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词条 Bartelkeite
释义

  1. Occurrence and association

  2. Crystal structure

  3. References

{{infobox mineral
| name = Bartelkeite
| category = Germanate mineral
| image =
| imagesize =
| alt =
| caption =
| formula = PbFeGe(Ge2O7)(OH)2•H2O
| strunz = 9.J0.10 (10 ed)
4/C.08-60 (8 ed)
| dana = 7.6.2.1
| system = Monoclinic
| class = Spheroidal (2) or prismatic (2/m)
| symmetry = P21 or P21/m
| unit cell = a = 5.83, b = 13.62, c = 6.31 [Å], β = 127.31° (approximated); Z = 2
| color = Colorless, white, very pale greenish
| colour =
| habit = tabular; acicular
| twinning =
| cleavage = {101}, distinct
| fracture =
| tenacity =
| mohs = 4
| luster = Subadamantine
| streak = White
| diaphaneity = Transparent
| gravity =
| density = 4.97
| polish =
| opticalprop = Biaxal (-)
| refractive = nα=1.89, nβ=1.91, nγ=1.91 (approximated)
| birefringence =
| pleochroism =
| 2V = ca. 35o (measured)
| dispersion =
| extinction =
| length fast/slow =
| fluorescence =
| absorption =
| melt =
| fusibility =
| diagnostic =
| solubility =
| impurities =
| alteration =
| other =
| references = [1][1][3]
}}Bartelkeite is an exceptionally rare mineral, one of scarce natural germanium compounds.[2] The formula was originally assumed to be PbFeGe3O8,[3] bartelkeite was later shown to be isostructural with a high-pressure form of the mineral lawsonite. Thus, its correct formula is PbFeGe(Ge2O7)(OH)2•H2O.[4] Bartelkeite and mathewrogersite are minerals with essential (dominant) lead, iron and germanium.[5] Both come from Tsumeb, Namibia - a world's "capital" of germanium minerals.[6]

Occurrence and association

Bartelkeite was detected in voids of germanium ore occurring within dolostones. The mineral associates with galena, germanite, reniérite, and tennantite.[1]

Crystal structure

Bartelkeite is the first analyzed mineral containing both tetrahedrally- and octahedrally-coordinated germanium. It is isostructural with high-pressure form of the silicate lawsonite. In the structure there are:[4]

  • chains of FeO6 and GeO6 octahedra, that share edges
  • Ge2O7 dimers that cross-link the chains
  • Pb atoms and water molecules in large cavities of the framework

References

1. ^{{cite web|url=http://www.handbookofmineralogy.org/pdfs/bartelkeite.pdf |title=Bartelkeite - Handbook of Mineralogy |website=Handbookofmineralogy.org |accessdate=2016-03-12}}
2. ^{{cite web|url=http://www.mindat.org/min-541.html |title=Bartelkeite: Bartelkeite mineral information and data |website=Mindat.org |accessdate=2016-03-04}}
3. ^Keller, V.P., Hess, H., and Dunn, P.J., 1981. Bartelkeit, PbFe2+Ge3O8, ein neues Germanium-Mineral von Tsumeb, Namibia. Chemie der Erde 40, 201-206 (in German)
4. ^Origlieri, M.J., Yang, H., Downs, R.T., Posner, E.S., Domanik, K.J., and Pinch, W.P., 2012. The crystal structure of bartelkeite, with a revised chemical formula, PbFeGeVI(Ge2IVO7)(OH)2·H2O, isotypic with high-pressure P21/m lawsonite. American Mineralogist 97(10), 1812-1815
5. ^{{cite web|url=http://www.mindat.org/min-2590.html |title=Mathewrogersite: Mathewrogersite mineral information and data |website=Mindat.org |accessdate=2016-03-04}}
6. ^{{cite web|url=http://www.mindat.org/loc-2428.html |title=Tsumeb Mine (Tsumcorp Mine), Tsumeb, Otjikoto Region (Oshikoto), Namibia - Mindat.org |website=Mindat.org |accessdate=2016-03-10}}
{{mineral-stub}}

5 : Oxide minerals|Germanium minerals|Lead minerals|Iron minerals|Monoclinic minerals

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