83 Bi

Post-transition metal

Overview

Bismuth is a chemical element; it has symbol Bi and atomic number 83. It is a post-transition metal and one of the pnictogens, with chemical properties resembling its lighter group 15 siblings arsenic and antimony. Elemental bismuth occurs naturally, and its sulfide and oxide forms are important commercial ores. The free element is 86% as dense as lead. It is a brittle metal with a silvery-white color when freshly produced. Surface oxidation generally gives samples of the metal a somewhat rosy cast. Further oxidation under heat can give bismuth a vividly iridescent appearance due to thin-film interference. Bismuth is the most diamagnetic element and of all the metals, it is among the most electrically resistive and least thermally conductive known.
Bismuth was formerly understood to be the element with the highest atomic mass whose nuclei do not spontaneously decay, but in 2003, it was found to be very slightly radioactive. The metal's only primordial isotope, bismuth-209, undergoes alpha decay with a half-life roughly a billion times longer than the estimated age of the universe.
Bismuth metal has been known since ancient times. Before modern analytical methods, bismuth's metallurgical similarities to lead and tin often led it to be confused with those metals. The etymology of "bismuth" is uncertain. The name may come from mid-16th-century neo-Latin translations of the German words weiße Masse or Wismuth, meaning "white mass", which were rendered as bisemutum or bisemutium. …

History

Bismuth was one of the first 11 metals to have been discovered. The name "bismuth" dates to around 1665 and is of uncertain etymology. The name possibly comes from German Bismuth, Wismut, Wissmuth (early 16th century), perhaps related to Old High German hwiz ("white"). The Neo-Latin bisemutium (coined by Georgius Agricola, who Latinized many German mining and technical words) is from the German Wismuth, itself perhaps from weiße Masse, meaning "white mass".
The element was confused in early times with tin and lead because of its resemblance to those elements. Because bismuth has been known since ancient times, no one person is credited with its discovery. Agricola (1546) states that bismuth is a distinct metal in a family of metals including tin and lead. This was based on observation of the metals and their physical properties. Miners in the age of alchemy also gave bismuth the name tectum argenti, or "silver being made" in the sense of silver still in the process of being formed within the Earth. Bismuth was also known to the Incas and used (along with the usual copper and tin) in a special bronze alloy for knives.

Beginning with Johann Heinrich Pott in 1738, Carl Wilhelm Scheele, and Torbern Olof Bergman, the distinctness of lead and bismuth became clear, and Claude François Geoffroy demonstrated in 1753 that this metal is distinct from lead and tin.

Properties

Bismuth is a brittle metal with a dark, silver-pink hue, often with an iridescent oxide tarnish showing many colors from yellow to blue. The spiral, stair-stepped structure of bismuth crystals is the result of a higher growth rate around the outside edges than on the inside edges. The variations in the thickness of the oxide layer that forms on the surface of the crystal cause different wavelengths of light to interfere upon reflection, thus displaying a rainbow of colors. When burned in oxygen, bismuth burns with a blue flame and its oxide forms yellow fumes. Its toxicity is much lower than that of its neighbors in the periodic table, such as lead and antimony.
No other metal is verified to be more naturally diamagnetic than bismuth. Of any metal, it has one of the lowest values of thermal conductivity (after manganese, neptunium, and plutonium) and the highest Hall coefficient. It has the fourth highest electrical resistivity of all the pure metals, only surpassed by gadolinium, manganese and plutonium. When deposited in sufficiently thin layers on a substrate, bismuth is a semiconductor, despite being a post-transition metal. Elemental bismuth is denser in the liquid phase than the solid, a characteristic it shares with germanium, silicon, gallium, plutonium, and water. …

Sources & occurrence

The reported abundance of bismuth in the Earth's crust varies significantly by source from 180 ppb (similar to that of silver) to 8 ppb (twice as common as gold). The most important ores of bismuth are bismuthinite and bismite. Native bismuth is known from Australia, Bolivia, and China.

According to the United States Geological Survey (USGS), 10,200 tonnes of bismuth were produced worldwide by mining and 17,100 tonnes by refining in 2016. Since then, USGS does not provide mining data for bismuth, considering them unreliable. Globally, bismuth is mostly produced by refining, as a byproduct of extraction of other metals such as lead, copper, tin, molybdenum, and tungsten, though the refining-to-mining ratio depends on the country.
Bismuth travels in crude lead bullion (which can contain up to 10% bismuth) through several stages of refining, until it is removed by the Kroll-Betterton process, which separates the impurities as slag, or the electrolytic Betts process. Bismuth behaves similarly with another of its major metals, copper. The raw bismuth metal from both processes contains still considerable amounts of other metals, foremost lead. By reacting the molten mixture with chlorine gas, the metals are converted to their chlorides, while bismuth remains unchanged. Impurities can also be removed by various other methods, for example, with fluxes and treatments yielding high-purity bismuth metal (over 99% Bi). …

Uses

Bismuth has few commercial applications, and those that use it generally require small quantities relative to other raw materials. In the United States, for example, 733 tonnes of bismuth were consumed in 2016, of which 70% went into chemicals (including pharmaceuticals, pigments, and cosmetics) and 11% into bismuth alloys.

Bismuth is an ingredient in some pharmaceuticals, although the use of some of these substances is declining.

Bismuth subsalicylate is used to treat diarrhea; it is the active ingredient in such "pink bismuth" preparations as Pepto-Bismol, as well as the 2004 reformulation of Kaopectate. It is also used to treat some other gastrointestinal diseases such as shigellosis and cadmium poisoning. The mechanism of action of this substance is still not well documented, although an oligodynamic effect (toxic effect of small doses of heavy metal ions on microbes) may be involved in at least some cases. Salicylic acid from hydrolysis of the compound is antimicrobial for toxogenic E. coli, an important pathogen in traveler's diarrhea.
A combination of bismuth subsalicylate and bismuth subcitrate is used to treat the bacteria causing peptic ulcers.
Bibrocathol is an organic bismuth-containing compound used to treat eye infections.
Bismuth subgallate, the active ingredient in Devrom, is used as an internal deodorant to treat malodor from flatulence and feces. …

Isotopes

The only primordial isotope of bismuth, bismuth-209, had long been regarded as the heaviest stable nuclide, but was suspected on theoretical grounds to be unstable to alpha decay. This was finally demonstrated in 2003, when researchers at the Institut d'astrophysique spatiale in Orsay, France, detected this decay; the best value of the half-life is now 2.01×1019 years (3 Bq/t), over 109 times longer than the estimated age of the universe. Due to its hugely long half-life, for all known medical and industrial applications, bismuth can be treated as stable. The radioactivity is of academic interest because bismuth is one of a few elements whose radioactivity was suspected and theoretically predicted before being detected in the laboratory. Bismuth has the longest known α-decay half-life, though tellurium-128 has the longest known by any mode: double beta decay at about 2.25×1024 years.
Six isotopes of bismuth with short half-lives (210–215 inclusive, but not 210m) occur in the natural radioactive decay chains of actinium, radium, thorium, and neptunium, and more have been synthesized. (Though all primordial 237Np has long since decayed, it is continually regenerated by (n,2n) knockout reactions on natural 238U.)
For medical use, bismuth-213 can be produced, as the parent isotope actinium-225, by bombarding radium with bremsstrahlung photons from a linear particle accelerator. …

Hazards & biological role

See also bismuthia, a rare dermatological condition that results from the prolonged use of bismuth.
Scientific literature indicates that some of the compounds of bismuth are less toxic to humans via ingestion than other heavy metals (lead, arsenic, antimony, etc.) presumably due to the comparatively low solubility of bismuth salts. Its biological half-life for whole-body retention is reported to be 5 days, but it can remain in the kidney for years in people treated with bismuth compounds.
Bismuth poisoning can occur and has, according to some reports, been common in relatively recent times. As with lead, bismuth poisoning can result in the formation of a black deposit on the gingiva, known as a bismuth line. Poisoning may be treated with dimercaprol, but evidence for benefit is unclear.
Bismuth's environmental impacts are not well known; it may be less likely to bioaccumulate than some other heavy metals, and this is an area of active research.