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(ăn'tə-mō') pronunciation
n. (Symbol Sb)
A metallic element having four allotropic forms, the most common of which is a hard, extremely brittle, lustrous, silver-white, crystalline material. It is used in a wide variety of alloys, especially with lead in battery plates, and in the manufacture of flame-proofing compounds, paint, semiconductor devices, and ceramic products. Atomic number 51; atomic weight 121.76; melting point 630.5°C; boiling point 1,380°C; specific gravity 6.691; valence 3, 5.

[Middle English antimonie, from Medieval Latin antimōnium, perhaps from Arabic al-'iṯmid : al-, the + 'iṯmid, antimony (perhaps from Greek stimmi).]


antimony

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Semimetallic to metallic chemical element (see metal), chemical symbol Sb, atomic number 51. Of its various allotropes, the most common is a lustrous, bluish, brittle, flaky solid. In nature antimony occurs chiefly as the gray sulfide mineral stibnite, Sb2S3. Pure antimony metal has no important uses, but its alloys and compounds are extremely useful. Some antimony alloys have the rare quality of expanding on solidifying; these are used for castings and for type metal. Alloys with lead are used in car batteries, bullets, and cable sheaths. Antifriction alloys with tin and lead (babbitt metals) are used as components of machine bearings. Antimony compounds (valences 3, 4, and 5) are widely used as flame retardants in paints, plastics, rubber, and textiles; others are used as paint pigments.

For more information on antimony, visit Britannica.com.

A chemical element, symbol Sb, atomic number 51. Antimony is not a naturally abundant element; it is occasionally found native, often in isomorphous mixture with arsenic, as allemonite. The symbol Sb is derived from the Latin name stibium. See also Periodic table.

The element is dimorphic, existing as a yellow, metastable form composed of Sb4 molecules, as in antimony vapor and the structural unit in yellow antimony; and a gray, metallic form, which crystallizes with a layered rhombohedral structure. Antimony differs from normal metals in having a lower electrical conductivity as a solid than as a liquid (as does its congener, bismuth). Metallic antimony is quite brittle, bluish-white with a typical metallic luster, but a flaky appearance. Although stable in air at normal temperatures, it burns brilliantly when heated, with the formation of a white smoke of Sb2O3. Vaporization of the metal gives molecules of Sb4O6, which break down to Sb2O3 above the transition temperature.

Antimony occurs in nature mainly as Sb2S3 (stibnite, antimonite); Sb2O3 (valentinite) occurs as a decomposition product of stibnite. Antimony is commonly found in ores of copper, silver, and lead. The metal antimonides NiSb (breithaupite), NiSbS (ullmannite), and Ag2Sb (dicrasite) also are found naturally; there are numerous thioantimonates such as Ag3SbS3 (pyrargyrite).

Antimony is produced either by roasting the sulfide with iron, or by roasting the sulfide and reducing the sublimate of Sb4O6 thus produced with carbon; high-purity antimony is produced by electrolytic refining.

Commercial-grade antimony is used in many alloys (1–20%), especially lead alloys, which are much harder and mechanically stronger than pure lead; batteries, cable sheathing, antifriction bearings, and type metal consume almost half of all the antimony produced. The valuable property of Sn-Sb-Pb alloys, that they expand on cooling from the melt, thus enabling the production of sharp castings, makes them especially useful as type metal.


Toxic metal of no known metabolic function, and therefore not a dietary essential. Antimony compounds are used in treatment of some parasitic diseases.

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antimony (ăn'tĭmō'nē) [Lat. antimoneum], semimetallic chemical element; symbol Sb [Lat. stibium,=a mark]; at. no. 51; at. wt. 121.760; m.p. 630.74°C; b.p. 1,750°C; sp. gr. (metallic form) 6.69 at 20°C; valence 0, +3, −3, or +5. Antimony exists in two allotropic forms (see allotropy); the more common is silvery blue-white and has a rhombohedral crystalline structure. It is a poor conductor of heat and electricity and is brittle and easily powdered. It is primarily used in alloys and chemical compounds. It is a member of Group 15 of the periodic table. Antimony rarely occurs free in nature, but its ores are widely distributed. The principal ore is stibnite, a sulfur compound known since early times; there are extensive deposits in China. Antimony is often found in other ores as well, e.g., silver, copper, and lead. The pure element antimony is produced from the ore by roasting it to form the oxide, then reducing the oxide with carbon or iron; often a flux of sodium sulfate or sodium carbonate is used to prevent loss of molten antimony by evaporation. Antimony does not react with air or water at room temperature; it does react with fluorine, chlorine, or bromine and is soluble in hot nitric or sulfuric acid; at higher temperatures, antimony will ignite and burn in air. It unites with hydrogen to form stibine, a poisonous gas. In combination with metals antimony forms alloys that are hard and brittle and have low melting points. The alloys of antimony include britannia metal, type metal, Babbitt metal, and sometimes pewter; these alloys expand on cooling, thereby retaining fine details of a mold. Alloys and compounds of antimony are used in bearings, storage batteries, safety matches, and as a red pigment in paint. Although antimony and many of its compounds are toxic, tartar emetic (potassium antimonyl tartrate) is used as a medicine. Small concentrations of antimony can be detected by a method similar to the Marsh test for arsenic. Antimony is mixed with soot and other substances to make kohl, used for centuries by women in some countries as an eye cosmetic. A method for the extraction of antimony from stibnite was first described c.1600 by Basilius Valentinus. Although known to the ancients, the element was first adequately described by Nicolas Lémery in 1707.


A chemical element, atomic number 51, atomic weight 121.75, symbol Sb. Trivalent and pentavalent antimony compounds are used in medicine as anti-infective agents in the treatment of tropical diseases, especially those of protozoan origin. All antimony compounds are potentially poisonous and must be used with caution. See also stibogluconate, meglumine.

  • a. poisoning — resembles arsenic poisoning. Signs include vomiting and diarrhea. Postmortem lesions are those of gastroenteritis.
  • a. potassium tartrate — a nauseant expectorant and ruminatoric. Also used as an antiparasitic agent in schistosomiasis, trypanosomiasis and leishmaniasis. Called also tarter emetic.

n

A bluish crystalline metallic element occurring in nature both free and as salts. Antimony compounds are used in the treatment of filariasis, leishmaniasis, and other parasitic diseases. Antimony is also used as an emetic.

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categories related to 'antimony'

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Random House Word Menu by Stephen Glazier
For a list of words related to antimony, see:

  See crossword solutions for the clue Antimony.
tinantimonytellurium
As

Sb

Bi
Appearance
silvery lustrous gray
General properties
Name, symbol, number antimony, Sb, 51
Pronunciation /ˈæntɨmɵnɪ/
AN-ti-mo-nee[note 1]
Element category metalloid
Group, period, block 155, p
Standard atomic weight 121.760(1)
Electron configuration [Kr] 4d10 5s2 5p3
Electrons per shell 2, 8, 18, 18, 5 (Image)
Physical properties
Phase solid
Density (near r.t.) 6.697 g·cm−3
Liquid density at m.p. 6.53 g·cm−3
Melting point 903.78 K, 630.63 °C, 1167.13 °F
Boiling point 1860 K, 1587 °C, 2889 °F
Heat of fusion 19.79 kJ·mol−1
Heat of vaporization 193.43 kJ·mol−1
Molar heat capacity 25.23 J·mol−1·K−1
Vapor pressure
P (Pa) 1 10 100 1 k 10 k 100 k
at T (K) 807 876 1011 1219 1491 1858
Atomic properties
Oxidation states 5, 3, -3
Electronegativity 2.05 (Pauling scale)
Ionization energies
(more)
1st: 834 kJ·mol−1
2nd: 1594.9 kJ·mol−1
3rd: 2440 kJ·mol−1
Atomic radius 140 pm
Covalent radius 139±5 pm
Van der Waals radius 206 pm
Miscellanea
Crystal structure trigonal
Magnetic ordering diamagnetic[1]
Electrical resistivity (20 °C) 417 nΩ·m
Thermal conductivity 24.4 W·m−1·K−1
Thermal expansion (25 °C) 11 µm·m−1·K−1
Speed of sound (thin rod) (20 °C) 3420 m·s−1
Young's modulus 55 GPa
Shear modulus 20 GPa
Bulk modulus 42 GPa
Mohs hardness 3.0
Brinell hardness 294 MPa
CAS registry number 7440-36-0
Most stable isotopes
Main article: Isotopes of antimony
iso NA half-life DM DE (MeV) DP
121Sb 57.36% 121Sb is stable with 70 neutrons
123Sb 42.64% 123Sb is stable with 72 neutrons
125Sb syn 2.7582 y β 0.767 125Te
· r

Antimony (play /ænˈtɪmɵni/ an-TI-mo-nee or play /ˈæntəˌmni/ AN-tə-MOH-nee;[note 2] Latin: stibium) is a toxic chemical element with the symbol Sb and an atomic number of 51. A lustrous grey metalloid, it is found in nature mainly as the sulfide mineral stibnite (Sb2S3). Antimony compounds have been known since ancient times and were used for cosmetics; metallic antimony was also known, but it was erroneously identified as lead. It was established to be an element around the 17th century.

For some time, China has been the largest producer of antimony and its compounds, with most production coming from the Xikuangshan Mine in Hunan. The industrial methods to produce antimony are roasting and subsequent carbothermal reduction or direct reduction of stibnite with iron.

The largest applications for metallic antimony are as alloying material for lead and tin and for lead antimony plates in lead-acid batteries. Alloying lead and tin with antimony improves the properties of the alloys which are used in solders, bullets and plain bearings. Antimony compounds are prominent additives for chlorine- and bromine-containing fire retardants found in many commercial and domestic products. An emerging application is the use of antimony in microelectronics.

Contents

Characteristics

Properties

A clear vial containing small chunks of a slightly lustrous black solid, labeled "Sb".
A vial containing the black allotrope of antimony
An irregular piece of silvery stone with spots of variation in lustre and shade.
Native antimony with oxidation products
Crystal structure common to Sb, AsSb and grey As

Antimony is in the nitrogen group (group 15) and has an electronegativity of 2.05. As expected by periodic trends, it is more electronegative than tin or bismuth, and less electronegative than tellurium or arsenic. Antimony is stable in air at room temperature, but reacts with oxygen if heated to form antimony trioxide, Sb2O3.[2]:758

Antimony is a silvery, lustrous gray metal that has a Mohs scale hardness of 3. Therefore, pure antimony is not used to make hard objects: coins made of antimony were issued in China's Guizhou province in 1931, but because of their rapid wear, their minting was discontinued.[3] Antimony is resistant to attack by acids.

Four allotropes of antimony are known, a stable metallic form and three metastable forms, explosive, black and yellow. Metallic antimony is a brittle, silver-white shiny metal. When molten antimony is slowly cooled, metallic antimony crystallizes in a trigonal cell, isomorphic with that of the grey allotrope of arsenic. A rare explosive form of antimony can be formed from the electrolysis of antimony(III) trichloride. When scratched with a sharp implement, an exothermic reaction occurs and white fumes are given off as metallic antimony is formed; when rubbed with a pestle in a mortar, a strong detonation occurs. Black antimony is formed upon rapid cooling of vapour derived from metallic antimony. It has the same crystal structure as red phosphorus and black arsenic, it oxidizes in air and may ignite spontaneously. At 100 °C, it gradually transforms into the stable form. The yellow allotrope of antimony is the most unstable. It has only been generated by oxidation of stibine (SbH3) at −90 °C. Above this temperature and in ambient light, this metastable allotrope transforms into the more stable black allotrope.[4][5][6]

Metallic antimony adopts a layered structure (space group R3m No. 166) in which layers consist of fused ruffled six-membered rings. The nearest and next-nearest neighbors form a distorted octahedral complex, with the three atoms in the same double-layer being slightly closer than the three atoms in the next. This relatively close packing leads to a high density of 6.697 g/cm3, but the weak bonding between the layers leads to the low hardness and brittleness of antimony.[2]:758

Isotopes

Antimony exists as two stable isotopes, 121Sb with a natural abundance of 57.36% and 123Sb with a natural abundance of 42.64%. It also has 35 radioisotopes, of which the longest-lived is 125Sb with a half-life of 2.75 years. In addition, 29 metastable states have been characterised. The most stable of these is 124Sb with a half-life of 60.20 days, which has an application in some neutron sources. Isotopes that are lighter than the stable 123Sb tend to decay by β+ decay, and those that are heavier tend to decay by β- decay, with some exceptions.[7]

Occurrence

Stibnite

The abundance of antimony in the Earth's crust is estimated at 0.2 to 0.5 parts per million, comparable to thallium at 0.5 parts per million and silver at 0.07 ppm.[8] Even though this element is not abundant, it is found in over 100 mineral species. Antimony is sometimes found natively, but more frequently it is found in the sulfide stibnite (Sb2S3) which is the predominant ore mineral.[8]

Compounds

Antimony compounds are often classified into those of Sb(III) and Sb(V).[9] Relative to its congener arsenic, the +5 oxidation state is more stable.

Oxides and hydroxides

Antimony trioxide (Sb4O6) is formed when antimony is burnt in air.[10] In the gas phase, this compound exists as Sb4O6, but it polymerises upon condensing.[2] Antimony pentoxide (Sb4O10) can only be formed by oxidation by concentrated nitric acid.[11] Antimony also forms a mixed-valence oxide, antimony tetroxide (Sb2O4), which features both Sb(III) and Sb(V).[11] Unlike phosphorus and arsenic, these various oxides are amphoteric, do not form well-defined oxoacids and react with acids to form antimony salts.

Antimonous acid Sb(OH)3 is unknown, but the conjugate base sodium antimonite ([Na3SbO3]4) forms upon fusing sodium oxide and Sb4O6.[2]:763 Transition metal antimonites are also known.[12]:122 Antimonic acid exists only as the hydrate HSb(OH)6, forming salts containing the antimonate anion Sb(OH)
6
. Dehydrating metal salts containing this anion yields mixed oxides.[12]:143

Many antimony ores are sulfides, including stibnite (Sb2S3), pyrargyrite (Ag3SbS3), zinkenite, jamesonite, and boulangerite.[2]:757 Antimony pentasulfide is non-stoichiometric and features antimony in the +3 oxidation state and S-S bonds.[13] Several thioantimonides are known, such as [Sb6S10]2− and [Sb8S13]2−.[14]

Halides

Antimony forms two series of halides, SbX3 and SbX5. The trihalides SbF3, SbCl3, SbBr3, and SbI3 are all molecular compounds having trigonal pyramidal molecular geometry. The trifluoride SbF3 is prepared by the reaction of Sb2O3 with HF:[2]:761–762

Sb2O3 + 6 HF → 2 SbF3 + 3 H2O

It is Lewis acidic and readily accepts fluoride ions to form the complex anions SbF
4
and SbF2−
5
. Molten SbF3 is a weak electrical conductor. The trichloride SbCl3 is prepared by dissolving Sb2S3 in hydrochloric acid:

Sb2S3 + 6 HCl → 2 SbCl3 + 3 H2S
Structure of gaseous SbF5

The pentahalides SbF5 and SbCl5 have trigonal bipyramidal molecular geometry in the gas phase, but in the liquid phase, SbF5 is polymeric, whereas SbCl5 is monomeric.[2]:761 SbF5 is a powerful Lewis acid used to make the superacid fluoroantimonic acid ("HSbF6").

Oxyhalides are more common for antimony than arsenic and phosphorus. Antimony trioxide dissolves in concentrated acid to form oxoantimonyl compounds such as SbOCl and (SbO)2SO4.[2]:764

Antimonides, hydrides, and organoantimony compounds

Compounds in this class generally are described as derivatives of Sb3-. Antimony forms antimonides with metals, such as indium antimonide (InSb) and silver antimonide (Ag3Sb).[2]:760 The alkali metal and zinc antimonides, such as Na3Sb and Zn3Sb2, are more reactive. Treating these antimonides with acid produces the unstable gas stibine, SbH3:[15]

Sb3− + 3 H+SbH3

Stibine can also be produced by treating Sb3+ salts with hydride reagents such as sodium borohydride. Stibine decomposes spontaneously at room temperature. Because stibine has a positive heat of formation, it is thermodynamically unstable and thus antimony does not react with hydrogen directly.[9]

Organoantimony compounds are typically prepared by alkylation of antimony halides with Grignard reagents.[16] A large variety of compounds are known with both Sb(III) and Sb(V) centers, including mixed chloro-organic derivatives, anions, and cations. Examples include Sb(C6H5)3 (triphenylstibine), Sb2(C6H5)4 (with an Sb-Sb bond), and cyclic [Sb(C6H5)]n. Pentacoordinated organoantimony compounds are common, examples being Sb(C6H5)5 and several related halides.

History

An unshaded circle surmounted by a cross.
One of the alchemical symbols for antimony

Antimony(III) sulfide, Sb2S3, was recognized in predynastic Egypt as an eye cosmetic (kohl) as early as about 3100 BC, when the cosmetic palette was invented.[17]

An artifact, said to be part of a vase, made of antimony dating to about 3000 BC was found at Telloh, Chaldea (part of present-day Iraq), and a copper object plated with antimony dating between 2500 BC and 2200 BC has been found in Egypt.[4] Austen, at a lecture by Herbert Gladstone in 1892[18] commented that "we only know of antimony at the present day as a highly brittle and crystalline metal, which could hardly be fashioned into a useful vase, and therefore this remarkable 'find' (artifact mentioned above) must represent the lost art of rendering antimony malleable."[18] However, Moorey was unconvinced the artefact was indeed a vase, mentioning that Selimkhanov, after his analysis of the Tello object (published in 1975), "attempted to relate the metal to Transcaucasian natural antimony" (i.e. native metal) and that "the antimony objects from Transcaucasia are all small personal ornaments."[18] This weakens the evidence for a lost art "of rendering antimony malleable."[18]

The first European description of a procedure for isolating antimony is in the book De la pirotechnia of 1540 by Vannoccio Biringuccio; this predates the more famous 1556 book by Agricola, De re metallica. In this context Agricola has been often incorrectly credited with the discovery of metallic antimony. The book Currus Triumphalis Antimonii (The Triumphal Chariot of Antimony), describing the preparation of metallic antimony, was published in Germany in 1604. It was purported to have been written by a Benedictine monk, writing under the name Basilius Valentinus, in the 15th century; if it were authentic, it would predate Biringuccio.[note 3][20][5][21]

Pure antimony was well known to Jābir ibn Hayyān in the 8th century. There is an ongoing controversy, with translator Marcellin Berthelot stating antimony was never found in Jābir's books, but others claiming[5][22] that Berthelot translated only some of the less important books, while the more interesting ones (some of which might describe antimony) are not yet translated, and their content is completely unknown.[23]

The first natural occurrence of pure antimony in the Earth's crust was described by the Swedish scientist and local mine district engineer Anton von Swab in 1783; the type-sample was collected from the Sala Silver Mine in the Bergslagen mining district of Sala, Västmanland, Sweden.[24][25]

Etymology

The ancient words for antimony mostly have, as their chief meaning, kohl, the sulfide of antimony. Pliny the Elder, however, distinguishes between male and female forms of antimony; the male form is probably the sulfide, while the female form, which is superior, heavier, and less friable, has been suspected to be native metallic antimony.[26]

The Egyptians called antimony mśdmt; in hieroglyphs, the vowels are uncertain, but there is an Arabic tradition that the word is ميسديميت mesdemet.[27][28] The Greek word, στίμμι stimmi, is probably a loan word from Arabic or Egyptian sdm

O34
D46
G17 F21
D4

and is used by Attic tragic poets of the 5th century BC; later Greeks also used στἰβι stibi, as did Celsus and Pliny, writing in Latin, in the first century AD. Pliny also gives the names stimi [sic], larbaris, alabaster, and the "very common" platyophthalmos, "wide-eye" (from the effect of the cosmetic). Later Latin authors adapted the word to Latin as stibium. The Arabic word for the substance, as opposed to the cosmetic, can appear as إثمد ithmid, athmoud, othmod, or uthmod. Littré suggests the first form, which is the earliest, derives from stimmida, an accusative for stimmi.[29]

The use of Sb as the standard chemical symbol for antimony is due to Jöns Jakob Berzelius, who used this abbreviation of the name stibium.[30] The medieval Latin form, from which the modern languages and late Byzantine Greek take their names for antimony, is antimonium. The origin of this is uncertain; all suggestions have some difficulty either of form or interpretation. The popular etymology, from ἀντίμοναχός anti-monachos or French antimoine, still has adherents; this would mean "monk-killer", and is explained by many early alchemists being monks, and antimony being poisonous.[note 4] Another popular etymology is the hypothetical Greek word ἀντίμόνος antimonos, "against aloneness", explained as "not found as metal", or "not found unalloyed".[4][31] Lippmann conjectured a hypothetical Greek word ανθήμόνιον anthemonion, which would mean "floret", and cites several examples of related Greek words (but not that one) which describe chemical or biological efflorescence.[32]

The early uses of antimonium include the translations, in 1050–1100, by Constantine the African of Arabic medical treatises.[33] Several authorities believe antimonium is a scribal corruption of some Arabic form; Meyerhof derives it from ithmid;[34] other possibilities include athimar, the Arabic name of the metalloid, and a hypothetical as-stimmi, derived from or parallel to the Greek.[35][36]

Production

Antimony output in 2010[8]
World production trend of antimony

Top producers and production volumes

The British Geological Survey reported that in 2005, the People's Republic of China was the top producer of antimony with an approximately 84% world share, followed at a distance by South Africa, Bolivia and Tajikistan. Xikuangshan Mine in Hunan province has the largest deposits in China with an estimated deposit of 2.1 million metric tons.[37]

In 2010, according to the US Geological Survey, China accounted for the 88.9% of total antimony production.

Antimony production in 2010[8]
Country Tonnes  % of total
 People's Republic of China 120,000 88.9
 South Africa 3,000 2.2
 Bolivia 3,000 2.2
 Russia 3,000 2.2
 Tajikistan 2,000 1.5
Top 5 131,000 97.0
Total world 135,000 100.0

However, Roskill Consulting estimates for primary production show that in 2010 China held a 76.75% share of world’s supply with 120,462 tonnes (90,000 tonnes of reported and 30,464 tonnes of un-reported production), followed by Russia (4.14% share, 6,500 tonnes of production), Myanmar (3.76% share, 5,897 tonnes), Canada (3.61% share, 5,660 tonnes), Tajikistan (3.42% share, 5,370 tonnes) and Bolivia (3.17% share, 4,980 tonnes)[38].

Roskill estimates that secondary production globally in 2010 was 39,540 tonnes.[38]

Antimony was ranked first in a Risk List published by the British Geological Survey in the second half 2011. The list provides an indication of the relative risk to the supply of chemical elements or element groups required to maintain the current British economy and lifestyle[39].

Also, antimony was identified as one of 12 critical raw materials for the EU in a report published in 2011, primarily due to the lack of supply outside China[40].

Reported production of antimony in China fell in 2010 and is unlikely to increase in the coming years, according to the Roskill report. No significant antimony deposits in Chinahave been developed for about ten years and the remaining economic reserves are being rapidly depleted.[38]

The world's largest antimony producers, according to Roskill, are listed below:

Largest antimony producers in 2010.[41]
Country Company Capacity (tonnes per year)
 Australia Mandalay Resources 2,750
 Bolivia various 5,460
 Canada Beaver Brook 6,000
 China Hsikwangshan Twinkling Star 55,000
 China Hunan Chenzhou Mining 20,000
 China China Tin Group 20,000
 China Shenyang Huacheng Antimony 15,000
 Kazakhstan Kazzinc 1,000
 Kyrgyzstan Kadamdzhai 500
 Laos SRS 500
 Mexico US Antimony 70
 Myanmar various 6,000
 Russia GeoProMining 6,500
 South Africa Consolidated Murchison 6,000
 Tajikistan Unzob 5,500
 Thailand unknown 600
 Turkey Cengiz & Özdemir Antimuan Madenleri 2,400

Reserves

According to statistics from the US Geological Survey (USGS), current global reserves of antimony will be depleted in 13 years. However, the United States Geological Survey expects more resources will be found.

World Antimony Reserves in 2010[41]
Country Reserves (tonnes of antimony content)  % of total
 People's Republic of China 950,000 51.88
 Russia 350,000 19.12
 Bolivia 310,000 16.93
 Tajikistan 50,000 2.73
 South Africa 21,000 1.15
Other countries 150,000 8.19
Total world 1,831,000 100.0

Production process

The extraction of antimony from ores depends on the quality of the ore and composition of the ore. Most antimony is mined as the sulfide; lower grade ores are concentrated by froth flotation, while higher grade ores are heated to 500–600°C, the temperature at which stibnite melts and is separated from the gangue minerals. Antimony can be isolated from the crude antimony sulfide by a reduction with scrap iron:[42]

Sb2S3 + 3 Fe → 2 Sb + 3 FeS

The sulfide is converted to an oxide and advantage is often taken of the volatility of antimony(III) oxide, which is recovered from roasting.[43] This material is often used directly for the main applications, impurities being arsenic and sulfide.[44][45] Isolating antimony from its oxide is performed by a carbothermal reduction:[42][44]

2 Sb2O3 + 3 C → 4 Sb + 3 CO2

The lower grade ores are reduced in blast furnaces while the higher grade ores are reduced in reverberatory furnaces.[42]

Applications

60% of antimony produced is used as a flame retardants, while 20% is used in alloys for batteries, plain bearings and solders.[42]

Flame retardants

Antimony is mainly used as its trioxide in making flame-proofing compounds. It is nearly always used in combination with halogenated flame retardants, with the only exception being in halogen-containing polymers. The formation of halogenated antimony compounds is the cause for the flame retarding effect of antimony trioxide.[46] Markets for these flame-retardant applications include children's clothing, toys, aircraft and automobile seat covers. It is also used in the fiberglass composites industry as an additive to polyester resins for such items as light aircraft engine covers. The resin will burn while a flame is held to it but will extinguish itself as soon as the flame is removed.[43][47]

Alloys

Antimony forms a highly useful alloy with lead, increasing its hardness and mechanical strength. For most applications involving lead, varying amounts of antimony are used as alloying metal. In lead–acid batteries, this addition improves the charging characteristics and reduces generation of unwanted hydrogen during charging.[43][48] It is used in antifriction alloys (such as Babbitt metal),[49] in bullets and lead shot, cable sheathing, type metal (for example, for linotype printing machines[50]), solder (some "lead-free" solders contain 5% Sb),[51] in pewter,[52] and in hardening alloys with low tin content in the manufacturing of organ pipes.

Other applications

Three other applications make up nearly all the rest of the consumption.[42] One of these uses is as a stabilizer and a catalyst for the production of polyethyleneterephthalate.[42] Another application is to serve as a fining agent to remove microscopic bubbles in glass, mostly for TV screens.[53] The third major application is the use as pigment.[42] Antimony is increasingly being used in the semiconductor industry as a dopant for ultra-high conductivity n-type silicon wafers[54] in the production of diodes, infrared detectors, and Hall-effect devices. In the 1950s, tiny beads of a lead-antimony alloy were used to dope the emitters and collectors of NPN alloy junction transistors with antimony.[55] Indium antimonide is used as a material for mid-infrared detectors.[56][57][58]

Captain James Cook's antimonial cup

Few biological or medical applications exist for antimony. Treatments principally containing antimony are known as antimonials and are used as emetics.[59] Antimony compounds are used as antiprotozoan drugs. Potassium antimonyl tartrate, or tartar emetic, was once used as an anti-schistosomal drug from 1919 on. It was subsequently replaced by praziquantel.[60] Antimony and its compounds are used in several veterinary preparations like anthiomaline or lithium antimony thiomalate, which is used as a skin conditioner in ruminants.[61] Antimony has a nourishing or conditioning effect on keratinized tissues, at least in animals.

Antimony-based drugs, such as meglumine antimoniate, are also considered the drugs of choice for treatment of leishmaniasis in domestic animals. Unfortunately, as well as having low therapeutic indices, the drugs are poor at penetrating the bone marrow, where some of the Leishmania amastigotes reside, and so cure of the disease – especially the visceral form – is very difficult.[62] Elemental antimony as an antimony pill was once used as a medicine. It could be reused by others after ingestion.[63]

In the heads of some safety matches, antimony(III) sulfide is used.[64][65] Antimony-124 is used together with beryllium in neutron sources; the gamma rays emitted by antimony-124 initiate the photodisintegration of beryllium.[66][67] The emmited neutrons have an average of 24 keV.[68] Antimony sulfides have been shown to help stabilize the friction coefficient in automotive brake pad materials.[69] Antimony also is used in the making of bullets and bullet tracers.[70] This element is also used in traditional cosmetics,[71][72] event paint and glass art crafts. An application as an opacifier in enamel declined in use after the 1930s, after several intoxications were reported.[64][73]

Precautions

Antimony and many of its compounds are toxic, and the effects of antimony poisoning are similar to arsenic poisoning. The toxicity of antimony is by far lower than that of arsenic; this might be caused by the significant differences of uptake, metabolism and excretion between arsenic and antimony. The uptake of antimony(III) or antimony(V) in the gastrointestinal tract is at most 20%. Antimony(V) is not quantitatively reduced to antimony(III) in the cell. Since methylation of antimony does not occur, the excretion of antimony(V) in urine is the main way of elimination.[74] Reported cases of intoxication by antimony equivalent to 90 mg antimony potassium tartrate dissolved from enamel has been reported to show only short term effects. An intoxication with 6 g of antimony potassium tartrate was reported to result in death after 3 days.[72]

Inhalation of antimony dust is harmful and in certain cases may be fatal; in small doses, antimony causes headaches, dizziness, and depression. Larger doses such as prolonged skin contact may cause dermatitis, or damage the kidneys and the liver, causing violent and frequent vomiting, leading to death in a few days.

Antimony is incompatible with strong oxidizing agents, strong acids, halogen acids, chlorine, or fluorine. It should be kept away from heat.[75]

Antimony leaches from polyethylene terephthalate (PET) bottles into liquids.[76] While levels observed for bottled water are below drinking water guidelines,[77] fruit juice concentrates (for which no guidelines are established) produced in the UK were found to contain up to 44.7 µg/L of antimony, well above the EU limits for tap water of 5 µg/L.[78][79] The guidelines are:

See also

Notes

  1. ^ In the UK, the variable vowel /ɵ/ is usually pronounced as a schwa [ə]; in the US, it is generally a full [oʊ].
  2. ^ In the UK, the variable vowel /ɵ/ is usually pronounced as a schwa [ə]; in the US, it is generally a full [oʊ].
  3. ^ Already in 1710 Wilhelm Gottlob Freiherr von Leibniz, after careful inquiry, concluded the work was spurious, there was no monk named Basilius Valentinus, and the book's author was its ostensible editor, Johann Thölde (c. 1565-c. 1624). Professional historians now agree the Currus Triumphalis ... was written after the middle of the 16th century and Thölde was likely its author.[19]
  4. ^ The use of a symbol resembling an upside down "female" symbol for antimony could also hint at a satirical pun in this origin

References

  1. ^ Magnetic susceptibility of the elements and inorganic compounds, in Handbook of Chemistry and Physics 81st edition, CRC press.
  2. ^ a b c d e f g h i Wiberg, Egon; Wiberg, Nils and Holleman, Arnold Frederick (2001). Inorganic chemistry. Academic Press. ISBN 0-12-352651-5. 
  3. ^ "Metals Used in Coins and Medals". ukcoinpics.co.uk. http://www.ukcoinpics.co.uk/metal.html. 
  4. ^ a b c Kirk-Othmer Encyclopedia of Chemical Technology, 5th ed. 2004. Entry for antimony.
  5. ^ a b c Wang, Chung Wu (1919). "The Chemistry of Antimony". Antimony: Its History, Chemistry, Mineralogy, Geology, Metallurgy, Uses, Preparation, Analysis, Production and Valuation with Complete Bibliographies. London, United Kingdom: Charles Geiffin and Co. Ltd. pp. 6–33. http://library.sciencemadness.org/library/books/antimony.pdf. 
  6. ^ Norman, Nicholas C (1998). page2 50–51 Chemistry of arsenic, antimony, and bismuth. ISBN 978-0-7514-0389-3. http://books.google.de/books?id=vVhpurkfeN4C&pg=PA50%7C page2 50–51. 
  7. ^ Georges, Audi; Bersillon, O.; Blachot, J.; Wapstra, A.H. (2003). "The NUBASE Evaluation of Nuclear and Decay Properties". Nuclear Physics A (Atomic Mass Data Center) 729: 3–128. Bibcode 2003NuPhA.729....3A. doi:10.1016/j.nuclphysa.2003.11.001. 
  8. ^ a b c d Carlin, Jr., James F.. "Mineral Commodity Summaries: Antimony". United States Geological Survey. http://minerals.usgs.gov/minerals/pubs/commodity/antimony/mcs-2011-antim.pdf. Retrieved 2012-01-23. 
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  20. ^ s.v. "Basilius Valentinus." Harold Jantz was perhaps the only modern scholar to deny Thölde's authorship, but he too agrees the work dates from after 1550: see his catalogue of German Baroque literature.
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  26. ^ Pliny, Natural history, 33.33; W.H.S. Jones, the Loeb Classical Library translator, supplies a note suggesting the identifications.
  27. ^ Albright, W. F. (1918). "Notes on Egypto-Semitic Etymology. II". The American Journal of Semitic Languages and Literatures 34 (4): 215–255. doi:10.1086/369866. JSTOR 528157. 
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  29. ^ LSJ, s.v., vocalisation, spelling, and declension vary; Endlich, p. 28; Celsus, 6.6.6 ff; Pliny Natural History 33.33; Lewis and Short: Latin Dictionary. OED, s. "antimony".
  30. ^ In his long article on chemical reactions and nomenclature – Jöns Jacob Berzelius, "Essay on the cause of chemical proportions, and on some circumstances relating to them: together with a short and easy method of expressing them," Annals of Philosophy, vol. 2, pages 443–454 (1813) and vol. 3, pages 51–62, 93–106, 244–255, 353–364 (1814) – on page 52, Berzelius lists the symbol for antimony as "St"; however, starting on page 248, Berzelius subsequently uses the symbol "Sb" for antimony.
  31. ^ Fernando, Diana (1998). Alchemy : an illustrated A to Z. Blandford.  Fernando even derives it from the story of how "Basil Valentine" and his fellow monastic alchemists poisoned themselves by working with antimony; antimonium is found two centuries before his time. "Popular etymology" from OED; as for antimonos, the pure negative would be more naturally expressed by a- "not".
  32. ^ Lippman, pp. 643–5
  33. ^ Lippman, p. 642, writing in 1919, says "zuerst".
  34. ^ Meyerhof as quoted in Sarton, asserts that ithmid or athmoud became corrupted in the medieval "traductions barbaro-latines".; the OED asserts some Arabic form is the origin, and if ithmid is the root, posits athimodium, atimodium, atimonium, as intermediate forms.
  35. ^ Endlich, p. 28; one of the advantages of as-stimmi would be that it has a whole syllable in common with antimonium.
  36. ^ Endlich, F. M. (1888). "On Some Interesting Derivations of Mineral Names". The American Naturalist 22 (253): 21–32. doi:10.1086/274630. JSTOR 2451020. 
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  44. ^ a b Norman, Nicholas C (1998). Chemistry of arsenic, antimony, and bismuth. p. 45. ISBN 978-0-7514-0389-3. http://books.google.de/books?id=vVhpurkfeN4C&pg=PA45. 
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Bibliography

External links


Translations:

Antimony

Top

Dansk (Danish)
n. - antimon

Nederlands (Dutch)
antimonium

Français (French)
n. - antimoine

Deutsch (German)
n. - (chem. min.) Antimon

Ελληνική (Greek)
n. - (χημ.) αντιμόνιο

Italiano (Italian)
antimonio

Português (Portuguese)
n. - antimônio (m) (Quím.)

Русский (Russian)
сурьма

Español (Spanish)
n. - antimonio

Svenska (Swedish)
n. - antimon (kem.)

中文(简体)(Chinese (Simplified))

中文(繁體)(Chinese (Traditional))
n. - 銻

한국어 (Korean)
n. - (화학) 안티모니

日本語 (Japanese)
n. - アンチモン

العربيه (Arabic)
‏(الاسم) انتيمون : معدن ذو لون فضي يستعمل في تقويه المعادن الأخرى‏

עברית (Hebrew)
n. - ‮אנטימון (יסוד מתכתי, BS, מס' אטומי 15)‬


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Sb (symbol – in chemistry)
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