Physical properties
Bismuth (Ger., Weisse Masse, white mass, later Wismuth, latinized to ‘bisemutum’). Atomic symbol: Bi. Atomic weight: 208.9804. Atomic number: 83. Electron configuration: [Xe]4f145d106s2p3. Melting point: 544.52°C. Boiling point: 1837°C. Density: 9.8 g/cm3 at 300 K. Oxidation states: 0, ±3, +5. Ionic radius: 1.01 Å. Electronegativity (Pauling's): 2.02. Crystal modifications: rhombohedral metallic form. Isotopic abundance; Bi 209, 100%; several other isotopes occur as short lived daughter products in the decay of the following radioisotopes: U238→Bi 210 and Bi 214; U235→Bi 211 and Bi 213; Th232→Bi 212. Bismuth is a brittle, diamagnetic, reddish white metal which tarnishes brassy and is a poor conductor of heat and electricity.
Minerals and compounds
Bismuth is occasionally found as native metal containing traces of arsenic (As), sulfur (S), and tellurium (Te). The most common natural mineral form is the mineral bismuthinite (Bi2S3). Bismuthinite closely resembles...
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Bibliography
Ahrens, L. and Erlank, A.J. (1969) Bismuth, in Handbook of Geochemistry (ed. K.H. Wedepohl). New York: Springer-Verlag, pp. 83–A–1–83–O–1.
Angino, E.E. and Long, D.T. (eds) (1969) The Geochemistry of Bismuth. Stroudsberg, PA: Dowden, Hutchinson, & Ross, 689 pp.
Fergusson, J.E. (1990) The Heavy Elements: Chemistry, Environmental Impact and Health Effects. New York: Pergamon Press, 614 pp.
Hale, M. (1981) Pathfinder applications of arsenic, antimony, and bismuth in geochemical exploration. J. Geochem. Exp., 15, 307–23.
Heinrichs, H., Schulz-Dobrick, B. and Wedepohl, K.H. (1980) Rb. Geochim. Cosmochim. Acta, 44, 1519–33.
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Lueth, V.W. (1998). Bismuth: Element and geochemistry. In: Geochemistry. Encyclopedia of Earth Science. Springer, Dordrecht. https://doi.org/10.1007/1-4020-4496-8_33
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DOI: https://doi.org/10.1007/1-4020-4496-8_33
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