Tellurium (Te)
metalloidSolid
Standart Atom Ağırlığı
127,6 uElektron dizilimi
[Kr] 5s2 4d10 5p4Erime noktası
449,51 °CKaynama noktası
987,85 °CYoğunluk
6232 kg/m³Yükseltgenme basamakları
−2, −1, 0, +1, +2, +3, +4, +5, +6Elektronegatiflik (Pauling)
2,1İyonlaşma enerjisi (1.)
9,009808 eVKeşif yılı
1782Atom yarıçapı
140 pmAyrıntılar
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.
Görseller
Özellikler
Fiziksel
- Atom yarıçapı (ampirik)
- 140 pm Tüm elementlerin Atom yarıçapı (ampirik) değerlerini karşılaştır →
- Kovalent yarıçap
- 138 pm Tüm elementlerin Kovalent yarıçap değerlerini karşılaştır →
- Van der Waals yarıçapı
- 206 pm Tüm elementlerin Van der Waals yarıçapı değerlerini karşılaştır →
- Metalik yarıçap
- 137 pm Tüm elementlerin Metalik yarıçap değerlerini karşılaştır →
- Yoğunluk
- 6232 kg/m³ Tüm elementlerin Yoğunluk değerlerini karşılaştır →
- Molar hacim
- 0,0205 L/mol
- STP'deki faz
- Katı Tüm elementlerin STP'deki faz değerlerini karşılaştır →
- Erime noktası
- 449,51 °C Tüm elementlerin Erime noktası değerlerini karşılaştır →
- Kaynama noktası
- 987,85 °C Tüm elementlerin Kaynama noktası değerlerini karşılaştır →
- Isıl iletkenlik
- 14,3 W/(m·K) Tüm elementlerin Isıl iletkenlik değerlerini karşılaştır →
- Özgül ısı kapasitesi
- 0,202 J/(g·K) Tüm elementlerin Özgül ısı kapasitesi değerlerini karşılaştır →
- Molar ısı kapasitesi
- 25,73 J/(mol·K) Tüm elementlerin Molar ısı kapasitesi değerlerini karşılaştır →
- Kristal yapı
- Hekzagonal sıkı paket Tüm elementlerin Kristal yapı değerlerini karşılaştır →
Kimyasal
- Elektronegatiflik (Pauling)
- 2,1 Tüm elementlerin Elektronegatiflik (Pauling) değerlerini karşılaştır →
- Elektronegatiflik (Allen)
- 2,158
- Elektron ilgisi
- 1,9708 eV
- İyonlaşma enerjisi (1.)
- 9,009808 eV Tüm elementlerin İyonlaşma enerjisi (1.) değerlerini karşılaştır →
- İyonlaşma enerjisi (2.)
- 18,600064 eV Tüm elementlerin İyonlaşma enerjisi (2.) değerlerini karşılaştır →
- İyonlaşma enerjisi (3.)
- 27,840096 eV Tüm elementlerin İyonlaşma enerjisi (3.) değerlerini karşılaştır →
- İyonlaşma enerjisi (4.)
- 37,415629 eV Tüm elementlerin İyonlaşma enerjisi (4.) değerlerini karşılaştır →
- İyonlaşma enerjisi (5.)
- 59,300204 eV Tüm elementlerin İyonlaşma enerjisi (5.) değerlerini karşılaştır →
- Yükseltgenme basamakları
- −2, −1, 0, +1, +2, +3, +4, +5, +6 Tüm elementlerin Yükseltgenme basamakları değerlerini karşılaştır →
- Değerlik elektronları
- 6 Tüm elementlerin Değerlik elektronları değerlerini karşılaştır →
- Elektron dizilimi
- [Kr] 5s2 4d10 5p4
Termodinamik
- Kritik nokta (sıcaklık)
- 2056 °C
- Erime ısısı
- 0,1812717 eV Tüm elementlerin Erime ısısı değerlerini karşılaştır →
- Buharlaşma ısısı
- 0,54412603 eV Tüm elementlerin Buharlaşma ısısı değerlerini karşılaştır →
- Süblimleşme ısısı
- 2,041768 eV
- Atomlaşma ısısı
- 2,041768 eV
- Atomlaşma entalpisi
- 2,037622 eV
Nükleer
- Protonlar
- 52 Tüm elementlerin Protonlar değerlerini karşılaştır →
- Nötronlar
- 74 Tüm elementlerin Nötronlar değerlerini karşılaştır →
- Bilinen izotoplar
- 42 Tüm elementlerin Bilinen izotoplar değerlerini karşılaştır →
- Kararlı izotoplar
- 4 Tüm elementlerin Kararlı izotoplar değerlerini karşılaştır →
- En kararlı izotop
- Te-126
- Keşif yılı
- 1782
Bolluk
- Bolluk (yer kabuğu)
- 0,001 mg/kg Tüm elementlerin Bolluk (yer kabuğu) değerlerini karşılaştır →
Kristal Yapı
- Örgü sabiti a
- 445 pm
Elektronik Yapı
- Kabuk başına elektron sayısı
- 2, 8, 18, 18, 6 Tüm elementlerin Kabuk başına elektron sayısı değerlerini karşılaştır →
Tanımlayıcılar
- CAS numarası
- 13494-80-9 Tüm elementlerin CAS numarası değerlerini karşılaştır →
- Terim simgesi
- 3P2
- InChI
- InChI=1S/Te
- InChI Anahtarı
- PORWMNRCUJJQNO-UHFFFAOYSA-N
Elektron Dizilimi Ölçülmüş
Te: 4d¹⁰ 5s² 5p⁴[Kr] 4d¹⁰ 5s² 5p⁴1s² 2s² 2p⁶ 3s² 3p⁶ 3d¹⁰ 4s² 4p⁶ 4d¹⁰ 5s² 5p⁴Atom modeli
İzotoplar nötron sayısını, kütleyi ve kararlılığı değiştirir; nötr bir atomun elektron dizilimini değiştirmez.
Şematik atom modeli, ölçekli değildir.
Atomik Parmak İzi
Emisyon / Soğurma Spektrumu
İzotop Dağılımı
| Kütle numarası | Atom kütlesi (u) | Doğal bolluk | Yarı ömür |
|---|---|---|---|
| 122 Kararlı | 121,9030435 ± 0,0000016 | 2,5500% | Kararlı |
| 124 Kararlı | 123,9028171 ± 0,0000016 | 4,7400% | Kararlı |
| 125 Kararlı | 124,9044299 ± 0,0000016 | 7,0700% | Kararlı |
| 126 Kararlı | 125,9033109 ± 0,0000016 | 18,8400% | Kararlı |
Faz / Hâl
Neden: erime noktasının (449,51 °C) 424,5 °C altında
Şematik, ölçekli değil
Faz geçiş noktaları
Geçiş enerjileri
Erime noktasında 1 mol maddeyi eritmek için gereken enerji
Kaynama noktasında 1 mol maddeyi buharlaştırmak için gereken enerji
Süblimleşme noktasında 1 mol maddeyi süblimleştirmek için gereken enerji
Yoğunluk
Standart koşullarda
Standart koşullarda
İleri düzey
Atomik Spektrumlar
52 kayıttan 10 tanesi gösteriliyor. İyon yüküne göre sıralandı (artan).
Spektral Çizgi Kayıtları ?
| İyon | Yük | Toplam çizgi sayısı | Geçiş olasılıkları | Düzey gösterimleri |
|---|---|---|---|---|
| Te I | 0 | 133 | 6 | 112 |
| Te II | +1 | 345 | 0 | 310 |
Enerji Düzeyi Kayıtları ?
| İyon | Yük | Düzeyler |
|---|---|---|
| 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 |
İyon Yarıçapları
| Yük | Koordinasyon | Spin | Yarıçap |
|---|---|---|---|
| -2 | 6 | Mevcut değil | 221 pm |
| +4 | 3 | Mevcut değil | 52 pm |
| +4 | 4 | Mevcut değil | 66 pm |
| +4 | 6 | Mevcut değil | 97 pm |
| +6 | 4 | Mevcut değil | 43 pm |
| +6 | 6 | Mevcut değil | 56.00000000000001 pm |
Bileşikler
İzotoplar (4)
Thirty isotopes of tellurium are known, with atomic masses ranging from 108 to 137. Natural tellurium consists of eight isotopes.
| Kütle numarası | Atom kütlesi (u) | Doğal bolluk | Yarı ömür | Bozunma türü | |
|---|---|---|---|---|---|
| 122 Kararlı | 121,9030435 ± 0,0000016 | 2,5500% ± 0,1200% | Kararlı | stable | |
| 124 Kararlı | 123,9028171 ± 0,0000016 | 4,7400% ± 0,1400% | Kararlı | stable | |
| 125 Kararlı | 124,9044299 ± 0,0000016 | 7,0700% ± 0,1500% | Kararlı | stable | |
| 126 Kararlı | 125,9033109 ± 0,0000016 | 18,8400% ± 0,2500% | Kararlı | stable |
Spektral Çizgiler
74 kayıttan 50 tanesi gösteriliyor. Varsayılan olarak yalnızca şiddeti ölçülmüş spektral çizgiler gösterilir.
| Dalga boyu (nm) | Şiddet | İyonlaşma aşaması | Tür | Geçiş | Doğruluk | Kaynak | |
|---|---|---|---|---|---|---|---|
| 486.623 nm | 2300 | Te II | emission | 5s2.5p2.(3P).6p 4D* → 5s2.5p2.(3P).6d 4F | Ölçülmüş | NIST | |
| 557.636 nm | 2100 | Te II | emission | 5s2.5p2.(1D).6s 2D → 5s2.5p2.(1D).6p 2F* | Ölçülmüş | NIST | |
| 570.812 nm | 1900 | Te II | emission | 5s2.5p2.(3P).6s 4P → 5s2.5p2.(3P).6p 4D* | Ölçülmüş | NIST | |
| 483.13 nm | 1600 | Te II | emission | 5s2.5p2.(3P).6p 4D* → 5s2.5p2.(3P).6d 4P | Ölçülmüş | NIST | |
| 564.926 nm | 1500 | Te II | emission | 5s2.5p2.(3P).6s 4P → 5s2.5p2.(3P).6p 4D* | Ölçülmüş | NIST | |
| 575.586 nm | 1500 | Te II | emission | 5s2.5p2.(3P).6s 4P → 5s2.5p2.(3P).6p 4D* | Ölçülmüş | NIST | |
| 544.984 nm | 1400 | Te II | emission | 5s2.5p2.(3P).6s 4P → 5s2.5p2.(3P).6p 4P* | Ölçülmüş | NIST | |
| 468.691 nm | 1310 | Te II | emission | 5s2.5p2.(3P).6p 4P* → 5s2.5p2.(3P).6d 4D | Ölçülmüş | NIST | |
| 476.605 nm | 1300 | Te II | emission | 5s2.5p2.(3P).6p 2D* → 5s2.5p2.(3P).6d 2F | Ölçülmüş | NIST | |
| 490.442 nm | 1300 | Te II | emission | 5s2.5p2.(3P).6p 2D* → 5s2.5p2.(3P).6d 2F | Ölçülmüş | NIST | |
| 566.622 nm | 1200 | Te II | emission | 5s2.5p2.(3P).6s 2P → 5s2.5p2.(3P).6p 2D* | Ölçülmüş | NIST | |
| 597.468 nm | 1200 | Te II | emission | 5s2.5p2.(3P).6s 4P → 5s2.5p2.(3P).6p 4P* | Ölçülmüş | NIST | |
| 548.795 nm | 1100 | Te II | emission | 5s2.5p2.(3P).5d 2P → 5s2.5p2.(3P).6p 4D* | Ölçülmüş | NIST | |
| 484.29 nm | 1000 | Te II | emission | 5s2.5p2.(3P).5d 2D → 5s2.5p2.(3P).4f 4D* | Ölçülmüş | NIST | |
| 486.513 nm | 1000 | Te II | emission | 5s2.5p2.(3P).6p 4D* → 5s2.5p2.(3P).6d 4D | Ölçülmüş | NIST | |
| 482.712 nm | 900 | Te II | emission | 5s2.5p2.(3P).6p 4P* → 5s2.5p2.(3P).6d 4D | Ölçülmüş | NIST | |
| 447.865 nm | 830 | Te II | emission | 5s2.5p2.(3P).6p 4P* → 5s2.5p2.(3P).6d 4D | Ölçülmüş | NIST | |
| 500.081 nm | 810 | Te II | emission | 5s2.5p2.(3P).6s 4P → 5s2.5p2.(3P).6p 2D* | Ölçülmüş | NIST | |
| 477.155 nm | 800 | Te II | emission | 5s2.5p2.(3P).6p 4D* → 5s2.5p2.(3P).6d 4F | Ölçülmüş | NIST | |
| 593.615 nm | 730 | Te II | emission | 5s2.5p2.(3P).6s 4P → 5s2.5p2.(3P).6p 4S* | Ölçülmüş | NIST | |
| 464.111 nm | 680 | Te II | emission | 5s2.5p2.(3P).6p 4D* → 5s2.5p2.(3P).6d 4D | Ölçülmüş | NIST | |
| 470.654 nm | 670 | Te II | emission | 5s2.5p2.(1D).6s 2D → 5s2.5p2.(1D).6p 2P* | Ölçülmüş | NIST | |
| 436.402 nm | 650 | Te II | emission | 5s2.5p2.(3P).5d 4P → 5s2.5p2.(3P).4f 4D* | Ölçülmüş | NIST | |
| 636.713 nm | 570 | Te II | emission | 5s.(2S).5p4.(1D) 2D → 5s2.5p2.(3P).6p 4D* | Ölçülmüş | NIST | |
| 469.638 nm | 560 | Te II | emission | 5s2.5p2.(3P).5d 4P → 5s2.5p2.(3P).4f 2D* | Ölçülmüş | NIST | |
| 416.977 nm | 540 | Te II | emission | 5s2.5p2.(3P).5d 2D → 5s2.5p2.(3P).4f 2F* | Ölçülmüş | NIST | |
| 463.062 nm | 540 | Te II | emission | 5s2.5p2.(3P).6p 4S* → 5s2.5p2.(3P).7s 2P | Ölçülmüş | NIST | |
| 478.488 nm | 510 | Te II | emission | 5s2.5p2.(1D).6s 2D → 5s2.5p2.(1D).6p 2P* | Ölçülmüş | NIST | |
| 455.778 nm | 480 | Te II | emission | 5s2.5p2.(3P).6p 4S* → 5s2.5p2.(3P).6d 4D | Ölçülmüş | NIST | |
| 683.7663 nm | 430 | Te I | emission | 5p3.(4S*).6p 5P → 5p3.(4S*).8d 5D* | Ölçülmüş | NIST | |
| 404.716 nm | 400 | Te II | emission | 5s2.5p2.(3P).5d 4P → 5s2.5p2.(3P).4f 2D* | Ölçülmüş | NIST | |
| 428.583 nm | 370 | Te II | emission | 5s2.5p2.(3P).6p 2S* → 5s2.5p2.(3P).6d 4D | Ölçülmüş | NIST | |
| 394.798 nm | 340 | Te II | emission | 5s2.5p2.(3P).5d 4P → 5s2.5p2.(3P).4f 4F* | Ölçülmüş | NIST | |
| 422.572 nm | 340 | Te II | emission | 5s2.5p2.(3P).5d 4P → 5s2.5p2.(3P).4f 4D* | Ölçülmüş | NIST | |
| 396.921 nm | 320 | Te II | emission | 5s.(2S).5p4.(1D) 2D → 5s2.5p2.(1D).6p 2D* | Ölçülmüş | NIST | |
| 410.105 nm | 320 | Te II | emission | 5s2.5p2.(1D).5d 2S → 5s2.5p2.(3P).4f 2D* | Ölçülmüş | NIST | |
| 412.732 nm | 320 | Te II | emission | 5s2.5p2.(1D).5d 2S → 5s2.5p2.(3P).4f 4D* | Ölçülmüş | NIST | |
| 496.187 nm | 320 | Te II | emission | 5s2.5p2.(3P).6p 4P* → 5s2.5p2.(3P).6d 4D | Ölçülmüş | NIST | |
| 400.653 nm | 310 | Te II | emission | 5s.(2S).5p4.(3P) 4P → 5s2.5p2.(3P).6p 4D* | Ölçülmüş | NIST | |
| 438.51 nm | 310 | Te II | emission | 5s2.5p2.(3P).5d 4P → 5s2.5p2.(3P).4f 2D* | Ölçülmüş | NIST | |
| 417.929 nm | 300 | Te II | emission | 5s2.5p2.(3P).5d 4P → 5s2.5p2.(1S).6p 2P* | Ölçülmüş | NIST | |
| 427.343 nm | 300 | Te II | emission | 5s2.5p2.(3P).6p 2S* → 5s2.5p2.(3P).7s 2P | Ölçülmüş | NIST | |
| 679.109 nm | 300 | Te I | emission | 5p3.(4S*).6p 5P → 5p3.(4S*).8d 3D* | Ölçülmüş | NIST | |
| 669.0154 nm | 290 | Te I | emission | 5p3.(4S*).6p 5P → 5p3.(4S*).8d 5D* | Ölçülmüş | NIST | |
| 453.708 nm | 260 | Te II | emission | 5s2.5p2.(3P).5d 4P → 5s2.5p2.(3P).4f 4F* | Ölçülmüş | NIST | |
| 397.592 nm | 250 | Te II | emission | 5s.(2S).5p4.(1D) 2D → 5s2.5p2.(1D).6p 2F* | Ölçülmüş | NIST | |
| 416.356 nm | 250 | Te II | emission | 5s2.5p2.(3P).5d 4P → 5s2.5p2.(3P).4f 4D* | Ölçülmüş | NIST | |
| 398.176 nm | 240 | Te II | emission | 5s2.5p2.(3P).6s 2P → 5s2.5p2.(1D).6p 2P* | Ölçülmüş | NIST | |
| 425.114 nm | 240 | Te II | emission | 5s2.5p2.(3P).5d 2D → 5s2.5p2.(3P).4f 2F* | Ölçülmüş | NIST | |
| 404.888 nm | 230 | Te II | emission | 5s.(2S).5p4.(3P) 4P → 5s2.5p2.(3P).6p 4S* | Ölçülmüş | NIST |
Genişletilmiş Özellikler
Kovalent Yarıçaplar (Genişletilmiş)
- Kovalent yarıçap (Pyykkö)
- 136 pm
- Kovalent yarıçap (Pyykkö, çift bağ)
- 128 pm
- Kovalent yarıçap (Pyykkö, üçlü bağ)
- 121 pm
- Kovalent yarıçap (Bragg)
- 133 pm
Van der Waals Yarıçapları
- Bondi
- 206 pm
- Batsanov
- 210 pm
- Alvarez
- 199 pm
- UFF
- 447 pm
- MM3
- 244 pm
- Dreiding
- 423 pm
Atom ve Metalik Yarıçaplar
- Atom yarıçapı (Rahm)
- 242 pm
- Metalik yarıçap (C12)
- 160 pm
Numaralandırma Ölçekleri
- Mendeleev
- 102
- Pettifor
- 92
- Glawe
- 94
Elektronegatiflik Ölçekleri
- Ghosh
- 0
- Gunnarsson–Lundqvist
- 6
- Robles–Bartolotti
- 4
Kutuplanabilirlik ve Dispersiyon
- Dipol kutuplanabilirliği
- 38 a.u.
- Dipol kutuplanabilirliği (belirsizlik)
- 4 a.u.
- C₆
- 445 Ha·Bohr6
- C₆ (Gould–Bučko)
- 471 Ha·Bohr6
Faz Geçişleri ve Allotroplar
| Erime noktası | 722,66 K |
| Kaynama noktası | 1261,15 K |
| Kritik nokta (sıcaklık) | 2329,15 K |
Yükseltgenme Basamağı Kategorileri
İleri Düzey Referans Verileri
Perdeleme Sabitleri (11)
| n | Orbital | 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 |
Kristal Yarıçaplarının Ayrıntıları (6)
| Yük | CN | Spin | rcrystal (pm) | Köken |
|---|---|---|---|---|
| -2 | VI | 207 | Pauling's (1960) crystal radius, | |
| 4 | III | 66 | ||
| 4 | IV | 80 | ||
| 4 | VI | 111 | ||
| 6 | IV | 57 | calculated, | |
| 6 | VI | 70 |
İzotop Bozunma Türleri (67)
| İzotop | Mod | Şiddet |
|---|---|---|
| 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 Işını Saçılma Faktörleri (508)
| Enerji (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 |
Ek Veriler
Estimated Crustal Abundance
The estimated element abundance in the earth's crust.
1×10-3 milligrams per kilogram
Kaynaklar (1)
- [5] Tellurium https://education.jlab.org/itselemental/ele052.html
Estimated Oceanic Abundance
The estimated element abundance in the earth's oceans.
Not Applicable
Kaynaklar (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.
Kaynaklar (1)
- [6] Tellurium https://periodic.lanl.gov/52.shtml
Kaynaklar
(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.