Tellurium

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antimony ← tellurium → iodine
Se
↑
Te
↓
Po
Appearance
silvery lustrous gray
Tellurium crystal.jpg
General properties
Name, symbol, number tellurium, Te, 52
Element category metalloid
Group, period, block 16, 5, p
Standard atomic weight 127.60 g·mol−1
Electron configuration [Kr] 4d10 5s2 5p4
Electrons per shell 2, 8, 18, 18, 6 (Image)
Physical properties
Phase solid
Density (near r.t.) 6.24 g·cm−3
Liquid density at m.p. 5.70 g·cm−3
Melting point 722.66 K, 449.51 °C, 841.12 °F
Boiling point 1261 K, 988 °C, 1810 °F
Heat of fusion 17.49 kJ·mol−1
Heat of vaporization 114.1 kJ·mol−1
Specific heat capacity (25 °C) 25.73 J·mol−1·K−1
Vapor pressure
P/Pa 1 10 100 1 k 10 k 100 k
at T/K     (775) (888) 1042 1266
Atomic properties
Oxidation states 6, 5, 4, 2, -2
(mildly acidic oxide)
Electronegativity 2.1 (Pauling scale)
Ionization energies 1st: 869.3 kJ·mol−1
2nd: 1790 kJ·mol−1
3rd: 2698 kJ·mol−1
Atomic radius 140 pm
Covalent radius 138±4 pm
Van der Waals radius 206 pm
Miscellanea
Crystal structure hexagonal
Magnetic ordering diamagnetic[1]
Thermal conductivity (300 K) (1.97–3.38) W·m−1·K−1
Speed of sound (thin rod) (20 °C) 2610 m/s
Young's modulus 43 GPa
Shear modulus 16 GPa
Bulk modulus 65 GPa
Mohs hardness 2.25
Brinell hardness 180 MPa
CAS registry number 13494-80-9
Most stable isotopes
Main article: Isotopes of tellurium
iso NA half-life DM DE (MeV) DP
120Te 0.09% >2.2×1016y ε ε 1.701 120Sn
121Te syn 16.78 d ε 1.040 121Sb
122Te 2.55% 122Te is stable with 70 neutrons
123Te 0.89% >1.0×1013 y ε 0.051 123Sb
124Te 4.74% 124Te is stable with 72 neutrons
125Te 7.07% 125Te is stable with 73 neutrons
126Te 18.84% 126Te is stable with 74 neutrons
127Te syn 9.35 h β− 0.698 127I
128Te 31.74% 2.2×1024 y β−β− 0.867 128Xe
129Te syn 69.6 min β− 1.498 129I
130Te 34.08% 7.9×1020 y β−β− 2.528 130Xe
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Tellurium (pronounced /tɪˈlʊəriəm, tɛ-/ te-LOOR-ee-əm) is a chemical element that has the symbol Te and atomic number 52. A brittle, mildly toxic, silver-white metalloid which looks similar to tin, tellurium is chemically related to selenium and sulfur. Tellurium was discovered in 1782 by Franz-Joseph Müller von Reichenstein in a mineral containing gold and tellurium. Martin Heinrich Klaproth named the new element in 1798 after the Latin word for "earth", tellus. Although several gold deposits contain tellurium minerals nearly all the tellurium is isolated in the process of copper and lead production as a by-product.

Tellurium is primarily used in alloys, foremost in steel and copper to improve machinability. Use in solar panels and as a semiconductor material also consume a considerable fraction of tellurium production.

Tellurium has no biological function, although fungi can incorporate it in place of sulfur and selenium into amino acids such as telluro-cysteine and telluro-methionine. In humans, tellurium is partly metabolized into dimethyl telluride, (CH3)2Te, a garlicky-odored gas which is exhaled in the breath of victims of tellurium toxicty or exposure.

Contents

[edit] History

Klaproth gave the named to the new element and credited von Reichenstein with its discovery

Tellurium (Latin tellus meaning "earth") was discovered in the 18th century in a gold ore from the mines in Zlatna (Klein Schlatten) close to Nagyszeben (now, Sibiu) Transylvania. This ore was known as "Faczebajer weißes blättriges Golderz" (white leafy gold ore from Faczebaja) or antimonalischer Goldkies (antimonic gold pyrite), and according to Anton von Rupprecht was Spießglaskönig (argent molybdique), containing native antimony.[2] In 1782, Franz-Joseph Müller von Reichenstein (Müller Ferenc) who was at that time Hungarian chief inspector of mines in Transylvania, concluded that the ore did not contain antimony, but that it was bismuth sulfide.[3] Next year, he reported that this was erroneous and that the ore contained mainly gold and an unknown metal very similar to antimony. After a thorough investigation which lasted for three years and consisted of more than fifty tests, Müller determined the specific gravity of the mineral and noted the radish odor of the white smoke which passed off when the new metal was heated, the red color which the metal imparts to sulfuric acid, and the black precipitate which this solution gives when diluted with water. Nevertheless, he was not able to identify this metal and gave it the name aurum paradoxium or metallum problematicum – as it did not show the properties predicted for the expected antimony.[4][5][6]

In 1789, another Hungarian scientist, Pál Kitaibel, also discovered the element independently in an ore from Deutsch-Pilsen which had been regarded as argentiferous molybdenite, but later he gave the credit to Müller. In 1798, it was named by Martin Heinrich Klaproth who earlier isolated it from the mineral calaverite.[5][6][7] Tellurium was used as a chemical bonder in the making of the outer shell of the first atom bomb. The 1960s brought growth in thermoelectric applications for tellurium, as well as its use in free-machining steel, which became the dominant use.

[edit] Characteristics

[edit] Physical

When crystalline, tellurium is silvery-white and when it is in pure state it has a metallic luster. It is a brittle and easily pulverized metalloid. Amorphous tellurium is found by precipitating it from a solution of tellurous or telluric acid (Te(OH)6).[8] However, there is some debate whether this form is really amorphous or made of minute crystals.

Tellurium is a p-type semiconductor that shows a greater conductivity in certain directions which depends on atomic alignment. Chemically related to selenium and sulfur, the conductivity of this element increases slightly when exposed to light (photoconductivity).[9]

[edit] Isotopes

Main article: isotopes of tellurium

Naturally occurring tellurium is consists of eight isotopes. Four of those isotopes, 122Te, 124Te, 125Te and 126Te, are stable. The other four, 120Te, 122Te, 128Te and 130Te, have been observed to be radioactive.[10][11] Th stable isotopes make up only 33.2 % of the natural occurring tellurium, this is possible due to the long half-lives of the instable isotopes. They are in the range from 1013 to 2.2 1024 years. This makes 128Te the isotope with the longest half life among all radioisotopes.[12]

There are 38 known nuclear isomers of tellurium with atomic masses that range from 105 to 142. Tellurium is the lightest element known to undergo alpha decay, with isotopes 106Te to 110Te being able to undergo this mode of decay.[10] The atomic mass of tellurium with 127.60 g·mol−1 exceeds that of the following element iodine 126.90 g·mol−1.[13]

[edit] Occurrence

See also: Category:Telluride minerals
Tellurium on quartz (Moctezuma, Sonora, Mexico)

With an abundance in the Earth's crust comparable to that of platinum, tellurium is one of the rarest stable solid element in the Earth's crust. Its abundance is about 1 µg/kg.[14] By comparison, even the rarest of the lanthanoids have crustal abundances of 500 µg/kg (see Abundance of elements in Earth's crust).[citation needed]

The extreme rarity of tellurium in the Earth's crust is not a reflection of its cosmic abundance, which is in fact greater than that of rubidium, even though rubidium is ten thousand times more abundant in the Earth's crust. The extraordinarily low abundance of tellurium on Earth is rather thought to be due to conditions in the Earth's formation, when the stable form of certain elements, in the absence of oxygen and water, was controlled by the reductive power of free hydrogen. Under this scenario, certain elements such as tellurium which form volatile hydrides were severely depleted during the formation of the Earth's crust, through evaporation of these hydrides. Tellurium and selenium are the heavy elements most depleted in the Earth's crust by this process.[citation needed]

Tellurium is sometimes found in its native (elemental) form, but is more often found as the tellurides of gold (calaverite, krennerite, petzite, sylvanite, and others). Tellurium compounds are the most common chemical compounds of gold found in nature (rare non-tellurides such as gold aurostibite and bismuthide are known). Tellurium is also found combined with elements other than gold, in salts of other metals. In contrast to selenium, tellurium is not able to replace sulfur in its minerals. This is due to the large difference in ion radius of sulfur and tellurium. In consequence, many sulfide minerals contain considerable amounts of selenium, but only traces of tellurium.[15]

[edit] Compounds and chemistry

See also: Category:Tellurium compounds

Tellurium belongs to the same chemical family as oxygen, sulfur, selenium, and polonium: the chalcogen family. It forms similar compounds to sulfur and selenium. It exhibits the oxidation states −2, +2, +4, and +6, with the +4 state being most common.[8]

Tellurides

The −2 oxidation state is exhibited in binary compounds with many metals, such as zinc telluride, ZnTe, formed by heating tellurium with zinc.[16] Decomposition of ZnTe with hydrochloric acid yields hydrogen telluride, H2Te, the tellurium analogue of the other chalcogen hydrides, H2O, H2S, and H2Se:

ZnTe + 2 HCl → ZnCl2 + H2Te

H2Te reacts with many metals to form tellurides, containing the Te2− anion.[16] Gold and silver tellurides are considered good ores.

Halides

The +2 oxidation state is exhibited by the monoxide, TeO, and the dihalides, TeCl2, TeBr2, and TeI2. The dihalides have not been obtained in pure form,[17]:274 although they are known decomposition products of the tetrahalides in organic solvents, and their derived tetrahalotellurates are well-characterized:

Te + X2 + 2 X− → TeX2−4

where X is Cl, Br, or I. These anions are square planar in geometry.[17]:281 Polynuclear anionic species also exist, such as the dark brown Te2I2−6,[17]:283 and the black Te4I2−14.[17]:285

Fluorine forms two halides with tellurium: the mixed-valence Te2F4, and TeF6. In the +6 oxidation state, the –OTeF5 structural group occurs in a number of compounds such as HOTeF5, B(OTeF5)3, Xe(OTeF5)2, Te(OTeF5)4, and Te(OTeF5)6.[18] The square antiprismic anion TeF2−8 is also attested.[19] The other halogens do not form halides with tellurium in the +6 oxidation state, but only tetrahalides (TeCl4, TeBr4, and TeI4) in the +4 state, and other lower halides (Te3Cl2, Te2Cl2, Te2Br2, Te2I, and two forms of TeI). In the +4 oxidation state, halotellurate anions are known, such as TeCl2−6 and Te2Cl2−10. Halotellurium cations are also attested, including TeI+3, found in TeI3AsF6.[20]

Oxocompounds
A sample of tellurium dioxide powder

Tellurium monoxide was first reported in 1883 as a black amorphous solid formed by the heat decomposition of TeSO3 in vacuum, disproportionating into tellurium dioxide, TeO2, and elemental tellurium upon heating.[21][22] Since then, however, some doubt has been cast on its existence in the solid phase, although it is known as a vapor phase fragment; the black solid may be merely an equimolar mixture of elemental tellurium and tellurium dioxide.[23]

Tellurium dioxide is formed by heating tellurium in air, causing it to burn with a blue flame.[16] Tellurium trioxide, β-TeO3, is obtained by thermal decomposition of Te(OH)6. The other two forms of trioxide reported in the literature, the α- and γ- forms, were found not to be true oxides of tellurium in the +6 oxidation state, but a mixture of Te4+, OH−, and O−2.[24] Tellurium also exhibits mixed-valence oxides, Te2O5 and Te4O9.[24]

The tellurium oxides and hydrated oxides form a series of acids, including tellurous acid (H2TeO3), orthotelluric acid (Te(OH)6), and metatelluric acid ((H2TeO4)n).[23] The two forms of telluric acid form tellurate salts containing the TeO2−4 and TeO6−6 anions, respectively. Tellurous acid forms tellurite salts containing the anion TeO2−3. Other tellurium cations include TeF2+8, which consists of two fused tellurium rings, and the polymeric TeF2+7.

Zintl cations

When tellurium is treated with concentrated sulfuric acid, it forms red solutions containing the Zintl ion, Te2+4. The oxidation of tellurium by AsF5 in liquid SO2 also produces this square planar cation, as well as with the trigonal prismatic, yellow-orange Te4+6:[19]

4 Te + 3 AsF5 → Te2+4(AsF−6)2 + AsF3
6 Te + 6 AsF5 → Te4+6(AsF−6)4 + 2 AsF3

Other tellurium Zintl cations include the polymeric Te2+7, and the blue-black Te2+8, which consists of two fused 5-membered tellurium rings. The latter cation is formed by the reaction of tellurium with tungsten hexachloride:[19]

8 Te + 2 WCl6 → Te2+8(WCl−6)2

Interchalcogen cations also exist, such as Te2Se2+6 (distorted cubic geometry) and Te2Se2+8. These are formed by oxidizing mixtures of tellurium and selenium with AsF5 or SbF5.[19]

Organotellurium copounds

In organic chemistry, tellurium forms analogues of alcohols and thiols, having the functional group –TeH, called tellurols. The –TeH functional group is also referred towith the prefix tellanyl-.[25]

[edit] Production

The principal source of tellurium is from anode sludges produced during the electrolytic refining of blister copper. It is a component of dusts from blast furnace refining of lead. Treatment of 500 tons of copper ore typically yields one pound (0.45 kg) of tellurium. Tellurium is produced mainly in the United States, Canada, Peru, and Japan.[26] For the year 2006 the British Geological Survey gives the following numbers: Canada 11 t United States 50 t , Peru 37 t and Japan 24 t.[27]

Grey and white world map with four countries colored to show the percentage of world wide tellurium production. US to produce 40%; Peru to produce 30%; Japan to produce 20%;and Canada to produce 10%
Tellurium production 2006

The anode sludges contain the selenides and tellurides of the noble metals in compounds with the formula M2Se or M2Te (M = Cu, Ag, Au). At temperatures of 500°C the anode sludges are roasted with sodium carbonate under air. The metals are reduced to the metals, while the tellurium is converted to sodium tellurite.[19]

M2Te + O2 + Na2CO3 → Na2TeO3 + 2M + CO2

The tellurites can be leached from the mixture with water. The tellurites normally are present as hydrotellurites HTeO3- in solution. The also formed selenates can be separated by adding sulfuric acid. The hydrotellurites are converted into the insoluble tellurium dioxide while the selenites stay in solution.[19]

HTeO3- + OH- +H2SO4 → TeO2 + 2SO42- + 2H2O

The reduction to the metal is done either by electrolysis or by reacting the tellurium dioxide with sulfur dioxide in sulfuric acid.[19]

TeO2 + 2SO2 + 2H2O → Te + SO42- + 4H+

Commercial-grade tellurium is usually marketed as minus 200-mesh powder but is also available as slabs, ingots, sticks, or lumps. The year-end price for tellurium in 2000 was US$14 per pound. In recent years, the tellurium price was driven up by increased demand and limited supply, reaching as high as US$100 per pound in 2006.[28][29]

[edit] Applications

[edit] Metallurgy

The largest consumer of tellurium is metallurgy, where it is used in iron, copper and lead alloys. When added to stainless steel and copper it makes these metals more machinable. It is alloyed into cast iron for promoting chill for spectroscopic purposes, as the presence of electrically conductive free graphite tends to deleteriously effect spark emission testing results. In lead it improves strength and durability, and decreases the corrosive action of sulfuric acid.[30]

[edit] Semiconductor and electronic industry uses

A CdTe photovoltaic array

Tellurium is used in cadmium telluride (CdTe) solar panels. National Renewable Energy Laboratory lab tests using this material achieved some of the highest efficiencies for solar cell electric power generation. Massive commercial production of CdTe solar panels by First Solar in recent years has significantly increased tellurium demand.[31][32] If some of the cadmium in CdTe is replaced by zinc then CdZnTe is formed which is used in solid-state x-ray detectors.[33]

Alloyed with both cadmium and mercury, to form mercury cadmium telluride, an infrared sensitive semiconductor material is formed.[34] Organotellurium compounds such as dimethyl telluride, diethyl telluride, diisopropyl telluride, diallyl telluride and methyl allyl telluride are used as precursors for Metalorganic vapour phase epitaxy growth of II-VI compound semiconductors. Diisopropyl telluride (DIPTe) is employed as the preferred precursor for achieving the low temperature growth of CdHgTe by MOVPE.[35] For these process high purity metalorganics of both selenium and tellurium are used. The compounds for semiconductor industry, and are prepared by adduct purification.[36][37]

Tellurium as a tellurium suboxide is used in the media layer of several types of rewritable optical discs, including ReWritable Compact Discs (CD-RW), ReWritable Digital Video Discs (DVD-RW) and ReWritable Blu-ray Discs.[38][39]

Tellurium is used in the new phase change memory chips[40] developed by Intel.[41] Bismuth telluride (Bi2Te3) is used in thermoelectric devices.

[edit] Other uses

[edit] Precautions

Tellurium and tellurium compounds are considered to be mildly toxic and need to be handled with care, although acute poisoning is rare.[48] Tellurium is not reported to be carcinogenic.[48]

Humans exposed to as little as 0.01 mg/m3 or less in air develop "tellurium breath", which has a garlic-like odor.[42] The garlic odor that is associated with human intake of tellurium compounds is caused from the tellurium being metabolized by the body. When the body metabolizes tellurium in any oxidation state, the tellurium gets converted into dimethyl telluride, (CH3)2Te, which is volatile and is the cause of the garlic-like smell. Even though the metabolic pathways of tellurium are not known, it is generally assumed that they resemble those of the more extensively studied selenium, because the final methylated metabolic products of the two elements are similar.[49][50][51]

[edit] References

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