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| caption = Uranopilite with Fluorescence - Exposed in the Mineralogical Museum, Bonn, Germany
| caption = Uranopilite with Fluorescence - Exposed in the Mineralogical Museum, Bonn, Germany
| category = [[Sulfate minerals]]
| category = [[Sulfate minerals]]
| formula = (UO<sub>2</sub>)<sub>6</sub>SO<sub>4</sub>(OH)<sub>6</sub>O<sub>2</sub>·12H<sub>2</sub>O
| formula = (UO<sub>2</sub>)<sub>6</sub>SO<sub>4</sub>(OH)<sub>6</sub>O<sub>2</sub>·14H<sub>2</sub>O
| strunz = 07.EA.05
| strunz = 7.EA.05
| dana =
| dana =
| symmetry =
| symmetry = Triclinic P{{overline|1}} ({{overline|1}})
| unit cell =
| unit cell =
| molweight =
| molweight =
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| habit =
| habit =
| system =
| system =
| twinning =
| twinning = Triclinic
| cleavage =
| cleavage =
| fracture =
| fracture =
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| prop1 =
| prop1 =
| prop1text =
| prop1text =
| references = <ref>http://www.mindat.org/min-4108.html Mindat</ref><ref>https://www.mineralienatlas.de/lexikon/index.php/MineralData?mineral=Uranopilite Mineralienatlas</ref>
| references =
}}
}}
'''Uranopilite''' is a minor [[ore]] of [[uranium]] with the chemistry ([[uranium|U]][[oxygen|O]]<sub>2</sub>)<sub>6</sub>[[sulfur|S]]O<sub>4</sub>(O[[hydrogen|H]])<sub>6</sub>O<sub>2</sub>·12[[water|H<sub>2</sub>O]] or, '''Hydrated Uranyl Sulfate Hydroxide'''.
'''Uranopilite''' is a minor [[ore]] of [[uranium]] with the chemistry ([[uranium|U]][[oxygen|O]]<sub>2</sub>)<sub>6</sub>[[sulfur|S]]O<sub>4</sub>(O[[hydrogen|H]])<sub>6</sub>O<sub>2</sub>·14[[water|H<sub>2</sub>O]] or, '''Hydrated Uranyl Sulfate Hydroxide'''.


As with many uranyl minerals, it is [[fluorescent]] and [[radioactive]]. It is straw yellow in normal light. Uranopilite fluoresces a bright green under [[ultraviolet light]]. Uranopilite contains clusters of six uranyl pentagonal bipyramids that share equatorial edges and vertices, with the clusters cross-linked to form chains by sharing vertices with sulfate tetrahedra. In uranopilite, the chains are linked directly by hydrogen bonds, as well as to interstitial H<sub>2</sub>O groups.
As with many uranyl minerals, it is [[fluorescent]] and [[radioactive]]. It is straw yellow in normal light. Uranopilite fluoresces a bright green under [[ultraviolet light]]. Uranopilite contains clusters of six uranyl pentagonal bipyramids that share equatorial edges and vertices, with the clusters cross-linked to form chains by sharing vertices with sulfate tetrahedra. In uranopilite, the chains are linked directly by hydrogen bonds, as well as to interstitial H<sub>2</sub>O groups.
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== References ==
== References ==
{{reflist}}
* [http://burgaz.mit.edu/PUBLICATIONS/PDF/pssc-30-1-2002.pdf Progress in Solid State Chemistry]
* [http://burgaz.mit.edu/PUBLICATIONS/PDF/pssc-30-1-2002.pdf Progress in Solid State Chemistry]
* [http://un2sg4.unige.ch/athena/cgi-bin/minfich?s=METAURANOPILITE ATHENA MINERAL: Mineral Data]
* [http://un2sg4.unige.ch/athena/cgi-bin/minfich?s=METAURANOPILITE ATHENA MINERAL: Mineral Data]

Revision as of 07:19, 9 March 2016

Uranopilite
Uranopilite with Fluorescence - Exposed in the Mineralogical Museum, Bonn, Germany
Allgemein
KategorieSulfate minerals
Formula
(repeating unit)
(UO2)6SO4(OH)6O2·14H2O
Strunz classification7.EA.05
Space groupTriclinic P1 (1)
Identification
TwinningTriclinic
References[1][2]

Uranopilite is a minor ore of uranium with the chemistry (UO2)6SO4(OH)6O2·14H2O or, Hydrated Uranyl Sulfate Hydroxide.

As with many uranyl minerals, it is fluorescent and radioactive. It is straw yellow in normal light. Uranopilite fluoresces a bright green under ultraviolet light. Uranopilite contains clusters of six uranyl pentagonal bipyramids that share equatorial edges and vertices, with the clusters cross-linked to form chains by sharing vertices with sulfate tetrahedra. In uranopilite, the chains are linked directly by hydrogen bonds, as well as to interstitial H2O groups.

Uranopilite is associated with other uranyl minerals such as zippeite and johannite and, like them, is usually found as an efflorescent crust in uranium mines.

Notable occurrences include:

See also

References