Tellurium (Te)
metalloidSolid
표준 원자량
127.6 u전자 배치
[Kr] 5s2 4d10 5p4녹는점
449.51 °C끓는점
987.85 °C밀도
6232 kg/m³산화 상태
−2, −1, 0, +1, +2, +3, +4, +5, +6전기 음성도(Pauling)
2.1제1 이온화 에너지
9.009808 eV발견 연도
1782원자 반지름
140 pm상세 정보
Tellurium is a brittle metalloid in group 16, below selenium and above polonium. It is chemically related to sulfur and selenium but is more metallic, less abundant, and more easily reduced. In nature it occurs mainly as telluride minerals and as a minor constituent of copper ores. Its technological importance comes from semiconducting and thermoelectric compounds, cadmium telluride photovoltaics, and small alloying additions that modify machinability and corrosion behavior.
Crystalline tellurium has a silvery-white appearance, and when pure it exhibits a metallic luster. It is brittle and easily pulverized. Amorphous tellurium is found by precipitating tellurium from a solution of telluric or tellurous acid. Whether this form is truly amorphous, or made of minute crystals, is open to question. Tellurium is a p-type semiconductor, and shows greater conductivity in certain directions, depending on alignment of the atoms.
Its conductivity increases slightly with exposure to light. It can be doped with silver, copper, gold, tin, or other elements. In air, tellurium burns with a greenish-blue flames, forming the dioxide. Molten tellurium corrodes iron, copper, and stainless steel.
The name derives from the Latin Tellus, who was the Roman goddess of the Earth. Tellurium was discovered by Franz Joseph Müller von Reichenstein in 1782 and overlooked for 15 years until it was isolated by the German chemist Martin-Heinrich Klaproth in 1798. The Hungarian chemist Paul Kitaibel independently discovered tellurium in 1789, prior to Klaproth's work but after von Reichenstein.
Tellurium was discovered by Franz Joseph Müller von Reichenstein, a Romanian mining official, in 1782. Reichenstein was the chief inspector of all mines, smelters and saltworks in Transylvania. He also had an interest in chemistry and extracted a new metal from an ore of gold, known as aurum album, which he believed was antimony. He shortly realized that the metal he had produced wasn't antimony at all, but a previously unknown element. Reichenstein's work was forgotten until 1798 when Martin Heinrich Klaproth, a German chemist, mentioned the substance in a paper. Klaproth named the new element tellurium but gave full credit for its discovery to Reichenstein. Tellurium is found free in nature, but is most often found in the ores sylvanite (AgAuTe4), calaverite (AuTe2) and krennerite (AuTe2). Today, most tellurium is obtained as a byproduct of mining and refining copper.
From the Latin word tellus, earth. Discovered by Muller von Reichenstein in 1782; named by Klaproth, who isolated it in 1798.
Pure tellurium is a silvery-white to gray, lustrous, crystalline solid at ordinary conditions. It is brittle and can be powdered, but it is not malleable. The common trigonal form has helical chains of atoms, giving the element anisotropic electrical and thermal properties.
The largest modern use of tellurium is in cadmium telluride, CdTe, thin-film solar cells. Tellurium is also used in bismuth telluride, Bi₂Te₃, and related thermoelectric materials for cooling and power generation from temperature differences. Small additions to copper, steel, and lead improve machinability or modify mechanical properties. Tellurium compounds are used in some infrared optical materials, phase-change chalcogenide systems, and specialized vulcanization and glass applications, but these uses are smaller and material-specific.
Tellurium is a semiconductor and is frequently doped with copper, tin, gold or silver. Tellurium is also used to color glass and ceramics and is one of the primary ingredients in blasting caps.
Tellurium is primarily used as an alloying agent. Small amounts of tellurium are added to copper and stainless steel to make them easier to machine and mill. Tellurium is also added to lead to increase its strength and resistance to sulfuric acid (H2SO4).
Tellurium forms many compounds, but none that are commercially important. They include: tellourous acid (H2TeO2), tellurium tetrachloride (TeCl4), tellurium dichloride (TeCl2), tellurium trioxide (TeO3), tellurium monoxide (TeO) and sodium telluride (Na2Te).
Tellurium improves the machinability of copper and stainless steel, and its addition to lead decreases the corrosive action of sulfuric acid on lead and improves its strength and hardness. Tellurium is used as a basic ingredient in blasting caps, and is added to cast iron for chill control. Tellurium is used in ceramics. Bismuth telluride has been used in thermoelectric devices.
Isotopes in Earth/Planetary Science
Tellurium isotopes are a mixture of r-process, s-process, and p-process nucleosynthesis products, making them useful for studying the contribution of stellar products to the molecular cloud from which the Sun and planets were formed (Fig. IUPAC.52.1) [378] M. Fehr. Tellurium Isotopes and their Applications in Cosmo- and Geochemistry, Swiss Federal Institute of Technology Zurich (2014), Feb. 26; http://e-collection.library.ethz.ch/eserv/eth:27380/eth-27380-01.pdf., [379] M. A. Fehr, M. Rehkämper, D. Porcelli, A. N. Halliday. Homogeneity of Tellurium Isotopes in Chondrites, Leachates of Allende and Canyon Diablo, Lunar and Planetary Science (2014), Feb. 26; http://www.lpi.usra.edu/meetings/lpsc2003/pdf/1655.pdf., [380] M. A. Fehr, M. Rehkämper, A. N. Halliday, U. Wiechert, B. Hattendorf, D. Günther, S. Ono, J. L. Eigenbrode, I. D. Rumble. Geochim. Cosmochim. Acta69, 5099 (2005)..
Isotopes in Geochronology
The double beta decay of 130Te (with a half-life of 7×1020 years) has been used for the determination of gas-retention ages of tellurium minerals [382] A. P. Meshik, C. M. Hohenberg, O. V. Pravdivtseva, T. J. Bernatowicz, Y. S. Kapustab. Nucl. Phys. A809, 275 (2008)..
Isotopes Used as a Source of Radioactive Isotope(s)
120Te is used for the production of 120gI, where “g” indicates ground state, via the 120Te (p, n) 120gI reaction, which is used as a positron emission tomography (PET) and beta-emitting isotope [383] A. Hohn, H. H. Coenen, S. M. Qaim. Appl. Radiat. Isot.49, 1493 (1998)., [384] H. Herzog, S. M. Qaim, L. Tellmann, S. Spellerberg, D. Kruecker, H. H. Coenen. Eur. J. Nucl. Med. Mol. Imaging33, 1249 (2006).. 120gI has a half-life of 1.36 h. 122Te is used in the production of the radioisotope 122I (with a half-life of 3.6 min) via the reaction 122Te (p, n) 122I, which is used in gamma imaging [385] A. Hohn, B. Scholten, H. H. Coenen, S. M. Qaim, Appl. Radiat. Isot.49, 93 (1998).. 123Te is used for the production of radioactive 123I (with a half-life of 13.2 h) via the 123Te (p, n) 123I reaction, which is used in thyroid imaging [386] T. Kakavand, M. Sadeghi, K. K. Moghaddam, S. S. Bonab, B. Fateh. Iran. J. Radiat. Res.5, 207 (2008). and for in vivo medical studies using single-photon emission computed tomography (SPECT) [386] T. Kakavand, M. Sadeghi, K. K. Moghaddam, S. S. Bonab, B. Fateh. Iran. J. Radiat. Res.5, 207 (2008).. 124Te is used for the production of both 123I and the PET isotope 124I via the 124Te (p, 2n) 123I and 124Te (p, n) 124I reactions, respectively [386] T. Kakavand, M. Sadeghi, K. K. Moghaddam, S. S. Bonab, B. Fateh. Iran. J. Radiat. Res.5, 207 (2008)., [387] M. L. Firouzbakht, D. J. Schlyer, R. D. Finn, G. Laguzzi, A. P. Wolf. Nucl. Instr. Methods Phys. Res. B79, 909 (1993)., [388] H. Herzog, L. Tellman, S. M. Qaim, S. Spellerberg, A. Schmid, H. H. Coenen. Appl. Radiat. Isot.56, 673 (2002)., [389] F. T. Lee, C. Hall, A. Rigopoulos, J. Zweit, K. Pathmaraj, G. J. O’Keefe, F. E. Smyth, S. Welt, L. J. Old, A. M. Scott. J. Nucl. Med.42, 764 (2001).. The half-life of 124I is 100 h.
Tellurium commonly shows oxidation states −2, +4, and +6, with +4 especially important in oxides and oxoanion chemistry. Hydrogen telluride, H₂Te, is an unstable and highly toxic hydride. Tellurium dioxide, TeO₂, is an amphoteric oxide used in tellurite glasses and as a chemical intermediate. Telluric acid, H₆TeO₆, contains tellurium in the +6 state. Metal tellurides include cadmium telluride, CdTe, and bismuth telluride, Bi₂Te₃, whose bonding and band structures are central to their electronic uses.
See more information at the Tellurium compound page.
Elemental tellurium has moderate acute toxicity, but dusts and fumes should be controlled because inhalation and ingestion can be harmful. Exposure to tellurium or some tellurium compounds can produce a persistent garlic-like odor in breath and sweat from volatile metabolites. Hydrogen telluride, H₂Te, is particularly hazardous. Cadmium telluride, CdTe, also requires controls because cadmium compounds are toxic, especially if dust is generated during manufacture or disposal.
Tellurium and its compounds are probably toxic and should be handled with care. Workmen exposed to as little as 0.01 mg/m3 of air, or less, develop "tellurium breath," which has a garlic-like odor.
Tellurium is a rare trace element in the crust and is strongly chalcophile, concentrating with sulfide and telluride mineral assemblages rather than forming abundant independent deposits. Weathering can release tellurium into soils and waters, where its speciation depends on redox conditions and pH. Tellurite and tellurate species can be mobile under some conditions, while reduction and adsorption tend to immobilize it. It has no known essential biological role for humans.
Tellurium is not usually mined as a primary product. Most commercial supply is recovered as a by-product from copper refining, especially from anode slimes produced during electrolytic purification. This dependence makes supply sensitive to copper ore composition, refinery practice, and the economics of by-product recovery rather than to tellurium demand alone. Demand is led by cadmium telluride photovoltaics and thermoelectric materials, with smaller metallurgical and chemical uses. Recycling is technically possible from manufacturing scrap and some end-of-life devices, but collection and separation can limit recovery.
Tellurium is occasionally found native, but is more often found as the telluride of gold (calaverite), and combined with other metals. It is recovered commercially from anode muds produced during the electrolytic refining of blister copper. The U.S., Canada, Peru, and Japan are the largest Free World producers of the element.
Tellurium is far less abundant in the universe than lighter chalcogens such as sulfur and selenium. Its stable isotopes are produced mainly by neutron-capture processes in earlier generations of stars, including slow and rapid neutron-capture pathways. In planetary materials it behaves as a chalcophile element and is associated with sulfide-rich phases rather than silicate minerals.
- Tellurium was named from tellus, the Latin word for Earth.
- It is one of the few elements whose name refers to Earth rather than a celestial object or place of discovery.
- Natural tellurium contains several stable isotopes and very long-lived radioactive isotopes.
- The element can impart a garlic-like odor to breath at exposures far below severe poisoning levels.
- Tellurium improves the machinability of copper without requiring large alloy additions.
- Many useful tellurium materials are semiconductors rather than metallic conductors.
이미지
특성
물리적 특성
- 원자 반지름(경험값)
- 140 pm 모든 원소의 원자 반지름(경험값) 비교 →
- 공유 결합 반지름
- 138 pm 모든 원소의 공유 결합 반지름 비교 →
- 반데르발스 반지름
- 206 pm 모든 원소의 반데르발스 반지름 비교 →
- 금속 반지름
- 137 pm 모든 원소의 금속 반지름 비교 →
- 밀도
- 6232 kg/m³ 모든 원소의 밀도 비교 →
- 몰 부피
- 0.0205 L/mol
- STP에서의 상
- 고체 모든 원소의 STP에서의 상 비교 →
- 녹는점
- 449.51 °C 모든 원소의 녹는점 비교 →
- 끓는점
- 987.85 °C 모든 원소의 끓는점 비교 →
- 열전도율
- 14.3 W/(m·K) 모든 원소의 열전도율 비교 →
- 비열
- 0.202 J/(g·K) 모든 원소의 비열 비교 →
- 몰 열용량
- 25.73 J/(mol·K) 모든 원소의 몰 열용량 비교 →
- 결정 구조
- 육방 조밀 충전 모든 원소의 결정 구조 비교 →
화학적 특성
- 전기 음성도(Pauling)
- 2.1 모든 원소의 전기 음성도(Pauling) 비교 →
- 전기 음성도(Allen)
- 2.158
- 전자 친화도
- 1.9708 eV
- 제1 이온화 에너지
- 9.009808 eV 모든 원소의 제1 이온화 에너지 비교 →
- 제2 이온화 에너지
- 18.600064 eV 모든 원소의 제2 이온화 에너지 비교 →
- 제3 이온화 에너지
- 27.840096 eV 모든 원소의 제3 이온화 에너지 비교 →
- 제4 이온화 에너지
- 37.415629 eV 모든 원소의 제4 이온화 에너지 비교 →
- 제5 이온화 에너지
- 59.300204 eV 모든 원소의 제5 이온화 에너지 비교 →
- 산화 상태
- −2, −1, 0, +1, +2, +3, +4, +5, +6 모든 원소의 산화 상태 비교 →
- 원자가 전자
- 6 모든 원소의 원자가 전자 비교 →
- 전자 배치
- [Kr] 5s2 4d10 5p4
열역학적 특성
- 임계점(온도)
- 2056 °C
- 융해열
- 0.1812717 eV 모든 원소의 융해열 비교 →
- 기화열
- 0.54412603 eV 모든 원소의 기화열 비교 →
- 승화열
- 2.041768 eV
- 원자화열
- 2.041768 eV
- 원자화 엔탈피
- 2.037622 eV
핵 특성
- 양성자 수
- 52 모든 원소의 양성자 수 비교 →
- 중성자 수
- 74 모든 원소의 중성자 수 비교 →
- 알려진 동위원소 수
- 42 모든 원소의 알려진 동위원소 수 비교 →
- 안정 동위원소 수
- 4 모든 원소의 안정 동위원소 수 비교 →
- 가장 안정한 동위원소
- Te-126
- 발견 연도
- 1782
존재비
- 존재비(지각)
- 0.001 mg/kg 모든 원소의 존재비(지각) 비교 →
결정 구조
- 격자 상수 a
- 445 pm
전자 구조
- 전자껍질별 전자 수
- 2, 8, 18, 18, 6 모든 원소의 전자껍질별 전자 수 비교 →
식별자
- CAS 등록 번호
- 13494-80-9 모든 원소의 CAS 등록 번호 비교 →
- 항 기호
- 3P2
- InChI
- InChI=1S/Te
- InChI 키
- PORWMNRCUJJQNO-UHFFFAOYSA-N
전자 배치 측정값
Te: 4d¹⁰ 5s² 5p⁴[Kr] 4d¹⁰ 5s² 5p⁴1s² 2s² 2p⁶ 3s² 3p⁶ 3d¹⁰ 4s² 4p⁶ 4d¹⁰ 5s² 5p⁴원자 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 |
|---|---|---|---|
| 122 안정 | 121.9030435 ± 0.0000016 | 2.5500% | 안정 |
| 124 안정 | 123.9028171 ± 0.0000016 | 4.7400% | 안정 |
| 125 안정 | 124.9044299 ± 0.0000016 | 7.0700% | 안정 |
| 126 안정 | 125.9033109 ± 0.0000016 | 18.8400% | 안정 |
상 / 상태
이유: 녹는점(449.51 °C)보다 424.5 °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 52개 중 10개를 표시합니다. 이온 전하순으로 정렬되었습니다(오름차순).
보유 에너지 준위 데이터 ?
| 이온 | 전하 | 준위 |
|---|---|---|
| Te I | 0 | 120 |
| Te II | +1 | 129 |
| Te III | +2 | 55 |
| Te IV | +3 | 16 |
| Te V | +4 | 45 |
| Te VI | +5 | 9 |
| Te VII | +6 | 60 |
| Te VIII | +7 | 2 |
| Te IX | +8 | 2 |
| Te X | +9 | 2 |
이온 반지름
| 전하 | 배위 | 스핀 | 반지름 |
|---|---|---|---|
| -2 | 6 | 해당 없음 | 221 pm |
| +4 | 3 | 해당 없음 | 52 pm |
| +4 | 4 | 해당 없음 | 66 pm |
| +4 | 6 | 해당 없음 | 97 pm |
| +6 | 4 | 해당 없음 | 43 pm |
| +6 | 6 | 해당 없음 | 56.00000000000001 pm |
화합물
동위원소 (4)
Thirty isotopes of tellurium are known, with atomic masses ranging from 108 to 137. Natural tellurium consists of eight isotopes.
| 질량수 | 원자 질량(u) | 천연 존재비 | 반감기 | 붕괴 방식 | |
|---|---|---|---|---|---|
| 122 안정 | 121.9030435 ± 0.0000016 | 2.5500% ± 0.1200% | 안정 | stable | |
| 124 안정 | 123.9028171 ± 0.0000016 | 4.7400% ± 0.1400% | 안정 | stable | |
| 125 안정 | 124.9044299 ± 0.0000016 | 7.0700% ± 0.1500% | 안정 | stable | |
| 126 안정 | 125.9033109 ± 0.0000016 | 18.8400% ± 0.2500% | 안정 | stable |
스펙트럼선
전체 74개 중 50개를 표시합니다. 기본적으로 세기가 측정된 스펙트럼선만 표시됩니다.
| 파장(nm) | 세기 | 이온화 단계 | 유형 | 전이 | 정확도 | 출처 | |
|---|---|---|---|---|---|---|---|
| 486.623 nm | 2300 | Te II | emission | 5s2.5p2.(3P).6p 4D* → 5s2.5p2.(3P).6d 4F | 측정값 | NIST | |
| 557.636 nm | 2100 | Te II | emission | 5s2.5p2.(1D).6s 2D → 5s2.5p2.(1D).6p 2F* | 측정값 | NIST | |
| 570.812 nm | 1900 | Te II | emission | 5s2.5p2.(3P).6s 4P → 5s2.5p2.(3P).6p 4D* | 측정값 | NIST | |
| 483.13 nm | 1600 | Te II | emission | 5s2.5p2.(3P).6p 4D* → 5s2.5p2.(3P).6d 4P | 측정값 | NIST | |
| 564.926 nm | 1500 | Te II | emission | 5s2.5p2.(3P).6s 4P → 5s2.5p2.(3P).6p 4D* | 측정값 | NIST | |
| 575.586 nm | 1500 | Te II | emission | 5s2.5p2.(3P).6s 4P → 5s2.5p2.(3P).6p 4D* | 측정값 | NIST | |
| 544.984 nm | 1400 | Te II | emission | 5s2.5p2.(3P).6s 4P → 5s2.5p2.(3P).6p 4P* | 측정값 | NIST | |
| 468.691 nm | 1310 | Te II | emission | 5s2.5p2.(3P).6p 4P* → 5s2.5p2.(3P).6d 4D | 측정값 | NIST | |
| 476.605 nm | 1300 | Te II | emission | 5s2.5p2.(3P).6p 2D* → 5s2.5p2.(3P).6d 2F | 측정값 | NIST | |
| 490.442 nm | 1300 | Te II | emission | 5s2.5p2.(3P).6p 2D* → 5s2.5p2.(3P).6d 2F | 측정값 | NIST | |
| 566.622 nm | 1200 | Te II | emission | 5s2.5p2.(3P).6s 2P → 5s2.5p2.(3P).6p 2D* | 측정값 | NIST | |
| 597.468 nm | 1200 | Te II | emission | 5s2.5p2.(3P).6s 4P → 5s2.5p2.(3P).6p 4P* | 측정값 | NIST | |
| 548.795 nm | 1100 | Te II | emission | 5s2.5p2.(3P).5d 2P → 5s2.5p2.(3P).6p 4D* | 측정값 | NIST | |
| 484.29 nm | 1000 | Te II | emission | 5s2.5p2.(3P).5d 2D → 5s2.5p2.(3P).4f 4D* | 측정값 | NIST | |
| 486.513 nm | 1000 | Te II | emission | 5s2.5p2.(3P).6p 4D* → 5s2.5p2.(3P).6d 4D | 측정값 | NIST | |
| 482.712 nm | 900 | Te II | emission | 5s2.5p2.(3P).6p 4P* → 5s2.5p2.(3P).6d 4D | 측정값 | NIST | |
| 447.865 nm | 830 | Te II | emission | 5s2.5p2.(3P).6p 4P* → 5s2.5p2.(3P).6d 4D | 측정값 | NIST | |
| 500.081 nm | 810 | Te II | emission | 5s2.5p2.(3P).6s 4P → 5s2.5p2.(3P).6p 2D* | 측정값 | NIST | |
| 477.155 nm | 800 | Te II | emission | 5s2.5p2.(3P).6p 4D* → 5s2.5p2.(3P).6d 4F | 측정값 | NIST | |
| 593.615 nm | 730 | Te II | emission | 5s2.5p2.(3P).6s 4P → 5s2.5p2.(3P).6p 4S* | 측정값 | NIST | |
| 464.111 nm | 680 | Te II | emission | 5s2.5p2.(3P).6p 4D* → 5s2.5p2.(3P).6d 4D | 측정값 | NIST | |
| 470.654 nm | 670 | Te II | emission | 5s2.5p2.(1D).6s 2D → 5s2.5p2.(1D).6p 2P* | 측정값 | NIST | |
| 436.402 nm | 650 | Te II | emission | 5s2.5p2.(3P).5d 4P → 5s2.5p2.(3P).4f 4D* | 측정값 | NIST | |
| 636.713 nm | 570 | Te II | emission | 5s.(2S).5p4.(1D) 2D → 5s2.5p2.(3P).6p 4D* | 측정값 | NIST | |
| 469.638 nm | 560 | Te II | emission | 5s2.5p2.(3P).5d 4P → 5s2.5p2.(3P).4f 2D* | 측정값 | NIST | |
| 416.977 nm | 540 | Te II | emission | 5s2.5p2.(3P).5d 2D → 5s2.5p2.(3P).4f 2F* | 측정값 | NIST | |
| 463.062 nm | 540 | Te II | emission | 5s2.5p2.(3P).6p 4S* → 5s2.5p2.(3P).7s 2P | 측정값 | NIST | |
| 478.488 nm | 510 | Te II | emission | 5s2.5p2.(1D).6s 2D → 5s2.5p2.(1D).6p 2P* | 측정값 | NIST | |
| 455.778 nm | 480 | Te II | emission | 5s2.5p2.(3P).6p 4S* → 5s2.5p2.(3P).6d 4D | 측정값 | NIST | |
| 683.7663 nm | 430 | Te I | emission | 5p3.(4S*).6p 5P → 5p3.(4S*).8d 5D* | 측정값 | NIST | |
| 404.716 nm | 400 | Te II | emission | 5s2.5p2.(3P).5d 4P → 5s2.5p2.(3P).4f 2D* | 측정값 | NIST | |
| 428.583 nm | 370 | Te II | emission | 5s2.5p2.(3P).6p 2S* → 5s2.5p2.(3P).6d 4D | 측정값 | NIST | |
| 394.798 nm | 340 | Te II | emission | 5s2.5p2.(3P).5d 4P → 5s2.5p2.(3P).4f 4F* | 측정값 | NIST | |
| 422.572 nm | 340 | Te II | emission | 5s2.5p2.(3P).5d 4P → 5s2.5p2.(3P).4f 4D* | 측정값 | NIST | |
| 396.921 nm | 320 | Te II | emission | 5s.(2S).5p4.(1D) 2D → 5s2.5p2.(1D).6p 2D* | 측정값 | NIST | |
| 410.105 nm | 320 | Te II | emission | 5s2.5p2.(1D).5d 2S → 5s2.5p2.(3P).4f 2D* | 측정값 | NIST | |
| 412.732 nm | 320 | Te II | emission | 5s2.5p2.(1D).5d 2S → 5s2.5p2.(3P).4f 4D* | 측정값 | NIST | |
| 496.187 nm | 320 | Te II | emission | 5s2.5p2.(3P).6p 4P* → 5s2.5p2.(3P).6d 4D | 측정값 | NIST | |
| 400.653 nm | 310 | Te II | emission | 5s.(2S).5p4.(3P) 4P → 5s2.5p2.(3P).6p 4D* | 측정값 | NIST | |
| 438.51 nm | 310 | Te II | emission | 5s2.5p2.(3P).5d 4P → 5s2.5p2.(3P).4f 2D* | 측정값 | NIST | |
| 417.929 nm | 300 | Te II | emission | 5s2.5p2.(3P).5d 4P → 5s2.5p2.(1S).6p 2P* | 측정값 | NIST | |
| 427.343 nm | 300 | Te II | emission | 5s2.5p2.(3P).6p 2S* → 5s2.5p2.(3P).7s 2P | 측정값 | NIST | |
| 679.109 nm | 300 | Te I | emission | 5p3.(4S*).6p 5P → 5p3.(4S*).8d 3D* | 측정값 | NIST | |
| 669.0154 nm | 290 | Te I | emission | 5p3.(4S*).6p 5P → 5p3.(4S*).8d 5D* | 측정값 | NIST | |
| 453.708 nm | 260 | Te II | emission | 5s2.5p2.(3P).5d 4P → 5s2.5p2.(3P).4f 4F* | 측정값 | NIST | |
| 397.592 nm | 250 | Te II | emission | 5s.(2S).5p4.(1D) 2D → 5s2.5p2.(1D).6p 2F* | 측정값 | NIST | |
| 416.356 nm | 250 | Te II | emission | 5s2.5p2.(3P).5d 4P → 5s2.5p2.(3P).4f 4D* | 측정값 | NIST | |
| 398.176 nm | 240 | Te II | emission | 5s2.5p2.(3P).6s 2P → 5s2.5p2.(1D).6p 2P* | 측정값 | NIST | |
| 425.114 nm | 240 | Te II | emission | 5s2.5p2.(3P).5d 2D → 5s2.5p2.(3P).4f 2F* | 측정값 | NIST | |
| 404.888 nm | 230 | Te II | emission | 5s.(2S).5p4.(3P) 4P → 5s2.5p2.(3P).6p 4S* | 측정값 | NIST |
확장 특성
공유 결합 반지름(확장)
- 공유 결합 반지름(Pyykkö)
- 136 pm
- 공유 결합 반지름(Pyykkö, 이중 결합)
- 128 pm
- 공유 결합 반지름(Pyykkö, 삼중 결합)
- 121 pm
- 공유 결합 반지름(Bragg)
- 133 pm
반데르발스 반지름
- Bondi
- 206 pm
- Batsanov
- 210 pm
- Alvarez
- 199 pm
- UFF
- 447 pm
- MM3
- 244 pm
- Dreiding
- 423 pm
원자 및 금속 반지름
- 원자 반지름(Rahm)
- 242 pm
- 금속 반지름(C12)
- 160 pm
번호 척도
- Mendeleev
- 102
- Pettifor
- 92
- Glawe
- 94
전기 음성도 척도
- Ghosh
- 0
- Gunnarsson–Lundqvist
- 6
- Robles–Bartolotti
- 4
분극률 및 분산
- 쌍극자 분극률
- 38 a.u.
- 쌍극자 분극률(불확도)
- 4 a.u.
- C₆
- 445 Ha·Bohr6
- C₆ (Gould–Bučko)
- 471 Ha·Bohr6
상전이 및 동소체
| 녹는점 | 722.66 K |
| 끓는점 | 1261.15 K |
| 임계점(온도) | 2329.15 K |
산화 상태 분류
심화 참고 데이터
차폐 상수 (11)
| n | 오비탈 | σ |
|---|---|---|
| 1 | s | 1.0432 |
| 2 | p | 4.14 |
| 2 | s | 13.6688 |
| 3 | d | 14.1607 |
| 3 | p | 17.9911 |
| 3 | s | 18.0019 |
| 4 | d | 32.04 |
| 4 | p | 28.878 |
| 4 | s | 27.5916 |
| 5 | p | 41.1915 |
결정 반지름 상세 정보 (6)
| 전하 | CN | 스핀 | rcrystal (pm) | 기원 |
|---|---|---|---|---|
| -2 | VI | 207 | Pauling's (1960) crystal radius, | |
| 4 | III | 66 | ||
| 4 | IV | 80 | ||
| 4 | VI | 111 | ||
| 6 | IV | 57 | calculated, | |
| 6 | VI | 70 |
동위원소 붕괴 방식 (67)
| 동위원소 | 모드 | 세기 |
|---|---|---|
| 104 | A | 100% |
| 105 | A | 100% |
| 106 | A | 100% |
| 107 | A | 70% |
| 107 | B+ | — |
| 107 | B+p | — |
| 108 | B+ | 51% |
| 108 | A | 49% |
| 108 | B+p | 2.4% |
| 108 | B+A | 0.1% |
X선 산란 인자 (508)
| 에너지 (eV) | f₁ | f₂ |
|---|---|---|
| 10 | — | 9.70237 |
| 10.1617 | — | 9.72653 |
| 10.3261 | — | 9.75076 |
| 10.4931 | — | 9.77506 |
| 10.6628 | — | 9.7994 |
| 10.8353 | — | 9.77638 |
| 11.0106 | — | 9.72308 |
| 11.1886 | — | 9.67008 |
| 11.3696 | — | 9.61736 |
| 11.5535 | — | 9.54395 |
추가 데이터
Estimated Crustal Abundance
The estimated element abundance in the earth's crust.
1×10-3 milligrams per kilogram
참고 문헌 (1)
- [5] Tellurium https://education.jlab.org/itselemental/ele052.html
Estimated Oceanic Abundance
The estimated element abundance in the earth's oceans.
Not Applicable
참고 문헌 (1)
- [5] Tellurium https://education.jlab.org/itselemental/ele052.html
Sources
Sources of this element.
Tellurium is occasionally found native, but is more often found as the telluride of gold (calaverite), and combined with other metals. It is recovered commercially from anode muds produced during the electrolytic refining of blister copper. The U.S., Canada, Peru, and Japan are the largest Free World producers of the element.
참고 문헌 (1)
- [6] Tellurium https://periodic.lanl.gov/52.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 Tellurium.
The element property data was retrieved from publications.