Shcherbinaite (original) (raw)
A valid IMA mineral species
About ShcherbinaiteHide
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Colour:
Yellow-green, golden-yellow
Specific Gravity:
3.38 (Calculated)
Crystal System:
Orthorhombic
Name:
Named after Vladimir Vital'evich Shcherbina (Владимир Витальевич Щербина) (20 November 1907, St. Petersburg, Russian Empire - 20 July 1978, Moscow, USSR), geochemist and mineralogist. He was a student of Alexander Fersman. In 1931, he led a team from the USSR Academy of Sciences in the mineralogical examination of the Lovozero Massif.
This page provides mineralogical data about Shcherbinaite.
Unique IdentifiersHide
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Long-form identifier:
mindat:1:1:3636:4
e1fba82f-26d9-4c2d-938c-b17bc81f42b0
IMA Classification of ShcherbinaiteHide
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Type description reference:
Classification of ShcherbinaiteHide
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4.HE.10
4 : OXIDES (Hydroxides, V[5,6] vanadates, arsenites, antimonites, bismuthites, sulfites, selenites, tellurites, iodates)
H : V[5,6] Vanadates
E : Phyllovanadates
4.6.1.1
4 : SIMPLE OXIDES
6 : Miscellaneous
Mineral SymbolsHide
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As of 2021 there are now IMA–CNMNC approved mineral symbols (abbreviations) for each mineral species, useful for tables and diagrams.
Symbol | Source | Reference |
---|---|---|
Shc | IMA–CNMNC | Warr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43 |
Physical Properties of ShcherbinaiteHide
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Colour:
Yellow-green, golden-yellow
Cleavage:
Perfect
Two perfect {010} and {001}
Density:
3.38 g/cm3 (Calculated)
Optical Data of ShcherbinaiteHide
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Dispersion:
marked to extreme
Chemistry of ShcherbinaiteHide
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Crystallography of ShcherbinaiteHide
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Crystal System:
Orthorhombic
Class (H-M):
m m m _(_2/_m_2/_m_2/m ) - Dipyramidal
Cell Parameters:
a = 11.51 Å, b = 3.55 Å, c = 4.37 Å
Ratio:
a:b:c = 3.242 : 1 : 1.231
Unit Cell V:
178.56 ų (Calculated from Unit Cell)
Morphology:
Needles and laths to 1 cm.
Twinning:
Contact twins {031}
Crystal StructureHide
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ID | Species | Reference | Link | Year | Locality | Pressure (GPa) | Temp (K) |
---|---|---|---|---|---|---|---|
0018020 | Shcherbinaite | Ketelaar J (1936) Die Kristallstruktur des Vanadinpentoxyds _cod_database_code 1011126 Zeitschrift fur Kristallographie 95 9-27 | 1936 | 0 | 293 | ||
0018140 | Shcherbinaite | Ketelaar J (1936) Die Kristallstruktur des Vanadiumpentoxyds _cod_database_code 1011291 Zeitschrift fur Kristallographie 95 9-27 | 1936 | 0 | 293 | ||
0018088 | Shcherbinaite | Ketelaar J (1936) Kristalstructuur en colloidchemische Eigenschappen van Vanadiumpentoxyd _cod_database_code 1011225 Chemisch Weekblad 33 51-57 | 1936 | 0 | 293 | ||
0013889 | Shcherbinaite | Shklover V, Haibach T, Ried F, Nesper R, Novak P (1996) Crystal structure of the product of Mg2+ insertion into V2O5 single crystals Journal of Solid State Chemistry 123 317-323 | 1996 | synthetic | 0 | 293 | |
0013890 | Shcherbinaite | Shklover V, Haibach T, Ried F, Nesper R, Novak P (1996) Crystal structure of the product of Mg2+ insertion into V2O5 single crystals Journal of Solid State Chemistry 123 317-323 | 1996 | synthetic | 0 | 293 | |
0013891 | Shcherbinaite | Shklover V, Haibach T, Ried F, Nesper R, Novak P (1996) Crystal structure of the product of Mg2+ insertion into V2O5 single crystals Journal of Solid State Chemistry 123 317-323 | 1996 | synthetic | 0 | 293 | |
0018051 | Shcherbinaite | Ketelaar J (1936) Crystal structure and shape of colloidal particles of vanadium pentoxide _cod_database_code 1011174 Nature (London) 137 316-316 | 1936 | 0 | 293 |
CIF Raw Data - click here to close
X-Ray Powder DiffractionHide
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Powder Diffraction Data:
d-spacing | Intensity |
---|---|
5.726 Å | (22) |
4.339 Å | (100) |
4.067 Å | (28) |
3.411 Å | (28) |
2.883 Å | (50) |
2.760 Å | (22) |
2.176 Å | (24) |
Geological EnvironmentHide
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Geological Setting:
Fumaroles
Type Occurrence of ShcherbinaiteHide
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General Appearance of Type Material:
Finely fibrous aggregates of acicular crystals <1.5 mm long and <0.1 mm thick.
Geological Setting of Type Material:
Fumarole with gasses rich in HCl and HF.
Reference:
Borisenko, L.F. (1972) The new mineral shcherbinaite. Zapiski Vsesoyuznogo Mineralogicheskogo Obshchestva: 101(4): 464-464.
Synonyms of ShcherbinaiteHide
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Other Language Names for ShcherbinaiteHide
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Common AssociatesHide
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Associated Minerals Based on Photo Data:
Related Minerals - Strunz-mindat GroupingHide
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4.HE.05 | Melanovanadite | Ca(V5+,V4+)4O10 · 5H2O | Tric. 1 : _P_1 |
---|---|---|---|
4.HE.15 | Hewettite | CaV6O16 · 9H2O | Mon. 2/m : _P_21/m |
4.HE.15 | Metahewettite | CaV6O16 · 3H2O | Mon. 2/m |
4.HE.20 | Bariandite | Al0.6(V5+,V4+)8O20 · 9H2O | Mon. |
4.HE.20 | Bokite | (Al,Fe)1.3(V5+,V4+,Fe3+)8O20 · 7.5H2O | Mon. |
4.HE.20 | Corvusite | (Na,K,Ca,Mg)2(V5+,V4+,Fe2+)8O20 · 6-10H2O | Mon. 2/m : _B_2/m |
4.HE.20 | Fernandinite | (Ca,K)(V5+,V4+,Fe2+)8O20 · 10H2O | Mon. 2/m : _B_2/m |
4.HE.20 | Straczekite | (Ca,K,Ba)(V5+,V4+)8O20 · 3H2O | Mon. 2/m : _B_2/m |
4.HE.25 | Häggite | V3+V4+O2(OH)3 | Mon. 2/m : _B_2/m |
4.HE.30 | Doloresite | V4+3O4(OH)4 | Mon. 2/m : _B_2/m |
4.HE.35 | Duttonite | V4+O(OH)2 | Mon. 2/m |
4.HE.40 | Cavoite | CaV4+3O7 | Orth. m m m _(_2/_m_2/_m_2/m ) : P n m a |
Other InformationHide
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Notes:
Dissolves readily in HCl or HNO3.
Health Risks:
No information on health risks for this material has been entered into the database. You should always treat mineral specimens with care.
Internet Links for ShcherbinaiteHide
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References for ShcherbinaiteHide
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Localities for ShcherbinaiteHide
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This map shows a selection of localities that have latitude and longitude coordinates recorded. Click on the symbol to view information about a locality. The symbol next to localities in the list can be used to jump to that position on the map.
Locality ListHide
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- This locality has map coordinates listed. - This locality has estimated coordinates. ⓘ - Click for references and further information on this occurrence. ? - Indicates mineral may be doubtful at this locality. - Good crystals or important locality for species. - World class for species or very significant. (TL) - Type Locality for a valid mineral species. (FRL) - First Recorded Locality for everything else (eg varieties). Struck out - Mineral was erroneously reported from this locality. Faded * - Never found at this locality but inferred to have existed at some point in the past (e.g. from pseudomorphs).
All localities listed without proper references should be considered as questionable.