Antimony

Antimony is a chemical element with the symbol Sb (from Latin: stibium) and atomic number 51. A lustrous gray metalloid, it is found in nature mainly as the sulfide mineral stibnite (Sb2S3). Antimony compounds have been known since ancient times and were powdered for use as medicine and cosmetics, often known by the Arabic name kohl.[5] The earliest known description of the metal in the West was written in 1540 by Vannoccio Biringuccio.

Antimony, 51Sb
Antimony
Pronunciation
  • UK: /ˈæntɪməni/
    (AN-tim-ə-nee)
  • US: /ˈæntɪmoʊni/
    (AN-tim-oh-nee)
Appearancesilvery lustrous gray
Standard atomic weight Ar°(Sb)
  • 121.760±0.001
  • 121.76±0.01 (abridged)[1]
Antimony in the periodic table
Hydrogen Helium
Lithium Beryllium Boron Carbon Nitrogen Oxygen Fluorine Neon
Sodium Magnesium Aluminium Silicon Phosphorus Sulfur Chlorine Argon
Potassium Calcium Scandium Titanium Vanadium Chromium Manganese Iron Cobalt Nickel Copper Zinc Gallium Germanium Arsenic Selenium Bromine Krypton
Rubidium Strontium Yttrium Zirconium Niobium Molybdenum Technetium Ruthenium Rhodium Palladium Silver Cadmium Indium Tin Antimony Tellurium Iodine Xenon
Caesium Barium Lanthanum Cerium Praseodymium Neodymium Promethium Samarium Europium Gadolinium Terbium Dysprosium Holmium Erbium Thulium Ytterbium Lutetium Hafnium Tantalum Tungsten Rhenium Osmium Iridium Platinum Gold Mercury (element) Thallium Lead Bismuth Polonium Astatine Radon
Francium Radium Actinium Thorium Protactinium Uranium Neptunium Plutonium Americium Curium Berkelium Californium Einsteinium Fermium Mendelevium Nobelium Lawrencium Rutherfordium Dubnium Seaborgium Bohrium Hassium Meitnerium Darmstadtium Roentgenium Copernicium Nihonium Flerovium Moscovium Livermorium Tennessine Oganesson
 As
↑
Sb
↓
Bi
tin ← antimony → tellurium
Atomic number (Z)51
Groupgroup 15 (pnictogens)
Periodperiod 5
Block  p-block
Electron configuration[Kr] 4d10 5s2 5p3
Electrons per shell2, 8, 18, 18, 5
Physical properties
Phase at STPsolid
Melting point903.78 K ​(630.63 °C, ​1167.13 °F)
Boiling point1908 K ​(1635 °C, ​2975 °F)
Density (near r.t.)6.697 g/cm3
when liquid (at m.p.)6.53 g/cm3
Heat of fusion19.79 kJ/mol
Heat of vaporization193.43 kJ/mol
Molar heat capacity25.23 J/(mol·K)
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−3, −2, −1, 0,[2] +1, +2, +3, +4, +5 (an amphoteric oxide)
ElectronegativityPauling scale: 2.05
Ionization energies
  • 1st: 834 kJ/mol
  • 2nd: 1594.9 kJ/mol
  • 3rd: 2440 kJ/mol
  • (more)
Atomic radiusempirical: 140 pm
Covalent radius139±5 pm
Van der Waals radius206 pm
Spectral lines of antimony
Other properties
Natural occurrenceprimordial
Crystal structure ​rhombohedral
Speed of sound thin rod3420 m/s (at 20 °C)
Thermal expansion11 µm/(m⋅K) (at 25 °C)
Thermal conductivity24.4 W/(m⋅K)
Electrical resistivity417 nΩ⋅m (at 20 °C)
Magnetic orderingdiamagnetic[3]
Molar magnetic susceptibility−99.0×10−6 cm3/mol[4]
Young's modulus55 GPa
Shear modulus20 GPa
Bulk modulus42 GPa
Mohs hardness3.0
Brinell hardness294–384 MPa
CAS Number7440-36-0
History
DiscoveryArabic alchemists (before AD 815)
Symbol"Sb": from Latin stibium 'stibnite'
Main isotopes of antimony
Iso­tope Abun­dance Half-life (t1/2) Decay mode Pro­duct
121Sb 57.21% stable
123Sb 42.79% stable
125Sb syn 2.7582 y β− 125Te

China is the largest producer of antimony and its compounds, with most production coming from the Xikuangshan Mine in Hunan. The industrial methods for refining antimony from stibnite are roasting followed by reduction with carbon, or direct reduction of stibnite with iron.

The largest applications for metallic antimony are in alloys with lead and tin, which have improved properties for solders, bullets, and plain bearings. It improves the rigidity of lead-alloy plates in lead–acid batteries. Antimony trioxide is a prominent additive for halogen-containing flame retardants. Antimony is used as a dopant in semiconductor devices.

Characteristics

Properties
A vial containing the black allotrope of antimony
Native antimony with oxidation products
Crystal structure common to Sb, AsSb and gray As

Antimony is a member of group 15 of the periodic table, one of the elements called pnictogens, and has an electronegativity of 2.05. In accordance with 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 produce antimony trioxide, Sb2O3.[6]: 758 

Antimony is a silvery, lustrous gray metalloid with a Mohs scale hardness of 3, which is too soft to mark hard objects. Coins of antimony were issued in China's Guizhou province in 1931; durability was poor, and minting was soon discontinued.[7] 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). Elemental antimony is a brittle, silver-white, shiny metalloid. When slowly cooled, molten antimony crystallizes into a trigonal cell, isomorphic with the gray allotrope of arsenic. A rare explosive form of antimony can be formed from the electrolysis of antimony trichloride. When scratched with a sharp implement, an exothermic reaction occurs and white fumes are given off as metallic antimony forms; when rubbed with a pestle in a mortar, a strong detonation occurs. Black antimony is formed upon rapid cooling of antimony vapor. 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 been generated only 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.[8][9][10]

Elemental antimony adopts a layered structure (space group R3m No. 166) whose layers consist of fused, ruffled, six-membered rings. The nearest and next-nearest neighbors form an irregular octahedral complex, with the three atoms in each double layer 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.[6]: 758 

Isotopes

Antimony has 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 characterized. The most stable of these is 120m1Sb with a half-life of 5.76 days. 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.[11]

Occurrence
Stibnite, China CM29287 Carnegie Museum of Natural History specimen on display in Hillman Hall of Minerals and Gems

The abundance of antimony in the Earth's crust is estimated to be 0.2 to 0.5 parts per million, comparable to thallium at 0.5 parts per million and silver at 0.07 ppm.[12] Even though this element is not abundant, it is found in more than 100 mineral species. Antimony is sometimes found natively (e.g. on Antimony Peak), but more frequently it is found in the sulfide stibnite (Sb2S3) which is the predominant ore mineral.[12]

Compounds

Antimony compounds are often classified according to their oxidation state: Sb(III) and Sb(V).[13] The +5 oxidation state is more stable.

Oxides and hydroxides

Antimony trioxide is formed when antimony is burnt in air.[14] In the gas phase, the molecule of the compound is Sb
4O
6, but it polymerizes upon condensing.[6] Antimony pentoxide (Sb
4O
10) can be formed only by oxidation with concentrated nitric acid.[15] Antimony also forms a mixed-valence oxide, antimony tetroxide (Sb
2O
4), which features both Sb(III) and Sb(V).[15] Unlike oxides of phosphorus and arsenic, these 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 ([Na
3SbO
3]
4) forms upon fusing sodium oxide and Sb
4O
6.[6]: 763  Transition metal antimonites are also known.[16]: 122  Antimonic acid exists only as the hydrate HSb(OH)
6, forming salts as the antimonate anion Sb(OH)−
6. When a solution containing this anion is dehydrated, the precipitate contains mixed oxides.[16]: 143 

Many antimony ores are sulfides, including stibnite (Sb
2S
3), pyrargyrite (Ag
3SbS
3), zinkenite, jamesonite, and boulangerite.[6]: 757  Antimony pentasulfide is non-stoichiometric and features antimony in the +3 oxidation state and S–S bonds.[17] Several thioantimonides are known, such as [Sb
6S
10]2−
 and [Sb
8S
13]2−
.[18]

Halides

Antimony forms two series of halides: SbX
3 and SbX
5. The trihalides SbF
3, SbCl
3, SbBr
3, and SbI
3 are all molecular compounds having trigonal pyramidal molecular geometry.

The trifluoride SbF
3 is prepared by the reaction of Sb
2O
3 with HF:[6]: 761–762 

Sb
2O
3 + 6 HF → 2 SbF
3 + 3 H
2O

It is Lewis acidic and readily accepts fluoride ions to form the complex anions SbF−
4 and SbF2−
5. Molten SbF
3 is a weak electrical conductor. The trichloride SbCl
3 is prepared by dissolving Sb
2S
3 in hydrochloric acid:

Sb
2S
3 + 6 HCl → 2 SbCl
3 + 3 H
2S
Structure of gaseous SbF5

The pentahalides SbF
5 and SbCl
5 have trigonal bipyramidal molecular geometry in the gas phase, but in the liquid phase, SbF
5 is polymeric, whereas SbCl
5 is monomeric.[6]: 761  SbF
5 is a powerful Lewis acid used to make the superacid fluoroantimonic acid ("H2SbF7").

Oxyhalides are more common for antimony than for arsenic and phosphorus. Antimony trioxide dissolves in concentrated acid to form oxoantimonyl compounds such as SbOCl and (SbO)
2SO
4.[6]: 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 (Ag
3Sb).[6]: 760  The alkali metal and zinc antimonides, such as Na3Sb and Zn3Sb2, are more reactive. Treating these antimonides with acid produces the highly unstable gas stibine, SbH
3:[19]

Sb3−
 + 3 H+
 → SbH
3

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.[13]

Organoantimony compounds are typically prepared by alkylation of antimony halides with Grignard reagents.[20] 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
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.[21]

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.[8] Austen, at a lecture by Herbert Gladstone in 1892, 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."[22]

The British archaeologist Roger Moorey was unconvinced the artifact 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."[22] This weakens the evidence for a lost art "of rendering antimony malleable."[22]

The Roman scholar Pliny the Elder described several ways of preparing antimony sulfide for medical purposes in his treatise Natural History, around 77 AD.[23] Pliny the Elder also made a distinction 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.[24]

The Greek naturalist Pedanius Dioscorides mentioned that antimony sulfide could be roasted by heating by a current of air. It is thought that this produced metallic antimony.[23]

The Italian metallurgist Vannoccio Biringuccio described a procedure to isolate antimony.

Antimony was frequently described in alchemical manuscripts, including the Summa Perfectionis of Pseudo-Geber, written around the 14th century.[25] A description of a procedure for isolating antimony is later given in the 1540 book De la pirotechnia by Vannoccio Biringuccio,[26] predating 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 be written by a Benedictine monk, writing under the name Basilius Valentinus in the 15th century; if it were authentic, which it is not, it would predate Biringuccio.[note 1][9][28][29]

The metal antimony was known to German chemist Andreas Libavius in 1615 who obtained it by adding iron to a molten mixture of antimony sulfide, salt and potassium tartrate. This procedure produced antimony with a crystalline or starred surface.[23]

With the advent of challenges to phlogiston theory, it was recognized that antimony is an element forming sulfides, oxides, and other compounds, as do other metals.[23]

The first discovery of naturally occurring 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.[30][31]

Etymology

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.[32] However, the low toxicity of antimony (see below) makes this unlikely.

Another popular etymology is the hypothetical Greek word ἀντίμόνος antimonos, "against aloneness", explained as "not found as metal", or "not found unalloyed".[8][33] 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.[34]

The early uses of antimonium include the translations, in 1050–1100, by Constantine the African of Arabic medical treatises.[35] Several authorities believe antimonium is a scribal corruption of some Arabic form; Meyerhof derives it from ithmid;[36] other possibilities include athimar, the Arabic name of the metalloid, and a hypothetical as-stimmi, derived from or parallel to the Greek.[37][38]

The standard chemical symbol for antimony (Sb) is credited to Jöns Jakob Berzelius, who derived the abbreviation from stibium.[39]

The ancient words for antimony mostly have, as their chief meaning, kohl, the sulfide of antimony. The Egyptians called antimony mśdmt;[40][41] in hieroglyphs, the vowels are uncertain, but the Coptic form of the word is ⲥⲧⲏⲙ (stēm).

Egyptian stm:[32]

The Greek word, στίμμι (stimmi) is used by Attic tragic poets of the 5th century BC, and is possibly a loan word from Arabic or from Egyptian stm. 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, 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.[42]

Production

Process

The extraction of antimony from ores depends on the quality 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 separates from the gangue minerals. Antimony can be isolated from the crude antimony sulfide by reduction with scrap iron:[43]

Sb
2S
3 + 3 Fe → 2 Sb + 3 FeS

The sulfide is converted to an oxide; the product is then roasted, sometimes for the purpose of vaporizing the volatile antimony(III) oxide, which is recovered.[44] This material is often used directly for the main applications, impurities being arsenic and sulfide.[45][46] Antimony is isolated from the oxide by a carbothermal reduction:[43][45]

2 Sb
2O
3 + 3 C → 4 Sb + 3 CO
2

The lower-grade ores are reduced in blast furnaces while the higher-grade ores are reduced in reverberatory furnaces.[43]

World antimony output in 2010[12]
World production trend of antimony

Top producers and production volumes

The British Geological Survey (BGS) reported that in 2005 China was the top producer of antimony with approximately 84% of the 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.[47]

In 2016, according to the US Geological Survey, China accounted for 76.9% of total antimony production, followed in second place by Russia with 6.9% and Tajikistan with 6.2%.[48]

Antimony production in 2016[12]
CountryTonnes % of total
 China 100,000 76.9
 Russia 9,000 6.9
 Tajikistan 8,000 6.2
 Bolivia 4,000 3.1
 Australia 3,500 2.7
Top 5 124,500 95.8
Total world 130,000 100.0

Chinese production of antimony is expected to decline in the future as mines and smelters are closed down by the government as part of pollution control. Especially due to an environmental protection law having gone into effect in January 2015[49] and revised "Emission Standards of Pollutants for Stanum, Antimony, and Mercury" having gone into effect, hurdles for economic production are higher. According to the National Bureau of Statistics in China, by September 2015 50% of antimony production capacity in the Hunan province (the province with biggest antimony reserves in China) had not been used.[50]

Reported production of antimony in China has fallen and is unlikely to increase in the coming years, according to the Roskill report. No significant antimony deposits in China have been developed for about ten years, and the remaining economic reserves are being rapidly depleted.[51]

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

Largest antimony producers in 2010.[52]
CountryCompanyCapacity
(tonnes per year)
 China Hsikwangshan Twinkling Star 55,000
 China China Tin Group 20,000
 China Hunan Chenzhou Mining 20,000
 China Shenyang Huachang Antimony 15,000
 Russia GeoProMining 6,500
 Canada Beaver Brook 6,000
 South Africa Consolidated Murchison 6,000
 Myanmar various 6,000
 Tajikistan Unzob 5,500
 Bolivia various 5,460
 Australia Mandalay Resources 2,750
 Turkey Cengiz & Özdemir Antimuan Madenleri 2,400
 Kazakhstan Kazzinc 1,000
 Thailand unknown 600
 Kyrgyzstan Kadamdzhai 500
 Laos SRS 500
 Mexico US Antimony 70

Reserves
World antimony reserves in 2015[52]
CountryReserves
(tonnes of antimony content)		 % of total
 People's Republic of China 950,000 47.81
 Russia 350,000 17.61
 Bolivia 310,000 15.60
 Australia 140,000 7.05
 United States 60,000 3.02
 Tajikistan 50,000 2.52
 South Africa 27,000 1.36
Other countries 100,000 5.03
Total world 1,987,000 100.0

Supply risk

For antimony-importing regions such as Europe and the U.S., antimony is considered to be a critical mineral for industrial manufacturing that is at risk of supply chain disruption. With global production coming mainly from China (74%), Tajikistan (8%), and Russia (4%), these sources are critical to supply.[53][54]

  • European Union: Antimony is considered a critical raw material for defense, automotive, construction and textiles. The E.U. sources are 100% imported, coming mainly from Turkey (62%), Bolivia (20%) and Guatemala (7%).[53]
  • United Kingdom: The British Geological Survey's 2015 risk list ranks antimony second highest (after rare earth elements) on the relative supply risk index.[55][56]
  • United States: Antimony is a mineral commodity considered critical to the economic and national security.[57][54] In 2021, no antimony was mined in the U.S.[58]

Applications

About 60% of antimony is consumed in flame retardants, and 20% is used in alloys for batteries, plain bearings, and solders.[43]

Flame retardants

Antimony is mainly used as the trioxide for flame-proofing compounds, always in combination with halogenated flame retardants except in halogen-containing polymers. The flame retarding effect of antimony trioxide is produced by the formation of halogenated antimony compounds,[59] which react with hydrogen atoms, and probably also with oxygen atoms and OH radicals, thus inhibiting fire.[60] Markets for these flame-retardants include children's clothing, toys, aircraft, and automobile seat covers. They are also added to polyester resins in fiberglass composites for such items as light aircraft engine covers. The resin will burn in the presence of an externally generated flame, but will extinguish when the external flame is removed.[44][61]

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 plate strength and charging characteristics.[44][62] For sailboats, lead keels are used to provide righting moment, ranging from 600 lbs to over 200 tons for the largest sailing superyachts; to improve hardness and tensile strength of the lead keel, antimony is mixed with lead between 2% and 5% by volume. Antimony is used in antifriction alloys (such as Babbitt metal),[63] in bullets and lead shot, electrical cable sheathing, type metal (for example, for linotype printing machines[64]), solder (some "lead-free" solders contain 5% Sb),[65] in pewter,[66] and in hardening alloys with low tin content in the manufacturing of organ pipes.

Other applications

Three other applications consume nearly all the rest of the world's supply.[43] One application is as a stabilizer and catalyst for the production of polyethylene terephthalate.[43] Another is as a fining agent to remove microscopic bubbles in glass, mostly for TV screens[67] – antimony ions interact with oxygen, suppressing the tendency of the latter to form bubbles.[68] The third application is pigments.[43]

In the 1990s antimony was increasingly being used in semiconductors as a dopant in n-type silicon wafers[69] for diodes, infrared detectors, and Hall-effect devices. In the 1950s, the emitters and collectors of n-p-n alloy junction transistors were doped with tiny beads of a lead-antimony alloy.[70] Indium antimonide is used as a material for mid-infrared detectors.[71][72][73]

Biology and medicine have few uses for antimony. Treatments containing antimony, known as antimonials, are used as emetics.[74] 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.[75] Antimony and its compounds are used in several veterinary preparations, such as anthiomaline and lithium antimony thiomalate, as a skin conditioner in ruminants.[76] Antimony has a nourishing or conditioning effect on keratinized tissues in animals.

Antimony-based drugs, such as meglumine antimoniate, are also considered the drugs of choice for treatment of leishmaniasis in domestic animals. Besides having low therapeutic indices, the drugs have minimal penetration of the bone marrow, where some of the Leishmania amastigotes reside, and curing the disease – especially the visceral form – is very difficult.[77] Elemental antimony as an antimony pill was once used as a medicine. It could be reused by others after ingestion and elimination.[78]

Antimony(III) sulfide is used in the heads of some safety matches.[79][80] Antimony sulfides help to stabilize the friction coefficient in automotive brake pad materials.[81] Antimony is used in bullets, bullet tracers,[82] paint, glass art, and as an opacifier in enamel. Antimony-124 is used together with beryllium in neutron sources; the gamma rays emitted by antimony-124 initiate the photodisintegration of beryllium.[83][84] The emitted neutrons have an average energy of 24 keV.[85] Natural antimony is used in startup neutron sources.

Historically, the powder derived from crushed antimony (kohl) has been applied to the eyes with a metal rod and with one's spittle, thought by the ancients to aid in curing eye infections.[86] The practice is still seen in Yemen and in other Muslim countries.[87]

Precautions

The effects of antimony and its compounds on human and environmental health differ widely. Elemental antimony metal does not affect human and environmental health. Inhalation of antimony trioxide (and similar poorly soluble Sb(III) dust particles such as antimony dust) is considered harmful and suspected of causing cancer. However, these effects are only observed with female rats and after long-term exposure to high dust concentrations. The effects are hypothesized to be attributed to inhalation of poorly soluble Sb particles leading to impaired lung clearance, lung overload, inflammation and ultimately tumour formation, not to exposure to antimony ions (OECD, 2008). Antimony chlorides are corrosive to skin. The effects of antimony are not comparable to those of arsenic; this might be caused by the significant differences of uptake, metabolism, and excretion between arsenic and antimony.

For oral absorption, ICRP (1994) has recommended values of 10% for tartar emetic and 1% for all other antimony compounds. Dermal absorption for metals is estimated to be at most 1% (HERAG, 2007). Inhalation absorption of antimony trioxide and other poorly soluble Sb(III) substances (such as antimony dust) is estimated at 6.8% (OECD, 2008), whereas a value <1% is derived for Sb(V) substances. Antimony(V) is not quantitatively reduced to antimony(III) in the cell, and both species exist simultaneously.

Antimony is mainly excreted from the human body via urine. Antimony and its compounds do not cause acute human health effects, with the exception of antimony potassium tartrate ("tartar emetic"), a prodrug that is intentionally used to treat leishmaniasis patients.

Prolonged skin contact with antimony dust may cause dermatitis. However, it was agreed at the European Union level that the skin rashes observed are not substance-specific, but most probably due to a physical blocking of sweat ducts (ECHA/PR/09/09, Helsinki, 6 July 2009). Antimony dust may also be explosive when dispersed in the air; when in a bulk solid it is not combustible.[88]

Antimony is incompatible with strong acids, halogenated acids, and oxidizers; when exposed to newly formed hydrogen it may form stibine (SbH3).[88]

The 8-hour time-weighted average (TWA) is set at 0.5 mg/m3 by the American Conference of Governmental Industrial Hygienists and by the Occupational Safety and Health Administration (OSHA) as a legal permissible exposure limit (PEL) in the workplace. The National Institute for Occupational Safety and Health (NIOSH) has set a recommended exposure limit (REL) of 0.5 mg/m3 as an 8-hour TWA.[88]

Antimony compounds are used as catalysts for polyethylene terephthalate (PET) production. Some studies report minor antimony leaching from PET bottles into liquids, but levels are below drinking water guidelines. Antimony concentrations in fruit juice concentrates were somewhat higher (up to 44.7 µg/L of antimony), but juices do not fall under the drinking water regulations. The drinking water guidelines are:

The tolerable daily intake (TDI) proposed by WHO is 6 µg antimony per kilogram of body weight.[91] The immediately dangerous to life or health (IDLH) value for antimony is 50 mg/m3.[88]

Toxicity

Certain compounds of antimony appear to be toxic, particularly antimony trioxide and antimony potassium tartrate.[92] Effects may be similar to arsenic poisoning.[93] Occupational exposure may cause respiratory irritation, pneumoconiosis, antimony spots on the skin, gastrointestinal symptoms, and cardiac arrhythmias. In addition, antimony trioxide is potentially carcinogenic to humans.[94]

Adverse health effects have been observed in humans and animals following inhalation, oral, or dermal exposure to antimony and antimony compounds.[92] Antimony toxicity typically occurs either due to occupational exposure, during therapy or from accidental ingestion. It is unclear if antimony can enter the body through the skin.[92] The presence of low levels of antimony in saliva may also be associated with dental decay.[95]

See also
  • Phase change memory

Notes
  1. 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.[27]

References
  1. "Standard Atomic Weights: Antimony". CIAAW. 1993.
  2. Anastas Sidiropoulos. "Studies of N-heterocyclic Carbene (NHC) Complexes of the Main Group Elements" (PDF). p. 39. doi:10.4225/03/5B0F4BDF98F60. S2CID 132399530.
  3. Lide, D. R., ed. (2005). "Magnetic susceptibility of the elements and inorganic compounds". CRC Handbook of Chemistry and Physics (PDF) (86th ed.). Boca Raton (FL): CRC Press. ISBN 0-8493-0486-5.
  4. Weast, Robert (1984). CRC, Handbook of Chemistry and Physics. Boca Raton, Florida: Chemical Rubber Company Publishing. pp. E110. ISBN 0-8493-0464-4.
  5. David Kimhi's Commentary on Jeremiah 4:30 and I Chronicles 29:2; Hebrew: פוך/כְּחֻל, Aramaic: כּוּחְלִי/צדידא; Arabic: كحل, and which can also refer to antimony trisulfide. See also Z. Dori, Antimony and Henna (Heb. הפוך והכופר), Jerusalem 1983 (Hebrew).
  6. Wiberg, Egon; Wiberg, Nils & Holleman, Arnold Frederick (2001). Inorganic chemistry. Academic Press. ISBN 978-0-12-352651-9.
  7. "Metals Used in Coins and Medals". ukcoinpics.co.uk. Archived from the original on 26 December 2010. Retrieved 16 October 2009.
  8. "Antimony" in Kirk-Othmer Encyclopedia of Chemical Technology, 5th ed. 2004. ISBN 978-0-471-48494-3
  9. Wang, Chung Wu (1919). "The Chemistry of Antimony" (PDF). 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. Archived (PDF) from the original on 9 October 2022.
  10. Norman, Nicholas C (1998). Chemistry of arsenic, antimony, and bismuth. pp. 50–51. ISBN 978-0-7514-0389-3.
  11. Audi, Georges; Bersillon, Olivier; Blachot, Jean; Wapstra, Aaldert Hendrik (2003), "The NUBASE evaluation of nuclear and decay properties", Nuclear Physics A, 729: 3–128, Bibcode:2003NuPhA.729....3A, doi:10.1016/j.nuclphysa.2003.11.001
  12. "Mineral Commodity Summaries: Antimony" (PDF). United States Geological Survey. Retrieved 1 January 2016.
  13. Greenwood, N. N.; & Earnshaw, A. (1997). Chemistry of the Elements (2nd Edn.), Oxford: Butterworth-Heinemann. ISBN 0-7506-3365-4.
  14. Reger, Daniel L.; Goode, Scott R. & Ball, David W. (2009). Chemistry: Principles and Practice (3rd ed.). Cengage Learning. p. 883. ISBN 978-0-534-42012-3.
  15. House, James E. (2008). Inorganic chemistry. Academic Press. p. 502. ISBN 978-0-12-356786-4.
  16. Godfrey, S. M.; McAuliffe, C. A.; Mackie, A. G. & Pritchard, R. G. (1998). Norman, Nicholas C. (ed.). Chemistry of arsenic, antimony, and bismuth. Springer. ISBN 978-0-7514-0389-3.
  17. Long, G.; Stevens, J. G.; Bowen, L. H.; Ruby, S. L. (1969). "The oxidation number of antimony in antimony pentasulfide". Inorganic and Nuclear Chemistry Letters. 5: 21. doi:10.1016/0020-1650(69)80231-X.
  18. Lees, R.; Powell, A.; Chippindale, A. (2007). "The synthesis and characterisation of four new antimony sulphides incorporating transition-metal complexes". Journal of Physics and Chemistry of Solids. 68 (5–6): 1215. Bibcode:2007JPCS...68.1215L. doi:10.1016/j.jpcs.2006.12.010.
  19. Kahlenberg, Louis (2008). Outlines of Chemistry – A Textbook for College Students. READ BOOKS. pp. 324–325. ISBN 978-1-4097-6995-8.
  20. Elschenbroich, C. "Organometallics" (2006) Wiley-VCH: Weinheim. ISBN 3-527-29390-6
  21. Shortland, A. J. (2006). "Application of Lead Isotope Analysis to a Wide Range of Late Bronze Age Egyptian Materials". Archaeometry. 48 (4): 657. doi:10.1111/j.1475-4754.2006.00279.x.
  22. Moorey, P. R. S. (1994). Ancient Mesopotamian Materials and Industries: the Archaeological Evidence. New York: Clarendon Press. p. 241. ISBN 978-1-57506-042-2.
  23. Mellor, Joseph William (1964). "Antimony". A comprehensive treatise on inorganic and theoretical chemistry. Vol. 9. p. 339.
  24. Pliny, Natural history, 33.33; W.H.S. Jones, the Loeb Classical Library translator, supplies a note suggesting the identifications.
  25. Montserrat Filella, ed. (2021). Antimony. De Gruyter. p. 4. ISBN 9783110668711.
  26. Vannoccio Biringuccio, De la Pirotechnia (Venice (Italy): Curtio Navo e fratelli, 1540), Book 2, chapter 3: Del antimonio & sua miniera, Capitolo terzo (On antimony and its ore, third chapter), pp. 27-28. [Note: Only every second page of this book is numbered, so the relevant passage is to be found on the 74th and 75th pages of the text.] (in Italian)
  27. Priesner, Claus; Figala, Karin, eds. (1998). Alchemie. Lexikon einer hermetischen Wissenschaft (in German). München: C.H. Beck.
  28. 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.
  29. Weeks, Mary Elvira (1932). "The discovery of the elements. II. Elements known to the alchemists". Journal of Chemical Education. 9 (1): 11. Bibcode:1932JChEd...9...11W. doi:10.1021/ed009p11.
  30. "Native antimony". Mindat.org.
  31. Klaproth, M. (1803). "XL. Extracts from the third volume of the analyses". Philosophical Magazine. Series 1. 17 (67): 230. doi:10.1080/14786440308676406.
  32. Harper, Douglas. "antimony". Online Etymology Dictionary.
  33. 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".
  34. Lippman, pp. 643–5
  35. Lippman, p. 642, writing in 1919, says "zuerst".
  36. 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.
  37. Endlich, p. 28; one of the advantages of as-stimmi would be that it has a whole syllable in common with antimonium.
  38. Endlich, F. M. (1888). "On Some Interesting Derivations of Mineral Names". The American Naturalist. 22 (253): 21–32. doi:10.1086/274630. JSTOR 2451020.
  39. 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.
  40. Albright, W. F. (1918). "Notes on Egypto-Semitic Etymology. II". The American Journal of Semitic Languages and Literatures. 34 (4): 215–255 [230]. doi:10.1086/369866. JSTOR 528157. S2CID 170203738.
  41. Sarton, George (1935). Translated by Max Meyerhof. "Review of Al-morchid fi'l-kohhl, ou Le guide d'oculistique". Isis (in French). 22 (2): 539–542 [541]. doi:10.1086/346926. JSTOR 225136. quotes Meyerhof, the translator of the book he is reviewing.
  42. 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".
  43. Butterman, C.; Carlin, J. F. Jr. (2003). "Mineral Commodity Profiles: Antimony" (PDF). United States Geological Survey. Archived (PDF) from the original on 9 October 2022. {{cite journal}}: Cite journal requires |journal= (help)
  44. Grund, Sabina C.; Hanusch, Kunibert; Breunig, Hans J.; Wolf, Hans Uwe (2006) "Antimony and Antimony Compounds" in Ullmann's Encyclopedia of Industrial Chemistry, Wiley-VCH, Weinheim. doi:10.1002/14356007.a03_055.pub2
  45. Norman, Nicholas C (1998). Chemistry of arsenic, antimony, and bismuth. p. 45. ISBN 978-0-7514-0389-3.
  46. Wilson, N. J.; Craw, D.; Hunter, K. (2004). "Antimony distribution and environmental mobility at an historic antimony smelter site, New Zealand". Environmental Pollution. 129 (2): 257–66. doi:10.1016/j.envpol.2003.10.014. PMID 14987811.
  47. Peng, J.; Hu, R.-Z.; Burnard, P. G. (2003). "Samarium–neodymium isotope systematics of hydrothermal calcites from the Xikuangshan antimony deposit (Hunan, China): the potential of calcite as a geochronometer". Chemical Geology. 200 (1–2): 129. Bibcode:2003ChGeo.200..129P. doi:10.1016/S0009-2541(03)00187-6.
  48. "Antimony Statistics and Information" (PDF). National Minerals Information Center. USGS. Archived (PDF) from the original on 9 October 2022.
  49. "Environmental Protection Law of the People's Republic of China" (PDF). 24 April 2014. Archived from the original (PDF) on 2 June 2014. Retrieved 14 October 2016.
  50. "U.S. Geological Survey, Mineral Commodity Summaries: Antimony" (PDF). 1 January 2016.
  51. "Study of the antimony market by Roskill Consulting Group" (PDF). Archived from the original (PDF) on 18 October 2012. Retrieved 9 April 2012.
  52. Antimony Uses, Production and Prices Primer Archived 25 October 2012 at the Wayback Machine . tri-starresources.com
  53. "Critical Raw Materials Resilience: Charting a Path towards greater Security and Sustainability". European Commission. 2020. Retrieved 2 February 2022.
  54. Nassar, Nedal T.; et al. (21 February 2020). "Evaluating the mineral commodity supply risk of the U.S. manufacturing sector". Sci. Adv. 6 (8): eaay8647. Bibcode:2020SciA....6.8647N. doi:10.1126/sciadv.aay8647. ISSN 2375-2548. PMC 7035000. PMID 32128413.
  55. "MineralsUK Risk List 2015". BGS.
  56. "British Geological Survey Risk list 2015" (PDF). Minerals UK. BGS. Archived (PDF) from the original on 9 October 2022. Retrieved 2 February 2022.
  57. "Interior Releases 2018's Final List of Critical Minerals". United States Geological Survey. Retrieved 1 February 2022.
  58. U.S. Geological Survey, Mineral Commodity Summaries, January 2022. "Antimony" (PDF). Archived (PDF) from the original on 9 October 2022. Retrieved 1 February 2022.{{cite web}}: CS1 maint: multiple names: authors list (link)
  59. Weil, Edward D.; Levchik, Sergei V. (4 June 2009). "Antimony trioxide and Related Compounds". Flame retardants for plastics and textiles: Practical applications. ISBN 978-3-446-41652-9.
  60. Hastie, John W. (1973). "Mass spectrometric studies of flame inhibition: Analysis of antimony trihalides in flames". Combustion and Flame. 21: 49. doi:10.1016/0010-2180(73)90006-0.
  61. Weil, Edward D.; Levchik, Sergei V. (4 June 2009). Flame retardants for plastics and textiles: Practical applications. pp. 15–16. ISBN 978-3-446-41652-9.
  62. Kiehne, Heinz Albert (2003). "Types of Alloys". Battery Technology Handbook. CRC Press. pp. 60–61. ISBN 978-0-8247-4249-2.
  63. Williams, Robert S. (2007). Principles of Metallography. Read books. pp. 46–47. ISBN 978-1-4067-4671-6.
  64. Holmyard, E. J. (2008). Inorganic Chemistry – A Textbook for Colleges and Schools. Read Books. pp. 399–400. ISBN 978-1-4437-2253-7.
  65. Ipser, H.; Flandorfer, H.; Luef, Ch.; Schmetterer, C.; Saeed, U. (2007). "Thermodynamics and phase diagrams of lead-free solder materials". Journal of Materials Science: Materials in Electronics. 18 (1–3): 3–17. doi:10.1007/s10854-006-9009-3. S2CID 85452380.
  66. Hull, Charles (1992). Pewter. Osprey Publishing. pp. 1–5. ISBN 978-0-7478-0152-8.
  67. De Jong, Bernard H. W. S.; Beerkens, Ruud G. C.; Van Nijnatten, Peter A. (2000). "Glass". Ullmann's Encyclopedia of Industrial Chemistry. doi:10.1002/14356007.a12_365. ISBN 978-3-527-30673-2.
  68. Yamashita, H.; Yamaguchi, S.; Nishimura, R.; Maekawa, T. (2001). "Voltammetric Studies of Antimony Ions in Soda-lime-silica Glass Melts up to 1873 K". Analytical Sciences. 17 (1): 45–50. doi:10.2116/analsci.17.45. PMID 11993676.
  69. O'Mara, William C.; Herring, Robert B.; Hunt, Lee Philip (1990). Handbook of semiconductor silicon technology. William Andrew. p. 473. ISBN 978-0-8155-1237-0.
  70. Maiti, C. K. (2008). Selected Works of Professor Herbert Kroemer. World Scientific, 2008. p. 101. ISBN 978-981-270-901-1.
  71. Committee on New Sensor Technologies: Materials And Applications, National Research Council (U.S.) (1995). Expanding the vision of sensor materials. p. 68. ISBN 978-0-309-05175-0.
  72. Kinch, Michael A (2007). Fundamentals of infrared detector materials. p. 35. ISBN 978-0-8194-6731-7.
  73. Willardson, Robert K & Beer, Albert C (1970). Infrared detectors. p. 15. ISBN 978-0-12-752105-3.
  74. Russell, Colin A. (2000). "Antimony's Curious History". Notes and Records of the Royal Society of London. 54 (1): 115–116. doi:10.1098/rsnr.2000.0101. JSTOR 532063. PMC 1064207.
  75. Harder, A. (2002). "Chemotherapeutic approaches to schistosomes: Current knowledge and outlook". Parasitology Research. 88 (5): 395–7. doi:10.1007/s00436-001-0588-x. PMID 12049454. S2CID 28243137.
  76. Kassirsky, I. A.; Plotnikov, N. N. (1 August 2003). Diseases of Warm Lands: A Clinical Manual. pp. 262–265. ISBN 978-1-4102-0789-0.
  77. Organisation Mondiale de la Santé (1995). Drugs used in parasitic diseases. pp. 19–21. ISBN 978-92-4-140104-3.
  78. McCallum, R. I. (1999). Antimony in medical history: an account of the medical uses of antimony and its compounds since early times to the present. Pentland Press. ISBN 978-1-85821-642-3.
  79. Stellman, Jeanne Mager (1998). Encyclopaedia of Occupational Health and Safety: Chemical, industries and occupations. p. 109. ISBN 978-92-2-109816-4.
  80. Jang, H & Kim, S. (2000). "The effects of antimony trisulfide Sb S and zirconium silicate in the automotive brake friction material on friction". Journal of Wear. 239 (2): 229. doi:10.1016/s0043-1648(00)00314-8.
  81. Randich, Erik; Duerfeldt, Wayne; McLendon, Wade; Tobin, William (2002). "A metallurgical review of the interpretation of bullet lead compositional analysis". Forensic Science International. 127 (3): 174–91. doi:10.1016/S0379-0738(02)00118-4. PMID 12175947. S2CID 22272775.
  82. Lalovic, M.; Werle, H. (1970). "The energy distribution of antimonyberyllium photoneutrons". Journal of Nuclear Energy. 24 (3): 123. Bibcode:1970JNuE...24..123L. doi:10.1016/0022-3107(70)90058-4.
  83. Ahmed, Syed Naeem (2007). Physics and engineering of radiation detection. p. 51. Bibcode:2007perd.book.....A. ISBN 978-0-12-045581-2.
  84. Schmitt, H (1960). "Determination of the energy of antimony-beryllium photoneutrons". Nuclear Physics. 20: 220. Bibcode:1960NucPh..20..220S. doi:10.1016/0029-5582(60)90171-1.
  85. Rabbeinu Hananel (1995), "Rabbeinu Hananel's Commentary on Tractate Shabbat", in Metzger, David (ed.), Perushe Rabenu Ḥananʼel Bar Ḥushiʼel la-Talmud (in Hebrew), Jerusalem: Mekhon 'Lev Sameaḥ', p. 215 (Shabbat 109a), OCLC 319767989
  86. "Sunan an-Nasa'i 5113 - The Book of Adornment - كتاب الزينة من السنن - Sunnah.com - Sayings and Teachings of Prophet Muhammad (صلى الله عليه و سلم)". sunnah.com. Retrieved 18 February 2021.
  87. NIOSH Pocket Guide to Chemical Hazards. "#0036". National Institute for Occupational Safety and Health (NIOSH).
  88. Wakayama, Hiroshi (2003) "Revision of Drinking Water Standards in Japan", Ministry of Health, Labor and Welfare (Japan); Table 2, p. 84
  89. Shotyk, W.; Krachler, M.; Chen, B. (2006). "Contamination of Canadian and European bottled waters with antimony from PET containers". Journal of Environmental Monitoring. 8 (2): 288–92. doi:10.1039/b517844b. PMID 16470261. S2CID 9416637.
  90. Guidelines for Drinking-water Quality (PDF) (4th ed.). World Health Organization. 2011. p. 314. ISBN 978-92-4-154815-1. Archived (PDF) from the original on 9 October 2022.
  91. "Toxicological Profile for Antimony and Compounds" (PDF). U.S. Department of Health and Human Services. Archived (PDF) from the original on 9 October 2022. Retrieved 19 May 2022.
  92. "Antimony poisoning". Encyclopedia Britannica.
  93. Sundar, S; Chakravarty, J (2010). "Antimony Toxicity". International Journal of Environmental Research and Public Health. 7 (12): 4267–4277. doi:10.3390/ijerph7124267. PMC 3037053. PMID 21318007.
  94. Davis, E.; Bakulski, K. M.; Goodrich, J. M. (2020). "Low levels of salivary metals, oral microbiome composition and dental decay". Scientific Reports. 10 (1): 14640. Bibcode:2020NatSR..1014640D. doi:10.1038/s41598-020-71495-9. PMC 7474081. PMID 32887894.

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