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Bismuth
Bismuth
Bismuth
Bismuth

Bismuth

Bismuth

A species of Arsenic Group

Bismuth is a crystalline white metal that forms into interesting step pyramid shapes and oxidizes into a variety of colors when heated and cooled. It is used to manufacture fire extinguishers, fire sprinkler systems, ammunition. Although bismuth is mined in several countries, only Bolivia has a mine where it is the primary mineral extracted.

Hardness
Hardness:

2 - 2.5

Density
Density:

9.753 g/cm³

General Info About Bismuth

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Physical Properties of Bismuth

Luster
Metallic
Diaphaneity
Opaque
Colors
Reddish-white to creamy-white, pinkish, yellowish, bluish
Magnetism
Non-magnetic
Tenacity
Sectile
Cleavage
Perfect
Fracture
Uneven
Streak
Silver-white
Crystal System
Trigonal
Hardness
2 - 2.5 , Extremely soft
Density
9.753 g/cm³, Obviously Heavy Weight
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Chemical Properties of Bismuth

Chemical Classification
Native elements
Formula
Bi
Elements listed
Bi
Common Impurities
Fe,Te,As,S,Sb

Discover the Value of Bismuth

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Rarity
Easy to obtain
Collection Recommendation
3.9 out of 5
Popularity
3.7
Aesthetic
4.1
Rarity
3.5
Sci-Cultural Value
3.7

The Market Price of Bismuth

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Size is a decisive factor affecting the price of bismuth. The price of a 100 g bismuth crystal is usually $15-$30/piece.

Rough/Tumbled Price

Fixed Price
$0.2 - $0.8 g

How to Care for Bismuth?

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Durability
Nondurable
Scratch resistance
Poor

Toughness of Bismuth

Poor
Fair
Good
Excellent
Bismuth exhibits poor toughness, meaning it can easily break, chip, or crack under daily impacts due to its cleavage and brittle internal structure.

Stability of Bismuth

Sensitive
Stable
Bismuth's susceptibility to oxidation in water, deformation under heat, and negative reactions with harsh chemicals makes it sensitive for daily use.
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Characteristics of Bismuth

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Characteristics of Bismuth

Bismuth is a brittle metal with a white, 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, antimony, and polonium. No other metal is verified to be more naturally diamagnetic than bismuth. (Superdiamagnetism is a different physical phenomenon.) Of any metal, it has one of the lowest values of thermal conductivity (after manganese, and maybe neptunium and plutonium) and the highest Hall coefficient. It has a high electrical resistivity. 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, and water. Bismuth expands 3.32% on solidification; therefore, it was long a component of low-melting typesetting alloys, where it compensated for the contraction of the other alloying components to form almost isostatic bismuth-lead eutectic alloys. Though virtually unseen in nature, high-purity bismuth can form distinctive, colorful hopper crystals. It is relatively nontoxic and has a low melting point just above 271 °C, so crystals may be grown using a household stove, although the resulting crystals will tend to be of lower quality than lab-grown crystals. At ambient conditions, bismuth shares the same layered structure as the metallic forms of arsenic and antimony, crystallizing in the rhombohedral lattice (Pearson symbol hR6, space group R3m No. 166) of the trigonal crystal system. When compressed at room temperature, this Bi-I structure changes first to the monoclinic Bi-II at 2.55 GPa, then to the tetragonal Bi-III at 2.7 GPa, and finally to the body-centered cubic Bi-V at 7.7 GPa. The corresponding transitions can be monitored via changes in electrical conductivity; they are rather reproducible and abrupt and are therefore used for calibration of high-pressure equipment.

Formation of Bismuth

In the Earth's crust, bismuth is about twice as abundant as gold. The most important ores of bismuth are bismuthinite and bismite. Native bismuth is known from Australia, Bolivia, and China. The difference between mining and refining production reflects bismuth's status as a byproduct of extraction of other metals such as lead, copper, tin, molybdenum and tungsten. World bismuth production from refineries is a more complete and reliable statistic. 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 will behave 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).

Cultural Significance of Bismuth

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Uses of Bismuth

Bismuth compounds account for about half the production of bismuth. They are used in cosmetics, pigments, and a few pharmaceuticals, notably bismuth subsalicylate, used to treat diarrhea. Bismuth's unusual propensity to expand as it solidifies is responsible for some of its uses, such as in the casting of printing type. Bismuth has unusually low toxicity for a heavy metal. As the toxicity of lead has become more apparent in recent years, there is an increasing use of bismuth alloys (presently about a third of bismuth production) as a replacement for lead.

The History of Bismuth

Bismuth metal has been known since ancient times, although it was often confused with lead and tin, which share some physical properties. The etymology is uncertain but possibly comes from the German words weiße Masse or Wismuth ("white mass"), translated in the mid-sixteenth century to New Latin bisemutum or bisemutium. The name bismuth dates from around the 1660s and is of uncertain etymology. It is one of the first 10 metals to have been discovered. Bismuth appears in the 1660s, from obsolete German Bismuth, Wismut, Wissmuth (early 16th century); perhaps related to Old High German hwiz ("white"). The New Latin bisemutium (due to Georgius Agricola, who Latinized many German mining and technical words) is from the German Wismuth, perhaps from weiße Masse, "white mass". The element was confused in early times with tin and lead because of it resembles those elements. Because Bismuth has been known since ancient times, no one person is credited with its discovery. Agricola, in De Natura Fossilium (c. 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. 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. Bismuth was also known to the Incas and used (along with the usual copper and tin) in a special bronze alloy for knives.

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