Sturmanite is a rare sulfate mineral with the chemical formula Ca6Fe3 2(SO4)2.5(B(OH)4)(OH)12 · 25 H2O.[2][3][4] It crystallises in the tetragonal system and it has a Moh's hardness of 2.5. Sturmanite has a bright yellow to amber colour and falls in the ettringite group. It was named after Bozidar Darko Sturman (born 1937), Croatian-Canadian mineralogist and Curator Emeritus of Mineralogy, Royal Ontario Museum.[5]

Sturmanite
Distinctive sturmanite on matrix from the N'Chwaning Mines. Size: 5.4 x 4.2 x 1.7 cm. Ex.Charlie Key Stock
General
CategorySulfate minerals
Formula
(repeating unit)
Ca6Fe3 2(SO4)2.5[B(OH)4](OH)12 · 25 H2O
IMA symbolStrm[1]
Strunz classification7.DG.15
Dana classification32.4.4.2
Crystal systemTrigonal
Crystal class3m - Ditrigonal Pyramidal
Space groupP31c (no. 159)
Unit cella = 11.188(9) Å, c = 21.91(7) Å
Identification
ColorBright yellow to amber
Crystal habitHexagonal, pyramidal, prismatic
CleavagePerfect {1010}
TenacityBrittle
Mohs scale hardness2.5
LusterVitreous, greasy
StreakPale yellow, greenish yellow, brownish orange
DiaphaneityTransparent to translucent
Specific gravity1.847 (measured) 1.855 (calculated)
Optical propertiesUniaxial ( /-)
Birefringenceδ = 0.002
Ultraviolet fluorescencenone

Occurrence

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Sturmanite was first identified in 1983 and approved by the IMA in the same year.[4][5] It was first found in the Black Rock Mine, Black Rock, Kalahari manganese field, Northern Cape Province, South Africa. It is found as flattened dipyramidal crystals on hematite and baryte.[5] Sturmanite has also been identified in mines near the Black Rock Mine, such as the Wessel's and Perth mines, in the N'Chwaning mines, and near Lakargi Mountain in Russia.[2] It is found as a rare secondary mineral embedded in manganese deposits and is associated with baryte, manganite, hausmannite, and hematite.[3]

Crystal structure

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The crystal structure of sturmanite shows two distinct features: one being columns of iron-octahedra and calcium polyhedra, the other being the SO4 and B(OH)4 tetrahedra surrounding these columns. These two structures are linked together through a dense and complex network of hydrogen bonds.[6]

References

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  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 235729616.291-320&rft.date=2021&rft_id=https://api.semanticscholar.org/CorpusID:235729616#id-name=S2CID&rft_id=info:doi/10.1180/mgm.2021.43&rft_id=info:bibcode/2021MinM...85..291W&rft.aulast=Warr&rft.aufirst=L.N.&rft_id=https://doi.org/10.1180%2Fmgm.2021.43&rfr_id=info:sid/en.wikipedia.org:Sturmanite" class="Z3988">
  2. ^ a b "Sturmanite: Sturmanite mineral information and data". www.mindat.org. Retrieved 2017-02-19.
  3. ^ a b "Sturmanite" (PDF). Handbook of mineralogy.
  4. ^ a b Barthelmy, Dave. "Sturmanite Mineral Data". www.webmineral.com. Retrieved 2017-02-19.
  5. ^ a b c Peacor, D.R., Dunn, P.J., Duggan, M. (1983). "Sturmanite, a ferric iron, boron analogue of ettringite". Canadian Mineralogist. 21: 705–709.705-709&rft.date=1983&rft.au=Peacor, D.R., Dunn, P.J., Duggan, M.&rft_id=https://www.researchgate.net/publication/242120069&rfr_id=info:sid/en.wikipedia.org:Sturmanite" class="Z3988">{{cite journal}}: CS1 maint: multiple names: authors list (link)
  6. ^ Pushcharovsky, D.Y., Lebedeva, Y.S., Zubkova, N.V., Pasero, M., Bellezza, M., Merlino, S., Chukanov, N.V. (2004). "The crystal structure of sturmanite" (PDF). The Canadian Mineralogist. 42 (3): 723–729. CiteSeerX 10.1.1.605.4915. doi:10.2113/gscanmin.42.3.723.723-729&rft.date=2004&rft_id=https://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.605.4915#id-name=CiteSeerX&rft_id=info:doi/10.2113/gscanmin.42.3.723&rft.au=Pushcharovsky, D.Y., Lebedeva, Y.S., Zubkova, N.V., Pasero, M., Bellezza, M., Merlino, S., Chukanov, N.V.&rft_id=http://rruff.info/doclib/cm/vol42/CM42_723.pdf&rfr_id=info:sid/en.wikipedia.org:Sturmanite" class="Z3988">{{cite journal}}: CS1 maint: multiple names: authors list (link)