Rock & Gem

BISMUTH: IRIDESCENC­E AND MORE

- BY STEVE VOYNICK

Among the most eye-catching items displayed at gem-and-mineral shows and rock shops are those familiar clusters of metallic “hopper” crystals that gleam like iridescent rainbows. These wildly colorful, synthetic crystals are bismuth and the only elemental bismuth that most of us ever see.

Bismuth is a brittle, silver-white metal with a hint of pink and sometimes a multicolor­ed tarnish. Its physical properties are somewhat similar to those of lead, although bismuth is more rigid and much less abundant. And bismuth’s melting point of 520 degrees F. (271 degrees C.) is substantia­lly lower than that of lead.

Bismuth’s large atom has a correspond­ingly high atomic weight of 208.9, higher even than gold and platinum. Atomic weight is a relative measure of atomic mass and does not indicate density. Bismuth’s loose atomic packing gives it a density (specific gravity 9.8) less than that of lead (specific gravity 11.3). Also, it weakens its metallic bonding, which explains its softness and low melting temperatur­e.

Believing it to be “unripened silver,” medieval alchemists knew bismuth as tectum argenti (“silver being made”). Bismuth was confused with lead and tin until 1546 when German scholar Georgius Agricola suggested a different metal (Revisit the March 2021 issue of Rock & Gem to learn more about Mr. Agricola). But it wasn’t until 1753 that French chemist Claude Françoise Geoffroy conclusive­ly proved that bismuth is a distinct element. Bismuth’s name stems from the German Wismut, or “white mass,” likely alluding to its white oxide.

Although occasional­ly occurring as a native metal, bismuth is most abundant as the trisulfide bismuthini­te (Bi2S3), which is often associated with the sulfide ores of lead, cobalt, zinc, and silver. Other important bismuthbea­ring minerals are bismutite (bismuth oxycarbona­te, BiO2CO3) and bismite (bismuth oxide, Bi2O3).

About 19,000 metric tons of bismuth are recovered worldwide annually, almost all as a by-product of lead and silver smelting. China accounts for 85 percent of the world’s production. With the demise of lead smelting in the United States, the nation depends on foreign sources for its entire bismuth supply.

The industrial price for refined metallic bismuth is now about $5 per pound.

Bismuth’s uses are keyed to its unusual properties. Many bismuth alloys have extremely low melting points, some even lower than the boiling point of water. Most metallic bismuth is used to man-ufacture heatliable plugs in automatic, sprinkler-type fire-suppressio­n systems.

Bismuth is extremely diamagneti­c and repels magnetism. And unlike other metals, its electrical re-sistance increases in magnetic fields, making it useful in magnetomet­ers and other instrument­s that measure magnetic intensity.

Bismuth expands upon solidifyin­g, a property shared by only two other common materials—water and antimony. Bismuth casting and soldering alloys, respective­ly, can thus fill the finest details of a mold and completely seal soldered joints. And because it is nontoxic, bismuth substitute­s for lead in shotgun pellets, fishing sinkers, ceramic glazes, crystal glass, and plumbing solders.

For centuries, bismuth compounds also have served as remedies for stomach ailments. The “Bis” in PeptoBismo­l® stems from its active ingredient—bismuth subsalicyl­ate, an antimicrob­ial and anti-inflammato­ry agent, and an antacid. Kaopectate® and similar over-thecounter remedies also contain bismuth subsalicyl­ate.

Despite its unusual properties and uses, bismuth remains best-known for those iridescent, synthetic crystals with their rainbow-like colors. These are created by cooling molten bismuth slowly so that it crystalliz­es into clusters of cubes with outward-extending edges and repetitive, inner “stair-steps” descending to concave centers—the classic “hopper” configurat­ion. Because bismuth crystalliz­es in the trigonal system, these cube-shaped crystals are actually a pseudocubi­c habit.

As it solidifies, bismuth reacts with atmospheri­c oxygen to form microscopi­cally thin, surface films of bismuth oxide. The bright, iridescent cyan, green, gold, and magenta colors that light up those hopper crystals are not related to metallic bismuth but are caused instead by how light interacts with and reflects from thin surface films of bismuth oxide.

 ?? WIKIMEDIA COMMONS ?? The bright, iridescent cyan, green, gold, and magenta colors seen on crystals of metallic bismuth are caused by the manner in which light interacts with, and reflects from, thin surface films of bismuth.
WIKIMEDIA COMMONS The bright, iridescent cyan, green, gold, and magenta colors seen on crystals of metallic bismuth are caused by the manner in which light interacts with, and reflects from, thin surface films of bismuth.
 ??  ?? Steve Voynick is a science writer, mineral collector, and former hardrock miner, and the author of guidebooks like Colorado Rockhoundi­ng and New Mexico Rockhoundi­ng.
Steve Voynick is a science writer, mineral collector, and former hardrock miner, and the author of guidebooks like Colorado Rockhoundi­ng and New Mexico Rockhoundi­ng.

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