Tellurium (Te)
metalloidSolid
標準原子量
127.6 u電子配置
[Kr] 5s2 4d10 5p4融点
449.51 °C沸点
987.85 °C密度
6232 kg/m³酸化数
−2, −1, 0, +1, +2, +3, +4, +5, +6電気陰性度（Pauling）
2.1第1イオン化エネルギー
9.009808 eV発見年
1782原子半径
140 pm詳細
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.
画像
性質
物理的性質
- 原子半径（経験値）
- 140 pm 全元素の原子半径（経験値）を比較 →
- 共有結合半径
- 138 pm 全元素の共有結合半径を比較 →
- ファンデルワールス半径
- 206 pm 全元素のファンデルワールス半径を比較 →
- 金属半径
- 137 pm 全元素の金属半径を比較 →
- 密度
- 6232 kg/m³ 全元素の密度を比較 →
- モル体積
- 0.0205 L/mol
- 標準温度・圧力（STP）での相
- 固体 全元素の標準温度・圧力（STP）での相を比較 →
- 融点
- 449.51 °C 全元素の融点を比較 →
- 沸点
- 987.85 °C 全元素の沸点を比較 →
- 熱伝導率
- 14.3 W/(m·K) 全元素の熱伝導率を比較 →
- 比熱容量
- 0.202 J/(g·K) 全元素の比熱容量を比較 →
- モル熱容量
- 25.73 J/(mol·K) 全元素のモル熱容量を比較 →
- 結晶構造
- 六方最密充填構造 全元素の結晶構造を比較 →
化学的性質
- 電気陰性度（Pauling）
- 2.1 全元素の電気陰性度（Pauling）を比較 →
- 電気陰性度（Allen）
- 2.158
- 電子親和力
- 1.9708 eV
- 第1イオン化エネルギー
- 9.009808 eV 全元素の第1イオン化エネルギーを比較 →
- 第2イオン化エネルギー
- 18.600064 eV 全元素の第2イオン化エネルギーを比較 →
- 第3イオン化エネルギー
- 27.840096 eV 全元素の第3イオン化エネルギーを比較 →
- 第4イオン化エネルギー
- 37.415629 eV 全元素の第4イオン化エネルギーを比較 →
- 第5イオン化エネルギー
- 59.300204 eV 全元素の第5イオン化エネルギーを比較 →
- 酸化数
- −2, −1, 0, +1, +2, +3, +4, +5, +6 全元素の酸化数を比較 →
- 価電子
- 6 全元素の価電子を比較 →
- 電子配置
- [Kr] 5s2 4d10 5p4
熱力学的性質
- 臨界点（温度）
- 2056 °C
- 融解熱
- 0.1812717 eV 全元素の融解熱を比較 →
- 蒸発熱
- 0.54412603 eV 全元素の蒸発熱を比較 →
- 昇華熱
- 2.041768 eV
- 原子化熱
- 2.041768 eV
- 原子化エンタルピー
- 2.037622 eV
原子核
- 陽子数
- 52 全元素の陽子数を比較 →
- 中性子数
- 74 全元素の中性子数を比較 →
- 既知の同位体
- 42 全元素の既知の同位体を比較 →
- 安定同位体
- 4 全元素の安定同位体を比較 →
- 最も安定な同位体
- Te-126
- 発見年
- 1782
存在度
- 存在度（地殻）
- 0.001 mg/kg 全元素の存在度（地殻）を比較 →
結晶構造
- 格子定数a
- 445 pm
電子構造
- 各電子殻の電子数
- 2, 8, 18, 18, 6 全元素の各電子殻の電子数を比較 →
識別子
- CAS登録番号
- 13494-80-9 全元素のCAS登録番号を比較 →
- 項記号
- 3P2
- InChI
- InChI=1S/Te
- InChI Key
- PORWMNRCUJJQNO-UHFFFAOYSA-N
電子配置 測定値
Te: 4d¹⁰ 5s² 5p⁴[Kr] 4d¹⁰ 5s² 5p⁴1s² 2s² 2p⁶ 3s² 3p⁶ 3d¹⁰ 4s² 4p⁶ 4d¹⁰ 5s² 5p⁴原子モデル
同位体によって中性子数、質量、安定性は変わりますが、中性原子の電子配置は変わりません。
模式的な原子モデルです。実際の縮尺とは異なります。
原子の指紋
発光／吸収スペクトル
同位体分布
| 質量数 | 原子質量（u） | 天然存在比 | 半減期 |
|---|---|---|---|
| 122 安定 | 121.9030435 ± 0.0000016 | 2.5500% | 安定 |
| 124 安定 | 123.9028171 ± 0.0000016 | 4.7400% | 安定 |
| 125 安定 | 124.9044299 ± 0.0000016 | 7.0700% | 安定 |
| 126 安定 | 125.9033109 ± 0.0000016 | 18.8400% | 安定 |
相／状態
理由: 融点（449.51 °C）より424.5 °C低い
模式図、実際の縮尺とは異なります
相転移点
相転移エネルギー
融点で1 molを融解させるのに必要なエネルギー
沸点で1 molを蒸発させるのに必要なエネルギー
昇華点で1 molを昇華させるのに必要なエネルギー
密度
標準条件下
標準条件下
詳細
原子スペクトル
全52件中10件を表示しています。 イオンの電荷の昇順で並べています。
準位データの収録状況 ?
| イオン | 電荷 | 準位 |
|---|---|---|
| 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 |
イオン半径
| 電荷 | 配位 | スピン | 半径 |
|---|---|---|---|
| -2 | 6 | データなし | 221 pm |
| +4 | 3 | データなし | 52 pm |
| +4 | 4 | データなし | 66 pm |
| +4 | 6 | データなし | 97 pm |
| +6 | 4 | データなし | 43 pm |
| +6 | 6 | データなし | 56.00000000000001 pm |
化合物
同位体 (4)
Thirty isotopes of tellurium are known, with atomic masses ranging from 108 to 137. Natural tellurium consists of eight isotopes.
| 質量数 | 原子質量（u） | 天然存在比 | 半減期 | 崩壊形式 | |
|---|---|---|---|---|---|
| 122 安定 | 121.9030435 ± 0.0000016 | 2.5500% ± 0.1200% | 安定 | stable | |
| 124 安定 | 123.9028171 ± 0.0000016 | 4.7400% ± 0.1400% | 安定 | stable | |
| 125 安定 | 124.9044299 ± 0.0000016 | 7.0700% ± 0.1500% | 安定 | stable | |
| 126 安定 | 125.9033109 ± 0.0000016 | 18.8400% ± 0.2500% | 安定 | stable |
スペクトル線
全74件中50件を表示しています。 初期設定では、強度の測定値があるスペクトル線のみを表示します。
| 波長（nm） | 強度 | 電離段階 | 種類 | 遷移 | 精度 | 出典 | |
|---|---|---|---|---|---|---|---|
| 486.623 nm | 2300 | Te II | emission | 5s2.5p2.(3P).6p 4D* → 5s2.5p2.(3P).6d 4F | 測定値 | NIST | |
| 557.636 nm | 2100 | Te II | emission | 5s2.5p2.(1D).6s 2D → 5s2.5p2.(1D).6p 2F* | 測定値 | NIST | |
| 570.812 nm | 1900 | Te II | emission | 5s2.5p2.(3P).6s 4P → 5s2.5p2.(3P).6p 4D* | 測定値 | NIST | |
| 483.13 nm | 1600 | Te II | emission | 5s2.5p2.(3P).6p 4D* → 5s2.5p2.(3P).6d 4P | 測定値 | NIST | |
| 564.926 nm | 1500 | Te II | emission | 5s2.5p2.(3P).6s 4P → 5s2.5p2.(3P).6p 4D* | 測定値 | NIST | |
| 575.586 nm | 1500 | Te II | emission | 5s2.5p2.(3P).6s 4P → 5s2.5p2.(3P).6p 4D* | 測定値 | NIST | |
| 544.984 nm | 1400 | Te II | emission | 5s2.5p2.(3P).6s 4P → 5s2.5p2.(3P).6p 4P* | 測定値 | NIST | |
| 468.691 nm | 1310 | Te II | emission | 5s2.5p2.(3P).6p 4P* → 5s2.5p2.(3P).6d 4D | 測定値 | NIST | |
| 476.605 nm | 1300 | Te II | emission | 5s2.5p2.(3P).6p 2D* → 5s2.5p2.(3P).6d 2F | 測定値 | NIST | |
| 490.442 nm | 1300 | Te II | emission | 5s2.5p2.(3P).6p 2D* → 5s2.5p2.(3P).6d 2F | 測定値 | NIST | |
| 566.622 nm | 1200 | Te II | emission | 5s2.5p2.(3P).6s 2P → 5s2.5p2.(3P).6p 2D* | 測定値 | NIST | |
| 597.468 nm | 1200 | Te II | emission | 5s2.5p2.(3P).6s 4P → 5s2.5p2.(3P).6p 4P* | 測定値 | NIST | |
| 548.795 nm | 1100 | Te II | emission | 5s2.5p2.(3P).5d 2P → 5s2.5p2.(3P).6p 4D* | 測定値 | NIST | |
| 484.29 nm | 1000 | Te II | emission | 5s2.5p2.(3P).5d 2D → 5s2.5p2.(3P).4f 4D* | 測定値 | NIST | |
| 486.513 nm | 1000 | Te II | emission | 5s2.5p2.(3P).6p 4D* → 5s2.5p2.(3P).6d 4D | 測定値 | NIST | |
| 482.712 nm | 900 | Te II | emission | 5s2.5p2.(3P).6p 4P* → 5s2.5p2.(3P).6d 4D | 測定値 | NIST | |
| 447.865 nm | 830 | Te II | emission | 5s2.5p2.(3P).6p 4P* → 5s2.5p2.(3P).6d 4D | 測定値 | NIST | |
| 500.081 nm | 810 | Te II | emission | 5s2.5p2.(3P).6s 4P → 5s2.5p2.(3P).6p 2D* | 測定値 | NIST | |
| 477.155 nm | 800 | Te II | emission | 5s2.5p2.(3P).6p 4D* → 5s2.5p2.(3P).6d 4F | 測定値 | NIST | |
| 593.615 nm | 730 | Te II | emission | 5s2.5p2.(3P).6s 4P → 5s2.5p2.(3P).6p 4S* | 測定値 | NIST | |
| 464.111 nm | 680 | Te II | emission | 5s2.5p2.(3P).6p 4D* → 5s2.5p2.(3P).6d 4D | 測定値 | NIST | |
| 470.654 nm | 670 | Te II | emission | 5s2.5p2.(1D).6s 2D → 5s2.5p2.(1D).6p 2P* | 測定値 | NIST | |
| 436.402 nm | 650 | Te II | emission | 5s2.5p2.(3P).5d 4P → 5s2.5p2.(3P).4f 4D* | 測定値 | NIST | |
| 636.713 nm | 570 | Te II | emission | 5s.(2S).5p4.(1D) 2D → 5s2.5p2.(3P).6p 4D* | 測定値 | NIST | |
| 469.638 nm | 560 | Te II | emission | 5s2.5p2.(3P).5d 4P → 5s2.5p2.(3P).4f 2D* | 測定値 | NIST | |
| 416.977 nm | 540 | Te II | emission | 5s2.5p2.(3P).5d 2D → 5s2.5p2.(3P).4f 2F* | 測定値 | NIST | |
| 463.062 nm | 540 | Te II | emission | 5s2.5p2.(3P).6p 4S* → 5s2.5p2.(3P).7s 2P | 測定値 | NIST | |
| 478.488 nm | 510 | Te II | emission | 5s2.5p2.(1D).6s 2D → 5s2.5p2.(1D).6p 2P* | 測定値 | NIST | |
| 455.778 nm | 480 | Te II | emission | 5s2.5p2.(3P).6p 4S* → 5s2.5p2.(3P).6d 4D | 測定値 | NIST | |
| 683.7663 nm | 430 | Te I | emission | 5p3.(4S*).6p 5P → 5p3.(4S*).8d 5D* | 測定値 | NIST | |
| 404.716 nm | 400 | Te II | emission | 5s2.5p2.(3P).5d 4P → 5s2.5p2.(3P).4f 2D* | 測定値 | NIST | |
| 428.583 nm | 370 | Te II | emission | 5s2.5p2.(3P).6p 2S* → 5s2.5p2.(3P).6d 4D | 測定値 | NIST | |
| 394.798 nm | 340 | Te II | emission | 5s2.5p2.(3P).5d 4P → 5s2.5p2.(3P).4f 4F* | 測定値 | NIST | |
| 422.572 nm | 340 | Te II | emission | 5s2.5p2.(3P).5d 4P → 5s2.5p2.(3P).4f 4D* | 測定値 | NIST | |
| 396.921 nm | 320 | Te II | emission | 5s.(2S).5p4.(1D) 2D → 5s2.5p2.(1D).6p 2D* | 測定値 | NIST | |
| 410.105 nm | 320 | Te II | emission | 5s2.5p2.(1D).5d 2S → 5s2.5p2.(3P).4f 2D* | 測定値 | NIST | |
| 412.732 nm | 320 | Te II | emission | 5s2.5p2.(1D).5d 2S → 5s2.5p2.(3P).4f 4D* | 測定値 | NIST | |
| 496.187 nm | 320 | Te II | emission | 5s2.5p2.(3P).6p 4P* → 5s2.5p2.(3P).6d 4D | 測定値 | NIST | |
| 400.653 nm | 310 | Te II | emission | 5s.(2S).5p4.(3P) 4P → 5s2.5p2.(3P).6p 4D* | 測定値 | NIST | |
| 438.51 nm | 310 | Te II | emission | 5s2.5p2.(3P).5d 4P → 5s2.5p2.(3P).4f 2D* | 測定値 | NIST | |
| 417.929 nm | 300 | Te II | emission | 5s2.5p2.(3P).5d 4P → 5s2.5p2.(1S).6p 2P* | 測定値 | NIST | |
| 427.343 nm | 300 | Te II | emission | 5s2.5p2.(3P).6p 2S* → 5s2.5p2.(3P).7s 2P | 測定値 | NIST | |
| 679.109 nm | 300 | Te I | emission | 5p3.(4S*).6p 5P → 5p3.(4S*).8d 3D* | 測定値 | NIST | |
| 669.0154 nm | 290 | Te I | emission | 5p3.(4S*).6p 5P → 5p3.(4S*).8d 5D* | 測定値 | NIST | |
| 453.708 nm | 260 | Te II | emission | 5s2.5p2.(3P).5d 4P → 5s2.5p2.(3P).4f 4F* | 測定値 | NIST | |
| 397.592 nm | 250 | Te II | emission | 5s.(2S).5p4.(1D) 2D → 5s2.5p2.(1D).6p 2F* | 測定値 | NIST | |
| 416.356 nm | 250 | Te II | emission | 5s2.5p2.(3P).5d 4P → 5s2.5p2.(3P).4f 4D* | 測定値 | NIST | |
| 398.176 nm | 240 | Te II | emission | 5s2.5p2.(3P).6s 2P → 5s2.5p2.(1D).6p 2P* | 測定値 | NIST | |
| 425.114 nm | 240 | Te II | emission | 5s2.5p2.(3P).5d 2D → 5s2.5p2.(3P).4f 2F* | 測定値 | NIST | |
| 404.888 nm | 230 | Te II | emission | 5s.(2S).5p4.(3P) 4P → 5s2.5p2.(3P).6p 4S* | 測定値 | NIST |
詳細な性質
共有結合半径（詳細）
- 共有結合半径（Pyykkö）
- 136 pm
- 共有結合半径（Pyykkö、二重結合）
- 128 pm
- 共有結合半径（Pyykkö、三重結合）
- 121 pm
- 共有結合半径（Bragg）
- 133 pm
ファンデルワールス半径
- Bondi
- 206 pm
- Batsanov
- 210 pm
- Alvarez
- 199 pm
- UFF
- 447 pm
- MM3
- 244 pm
- Dreiding
- 423 pm
原子半径と金属半径
- 原子半径（Rahm）
- 242 pm
- 金属半径（C12）
- 160 pm
番号付けの尺度
- Mendeleev
- 102
- Pettifor
- 92
- Glawe
- 94
電気陰性度の尺度
- Ghosh
- 0
- Gunnarsson–Lundqvist
- 6
- Robles–Bartolotti
- 4
分極率と分散
- 双極子分極率
- 38 a.u.
- 双極子分極率（不確かさ）
- 4 a.u.
- C₆
- 445 Ha·Bohr6
- C₆ (Gould–Bučko)
- 471 Ha·Bohr6
相転移と同素体
| 融点 | 722.66 K |
| 沸点 | 1261.15 K |
| 臨界点（温度） | 2329.15 K |
酸化数の分類
専門参考データ
遮蔽定数 (11)
| n | 軌道 | 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 |
結晶半径の詳細 (6)
| 電荷 | CN | スピン | rcrystal (pm) | 由来 |
|---|---|---|---|---|
| -2 | VI | 207 | Pauling's (1960) crystal radius, | |
| 4 | III | 66 | ||
| 4 | IV | 80 | ||
| 4 | VI | 111 | ||
| 6 | IV | 57 | calculated, | |
| 6 | VI | 70 |
同位体の崩壊形式 (67)
| 同位体 | モード | 強度 |
|---|---|---|
| 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% |
X線散乱因子 (508)
| エネルギー (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 |
追加データ
Estimated Crustal Abundance
The estimated element abundance in the earth's crust.
1×10-3 milligrams per kilogram
参考文献 (1)
- [5] Tellurium https://education.jlab.org/itselemental/ele052.html
Estimated Oceanic Abundance
The estimated element abundance in the earth's oceans.
Not Applicable
参考文献 (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.
参考文献 (1)
- [6] Tellurium https://periodic.lanl.gov/52.shtml
参考文献
(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.