Lipscombite

Lipscombite: Small green crystals on quartz, Harvard Museum of Natural History

General
Category| Phosphate minerals
Formula
(repeating unit)| (Fe2+,Mn2+)(Fe3+)2(PO4)2(OH)2
IMA symbol| Lcb[1]
Strunz classification| 8.BB.90
Dana classification| 41.10.02.01
Crystal system| Tetragonal
Crystal class| Trapezohedral (422)
(same H-M symbol)
Space group| P43212
Unit cell| a = 5.37, c = 12.81 [Å]; Z = 4
Identification
Formula mass| 391.27 g/mol
Color| Green gray, olive green, black.
Specific gravity| 3.68
Optical properties| Translucent to opaque
References| [2][3]
Lipscombite: Small yellowish-green crystals, Lichtenberg Absetzer Mine dump, Ronneburg Uranium deposit, Gera, Thuringia, Germany Lipscombite: Small black crystals on dark background. Smithsonian National Museum of Natural History

Lipscombite (Fe2+,Mn2+)(Fe3+)2(PO4)2(OH)2[2][3] is a green gray, olive green, or black. phosphate-based mineral containing iron, manganese, and iron phosphate.

Lipscombite is often formed at meteorite impact sites where its crystals are microscopically small, because crystal-forming conditions of pressure and temperature are brief.

In the Classification of non-silicate minerals lipscombite is in the lipscombite group, which also includes zinclipscombite. This group is within the non-silicate, category 8, anhydrous phosphates, lazulite supergroup.

## Discovery[edit]

The mineral lipscombite was first made artificially and then found in nature. It was named after chemist William Lipscomb by the mineralogist John W. Gruner who first made it artificially.[4][5]

While investigating the stability relations of iron oxides small, black, shiny crystals were obtained when a spherical iron pressure-temperature vessel was contaminated with phosphorus.[6] The x-ray powder diffraction pattern was similar to lazulite, but unknown.

Gruner, a mineralogist at the University of Minnesota, gave Lipscomb, a chemistry professor there, the crystals for Lewis Katz and Lipscomb to determine the atomic structure using single-crystal x-ray diffraction. They initially called the mineral iron lazulite.[7]

## References[edit]

1. ^ Warr, L.N. (2021). "IMA–CNMNC approved mineral symbols". Mineralogical Magazine. 85 (3): 291–320. Bibcode:2021MinM...85..291W. doi:10.1180/mgm.2021.43. S2CID 235729616.
2. ^ a b Lipscombite on Mindat
3. ^ a b Lipscombite data on WebMineral
4. ^ Gheith, M. A. , Lipscombite: A New Synthetic Iron Lazulite, Amer. Mineral., 38, 612-628 (1953)
5. ^ Structures and Mechanisms: From Ashes to Enzymes (Acs Symposium Series) Gareth R. Eaton (Editor), Don C. Wiley (Editor), Oleg Jardetzky (Editor), American Chemical Society, Washington, DC (2002) (Autobiographical sketch by William Lipscomb, 14 pp. (Lipscombite: p. xvii). This chapter is online at pubs.acs.org. Click PDF symbols at right.
6. ^ Gheith, Mohamed A. Stability relations of ferric oxides and their hydrates. Lipscombite: a new synthetic iron lazulite. Thesis University of Minnesota (1951)
7. ^ Katz L., Lipscomb W. N. The crystal structure of iron lazulite, a synthetic mineral related to lazulite: Acta Crystallographica, 4, 345-348 (1951).

## External links[edit]

Gallery of lipscombite pictures at mindat.org.

Wikimedia Commons has media related to Lipscombite.

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