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Antimony

Chemical element with atomic number 51 (Sb)

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Antimony crystal, 2 grams, 1 cm.
Unknown author Unknown author · CC BY 3.0

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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 most common 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

Antimony is a member of group 15 of the periodic table. As one of the elements called pnictogens, it 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. As a metalloid, it has a Mohs scale hardness of 3.

Antimony is a silvery, lustrous gray solid that is stable in air at room temperature. If heated, it reacts with oxygen to produce antimony trioxide,Sb2O3. Antimony is attacked by oxidizing acids.

The stable allotrope of antimony crystallises in a trigonal cell, isomorphic with bismuth and the gray allotrope of arsenic.

A yellow allotrope of antimony, assumed to be analogous to yellow arsenic, forms by oxidation of stibine (SbH3) with air or oxygen at −90 °C. At ambient temperatures and in ambient light, it transforms into the more stable black allotrope. A rare explosive form of antimony can be formed from the electrolysis of antimony trichloride, but it always contains appreciable chlorine and is not really an antimony allotrope. 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.

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.

Isotopes

Antimony has two stable isotopes: 121Sb with a natural abundance of 57.21% and 123Sb with a natural abundance of 42.79%. There are 37 artificial radioactive isotopes known with mass numbers 104 to 142, of which the longest-lived is the fission product 125Sb with a half-life of 2.758 years. Numerous meta states are known, of which the most stable is 120m1Sb with a half-life of 5.76 days. Isotopes that are lighter than the stable 123Sb tend to undergo β+ decay, and those that are heavier experience β− decay, with some exceptions.

Occurrence

The abundance of antimony in the Earth's crust is estimated at 0.2 parts per million, comparable to thallium at 0.5 ppm and silver at 0.07 ppm. It is the 63rd most abundant element in the crust. 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.

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