fission product that behaves partly like calcium in the body and irradiates bone and marrow through beta decay. Stable strontium in ordinary environmental concentrations is not highly hazardous.
Strontium is dispersed in rocks, soils, freshwater, and seawater, with higher mobility in soluble forms than barium but less than many alkali metals. It substitutes for calcium in minerals and biological hard tissues because Sr²⁺ and Ca²⁺ have similar charge and chemistry. Weathering releases strontium to waters, while carbonate, sulfate, and adsorption processes remove it. ⁹⁰Sr from nuclear fallout or accidents is environmentally important because it can enter food chains.
Commercial strontium is obtained chiefly from celestine, SrSO₄, which is converted to strontium carbonate, SrCO₃, or other salts before further use. Demand is concentrated in ferrite magnets, pyrotechnics, ceramics, and specialty glass, so the market is smaller and less diversified than for calcium or magnesium. Production of the metal itself is limited because most applications use compounds. Recycling is modest and usually indirect, for example through recovery or reuse of magnet-containing products rather than elemental strontium recovery.
Found in minerals celestite and strontianite.
Strontium is a trace element in the cosmos, produced mainly by neutron-capture processes in evolved stars and explosive stellar events. It is much less abundant than lighter rock-forming elements but is detectable in stellar spectra. In the solar system it follows calcium and other lithophile elements into silicate minerals, while only minute amounts occur in metallic phases or volatile reservoirs.
- The element is named after Strontian, a village in Scotland where strontianite was identified.
- Strontium salts give a cleaner crimson flame than many mixtures based on lithium or calcium.
- Strontium titanate was once used as a diamond simulant before harder simulants became common.
- Natural ⁸⁷Sr partly derives from the decay of ⁸⁷Rb, making Sr isotope ratios useful as geological clocks.
- Celestine is named for its pale blue color, although strontium compounds themselves are often white.
이미지
특성
물리적 특성
- 원자 반지름(경험값)
- 200 pm 모든 원소의 원자 반지름(경험값) 비교 →
- 공유 결합 반지름
- 195 pm 모든 원소의 공유 결합 반지름 비교 →
- 반데르발스 반지름
- 249 pm 모든 원소의 반데르발스 반지름 비교 →
- 금속 반지름
- 191 pm 모든 원소의 금속 반지름 비교 →
- 밀도
- 2640 kg/m³ 모든 원소의 밀도 비교 →
- 몰 부피
- 0.0337 L/mol
- STP에서의 상
- 고체 모든 원소의 STP에서의 상 비교 →
- 녹는점
- 776.85 °C 모든 원소의 녹는점 비교 →
- 끓는점
- 1381.85 °C 모든 원소의 끓는점 비교 →
- 비열
- 0.306 J/(g·K) 모든 원소의 비열 비교 →
- 몰 열용량
- 26.79 J/(mol·K) 모든 원소의 몰 열용량 비교 →
- 결정 구조
- 면심 입방 모든 원소의 결정 구조 비교 →
화학적 특성
- 전기 음성도(Pauling)
- 0.95 모든 원소의 전기 음성도(Pauling) 비교 →
- 전기 음성도(Allen)
- 0.963
- 전자 친화도
- 0.052 eV
- 제1 이온화 에너지
- 5.694867 eV 모든 원소의 제1 이온화 에너지 비교 →
- 제2 이온화 에너지
- 11.030314 eV 모든 원소의 제2 이온화 에너지 비교 →
- 제3 이온화 에너지
- 42.883678 eV 모든 원소의 제3 이온화 에너지 비교 →
- 제4 이온화 에너지
- 56.280194 eV 모든 원소의 제4 이온화 에너지 비교 →
- 제5 이온화 에너지
- 70.700243 eV 모든 원소의 제5 이온화 에너지 비교 →
- 산화 상태
- +1, +2 모든 원소의 산화 상태 비교 →
- 원자가 전자
- 2 모든 원소의 원자가 전자 비교 →
- 전자 배치
- [Kr] 5s2
열역학적 특성
- 융해열
- 0.08602373 eV 모든 원소의 융해열 비교 →
- 기화열
- 1.421983 eV 모든 원소의 기화열 비교 →
- 승화열
- 1.703892 eV
- 원자화열
- 1.703892 eV
- 원자화 엔탈피
- 1.699746 eV
핵 특성
- 양성자 수
- 38 모든 원소의 양성자 수 비교 →
- 중성자 수
- 50 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
- Sr-88
- 발견 연도
- 1792
존재비
- 존재비(지각)
- 370 mg/kg 모든 원소의 존재비(지각) 비교 →
- 존재비(해양)
- 7.9 mg/L 모든 원소의 존재비(해양) 비교 →
결정 구조
- 격자 상수 a
- 608 pm
전자 구조
- 전자껍질별 전자 수
- 2, 8, 18, 8, 2 모든 원소의 전자껍질별 전자 수 비교 →
식별자
- CAS 등록 번호
- 7440-24-6 모든 원소의 CAS 등록 번호 비교 →
- 항 기호
- 1S0
- InChI
- InChI=1S/Sr
- InChI 키
- CIOAGBVUUVVLOB-UHFFFAOYSA-N
전자 배치 측정값
Sr: 5s²[Kr] 5s²1s² 2s² 2p⁶ 3s² 3p⁶ 3d¹⁰ 4s² 4p⁶ 5s²원자 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 |
|---|---|---|---|
| 84 안정 | 83.9134191 ± 0.0000013 | 0.5600% | 안정 |
| 86 안정 | 85.9092606 ± 0.0000012 | 9.8600% | 안정 |
| 87 안정 | 86.9088775 ± 0.0000012 | 7.0000% | 안정 |
| 88 안정 | 87.9056125 ± 0.0000012 | 82.5800% | 안정 |
상 / 상태
이유: 녹는점(776.85 °C)보다 751.9 °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 38개 중 10개를 표시합니다. 이온 전하순으로 정렬되었습니다(오름차순).
보유 스펙트럼선 데이터 ?
| 이온 | 전하 | 총 스펙트럼선 수 | 전이 확률 | 준위 표기 |
|---|---|---|---|---|
| Sr I | 0 | 361 | 86 | 361 |
| Sr II | +1 | 135 | 33 | 135 |
| Sr III | +2 | 613 | 0 | 613 |
| Sr IV | +3 | 1183 | 0 | 1183 |
| Sr V | +4 | 625 | 0 | 625 |
| Sr VI | +5 | 57 | 14 | 57 |
| Sr VII | +6 | 30 | 30 | 30 |
| Sr VIII | +7 | 26 | 24 | 26 |
| Sr IX | +8 | 46 | 28 | 46 |
| Sr X | +9 | 54 | 51 | 54 |
보유 에너지 준위 데이터 ?
| 이온 | 전하 | 준위 |
|---|---|---|
| Sr I | 0 | 380 |
| Sr II | +1 | 72 |
| Sr III | +2 | 150 |
| Sr IV | +3 | 255 |
| Sr V | +4 | 144 |
| Sr VI | +5 | 22 |
| Sr VII | +6 | 20 |
| Sr VIII | +7 | 21 |
| Sr IX | +8 | 31 |
| Sr X | +9 | 47 |
이온 반지름
| 전하 | 배위 | 스핀 | 반지름 |
|---|---|---|---|
| +2 | 6 | 해당 없음 | 118 pm |
| +2 | 7 | 해당 없음 | 121 pm |
| +2 | 8 | 해당 없음 | 126 pm |
| +2 | 9 | 해당 없음 | 131 pm |
| +2 | 10 | 해당 없음 | 136 pm |
| +2 | 12 | 해당 없음 | 144 pm |
화합물
동위원소 (4)
Sixteen other unstable isotopes are known to exist. Of greatest importance is 90Sr with a half-life of 29 years. It is a product of nuclear fallout and presents a health problem. This isotope is one of the best long-lived high-energy beta emitters known, and is used in SNAP (Systems for Nuclear Auxilliary Power) devices. These devices hold promise for use in space vehicles, remote weather stations, navigational buoys, etc., and where a lightweight, long-lived, nuclear-electric power source is needed.
| 질량수 | 원자 질량(u) | 천연 존재비 | 반감기 | 붕괴 방식 | |
|---|---|---|---|---|---|
| 84 안정 | 83.9134191 ± 0.0000013 | 0.5600% ± 0.0100% | 안정 | stable | |
| 86 안정 | 85.9092606 ± 0.0000012 | 9.8600% ± 0.0100% | 안정 | stable | |
| 87 안정 | 86.9088775 ± 0.0000012 | 7.0000% ± 0.0100% | 안정 | stable | |
| 88 안정 | 87.9056125 ± 0.0000012 | 82.5800% ± 0.0100% | 안정 | stable |
스펙트럼선
전체 500개 중 50개를 표시합니다. 기본적으로 세기가 측정된 스펙트럼선만 표시됩니다.
| 파장(nm) | 세기 | 이온화 단계 | 유형 | 전이 | 정확도 | 출처 | |
|---|---|---|---|---|---|---|---|
| 707.0072 nm | 14000 | Sr I | emission | 5s.5p 3P* → 5s.6s 3S | 측정값 | NIST | |
| 687.83128 nm | 12000 | Sr I | emission | 5s.5p 3P* → 5s.6s 3S | 측정값 | NIST | |
| 679.10198 nm | 7000 | Sr I | emission | 5s.5p 3P* → 5s.6s 3S | 측정값 | NIST | |
| 525.68986 nm | 3400 | Sr I | emission | 5s.4d 3D → 4d.5p 3P* | 측정값 | NIST | |
| 640.8463 nm | 3100 | Sr I | emission | 5s.4d 3D → 4d.5p 3F* | 측정값 | NIST | |
| 483.20425 nm | 2900 | Sr I | emission | 5s.5p 3P* → 5s.5d 3D | 측정값 | NIST | |
| 548.08638 nm | 2700 | Sr I | emission | 5s.4d 3D → 4d.5p 3D* | 측정값 | NIST | |
| 496.2263 nm | 2500 | Sr I | emission | 5s.5p 3P* → 5s.5d 3D | 측정값 | NIST | |
| 481.18799 nm | 2300 | Sr I | emission | 5s.5p 3P* → 5p2 3P | 측정값 | NIST | |
| 689.25894 nm | 2300 | Sr I | emission | 5s2 1S → 5s.5p 3P* | 측정값 | NIST | |
| 650.3992 nm | 2100 | Sr I | emission | 5s.4d 3D → 4d.5p 3F* | 측정값 | NIST | |
| 523.85479 nm | 2000 | Sr I | emission | 5s.4d 3D → 4d.5p 3P* | 측정값 | NIST | |
| 550.4181 nm | 2000 | Sr I | emission | 5s.4d 3D → 4d.5p 3D* | 측정값 | NIST | |
| 496.5585 nm | 1900 | Sr I | emission | 5s.5p 1P* → 5s.7d 1D | 측정값 | NIST | |
| 516.5486 nm | 1800 | Sr I | emission | 5s.5p 1P* → 5s.8s 1S | 측정값 | NIST | |
| 478.43198 nm | 1700 | Sr I | emission | 5s.5p 3P* → 5p2 3P | 측정값 | NIST | |
| 552.1768 nm | 1700 | Sr I | emission | 5s.4d 3D → 4d.5p 3D* | 측정값 | NIST | |
| 730.94166 nm | 1700 | Sr I | emission | 5s.4d 1D → 4d.5p 1D* | 측정값 | NIST | |
| 472.22769 nm | 1600 | Sr I | emission | 5s.5p 3P* → 5p2 3P | 측정값 | NIST | |
| 474.19221 nm | 1600 | Sr I | emission | 5s.5p 3P* → 5p2 3P | 측정값 | NIST | |
| 478.3782 nm | 1500 | Sr I | emission | 5s.5p 1P* → 5s.9s 1S | 측정값 | NIST | |
| 487.249 nm | 1500 | Sr I | emission | 5s.5p 3P* → 5s.5d 3D | 측정값 | NIST | |
| 489.198 nm | 1500 | Sr I | emission | 5s.4d 3D → 5s.4f 3F* | 측정값 | NIST | |
| 581.67702 nm | 1500 | Sr I | emission | 5s.4d 1D → 4d.5p 3P* | 측정값 | NIST | |
| 468.8546 nm | 1400 | Sr I | emission | 5s.5p 1P* → 5s.8d 1D | 측정값 | NIST | |
| 522.21992 nm | 1400 | Sr I | emission | 5s.4d 3D → 4d.5p 3P* | 측정값 | NIST | |
| 522.51079 nm | 1400 | Sr I | emission | 5s.4d 3D → 4d.5p 3P* | 측정값 | NIST | |
| 522.92697 nm | 1400 | Sr I | emission | 5s.4d 3D → 4d.5p 3P* | 측정값 | NIST | |
| 555.6375 nm | 1400 | Sr I | emission | 5s.5p 1P* → 5s.6d 3D | 측정값 | NIST | |
| 634.57265 nm | 1400 | Sr I | emission | 5s.4d 3D → 5s.6p 3P* | 측정값 | NIST | |
| 655.0244 nm | 1400 | Sr I | emission | 5s.5p 1P* → 4d2 1D | 측정값 | NIST | |
| 495.6274 nm | 1300 | Sr I | emission | 5s.5p 1P* → 5s.7d 3D | 측정값 | NIST | |
| 638.64581 nm | 1300 | Sr I | emission | 5s.4d 3D → 5s.6p 3P* | 측정값 | NIST | |
| 485.50448 nm | 1200 | Sr I | emission | 5s.4d 3D → 5s.4f 3F* | 측정값 | NIST | |
| 486.87005 nm | 1200 | Sr I | emission | 5s.4d 3D → 5s.4f 3F* | 측정값 | NIST | |
| 487.60745 nm | 1200 | Sr I | emission | 5s.5p 3P* → 5s.5d 3D | 측정값 | NIST | |
| 496.7942 nm | 1200 | Sr I | emission | 5s.5p 3P* → 5s.5d 3D | 측정값 | NIST | |
| 559.8159 nm | 1200 | Sr I | emission | 5s.4d 1D → 4d.5p 1F* | 측정값 | NIST | |
| 458.29879 nm | 1100 | Sr I | emission | 5s.5p 1P* → 5s.10s 1S | 측정값 | NIST | |
| 486.91724 nm | 1100 | Sr I | emission | 5s.4d 3D → 5s.4f 3F* | 측정값 | NIST | |
| 489.2642 nm | 1100 | Sr I | emission | 5s.4d 3D → 5s.4f 3F* | 측정값 | NIST | |
| 661.72651 nm | 1100 | Sr I | emission | 5s.4d 3D → 4d.5p 3F* | 측정값 | NIST | |
| 403.03772 nm | 1000 | Sr I | emission | 5s.5p 3P* → 5s.6d 3D | 측정값 | NIST | |
| 443.8043 nm | 1000 | Sr I | emission | 5s.5p 3P* → 5s.7s 3S | 측정값 | NIST | |
| 446.32981 nm | 1000 | Sr I | emission | 5s.5p 1P* → 5s.11s 1S | 측정값 | NIST | |
| 453.2375 nm | 1000 | Sr I | emission | 5s.5p 1P* → 5s.9d 1D | 측정값 | NIST | |
| 471.2151 nm | 1000 | Sr I | emission | 5s.4d 1D → 5s.5f 3F* | 측정값 | NIST | |
| 545.08373 nm | 1000 | Sr I | emission | 5s.4d 3D → 4d.5p 3D* | 측정값 | NIST | |
| 548.6135 nm | 1000 | Sr I | emission | 5s.4d 3D → 4d.5p 3D* | 측정값 | NIST | |
| 553.4799 nm | 1000 | Sr I | emission | 5s.4d 3D → 4d.5p 3D* | 측정값 | NIST |
확장 특성
공유 결합 반지름(확장)
- 공유 결합 반지름(Pyykkö)
- 185 pm
- 공유 결합 반지름(Pyykkö, 이중 결합)
- 157 pm
- 공유 결합 반지름(Pyykkö, 삼중 결합)
- 139 pm
- 공유 결합 반지름(Bragg)
- 195 pm
반데르발스 반지름
- Truhlar
- 249 pm
- Batsanov
- 255 pm
- Alvarez
- 284 pm
- UFF
- 364.1 pm
- MM3
- 300 pm
원자 및 금속 반지름
- 원자 반지름(Rahm)
- 279 pm
- 금속 반지름(C12)
- 215 pm
번호 척도
- Mendeleev
- 8
- Pettifor
- 15
- Glawe
- 15
전기 음성도 척도
- Ghosh
- 0
- Miedema
- 2
- Gunnarsson–Lundqvist
- 3
- Robles–Bartolotti
- 2
분극률 및 분산
- 쌍극자 분극률
- 197.2 a.u.
- 쌍극자 분극률(불확도)
- 0.2 a.u.
- C₆
- 3175 Ha·Bohr6
- C₆ (Gould–Bučko)
- 3230 Ha·Bohr6
미데마 매개변수
- 미데마 몰 부피
- 33.93 cm3/mol
- 미데마 전자 밀도
- 1
공급 위험 및 경제성
- 생산 집중도
- 83
- 상대적 공급 위험
- 9
- 매장량 분포
- 100
- 정치적 안정성(최대 생산국)
- 24
- 정치적 안정성(최대 매장국)
- 24
상전이 및 동소체
| 녹는점 | 1050.15 K |
| 끓는점 | 1650.15 K |
산화 상태 분류
심화 참고 데이터
차폐 상수 (9)
| n | 오비탈 | σ |
|---|---|---|
| 1 | s | 0.8089 |
| 2 | p | 3.9696 |
| 2 | s | 10.0982 |
| 3 | d | 15.2738 |
| 3 | p | 15.8324 |
| 3 | s | 15.3362 |
| 4 | p | 26.068 |
| 4 | s | 24.5556 |
| 5 | s | 31.9295 |
결정 반지름 상세 정보 (6)
| 전하 | CN | 스핀 | rcrystal (pm) | 기원 |
|---|---|---|---|---|
| 2 | VI | 132 | ||
| 2 | VII | 135 | ||
| 2 | VIII | 140 | ||
| 2 | IX | 145 | ||
| 2 | X | 150 | calculated, | |
| 2 | XII | 158 | calculated, |
동위원소 붕괴 방식 (54)
| 동위원소 | 모드 | 세기 |
|---|---|---|
| 73 | B+ | 100% |
| 73 | B+p | 63% |
| 74 | B+ | 100% |
| 74 | B+p | — |
| 75 | B+ | 100% |
| 75 | B+p | 5.2% |
| 76 | B+ | 100% |
| 76 | B+p | 3.4% |
| 77 | B+ | 100% |
| 77 | B+p | 0.1% |
X선 산란 인자 (508)
| 에너지 (eV) | f₁ | f₂ |
|---|---|---|
| 10 | — | 0.17126 |
| 10.1617 | — | 0.1749 |
| 10.3261 | — | 0.17861 |
| 10.4931 | — | 0.1824 |
| 10.6628 | — | 0.18627 |
| 10.8353 | — | 0.19061 |
| 11.0106 | — | 0.19514 |
| 11.1886 | — | 0.19977 |
| 11.3696 | — | 0.2045 |
| 11.5535 | — | 0.20936 |
추가 데이터
Estimated Crustal Abundance
The estimated element abundance in the earth's crust.
3.70×102 milligrams per kilogram
참고 문헌 (1)
- [5] Strontium https://education.jlab.org/itselemental/ele038.html
Estimated Oceanic Abundance
The estimated element abundance in the earth's oceans.
7.9 milligrams per liter
참고 문헌 (1)
- [5] Strontium https://education.jlab.org/itselemental/ele038.html
Isotopes in Forensic Science and Anthropology
Information on the use of this element's isotopes in forensic science and anthropology.
The isotope-amount ratio n(87Sr)/n(86Sr) is highly variable in rocks, minerals, soils, and waters, and it can be transmitted to plants (Fig. IUPAC.38.1), animals, and manufactured materials. Measurements of n(87Sr)/n(86Sr) ratios are used for forensic applications in food authentication (determining where food came from), archaeology, crime-scene investigation, and human migration [298] B. L. Beard, C. M. Johnson. J. Forensic Sci.45, 1049 (2000)., [299] K. M. Frei, R. Frei. Appl. Geochem.26, 326 (2011)..
참고 문헌 (4)
- [298] B. L. Beard, C. M. Johnson. J. Forensic Sci.45, 1049 (2000).
- [299] K. M. Frei, R. Frei. Appl. Geochem.26, 326 (2011).
- [300] K. Miller, T. B. Coplen, M. Wieser. “Identification of the geographical origin of exotic wood species using 87Sr/86Sr isotope amount ratios”, in Goldschmidt 22nd Conference, Montreal, Quebec, Canada.
- [4] IUPAC Periodic Table of the Elements and Isotopes (IPTEI) https://doi.org/10.1515/pac-2015-0703
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 Strontium.
The element property data was retrieved from publications.