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Schmitterite

A valid IMA mineral species
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About SchmitteriteHide

Formula:
(UO2)(TeO3)
Colour:
Very pale straw yellow, colourless to pale yellow
Lustre:
Pearly
Hardness:
1
Specific Gravity:
6.878
Crystal System:
Orthorhombic
Name:
Named in honor of Eduardo Schmitter Villada (21 June 1904, Toluca, Mexico - 1982(?)), Professor of Mineralogy and Petrology at the National University of Mexico and also Research Petrologist at the Mexican Institute of Geology at the University.
Structurally related to Moctezumite.


Unique IdentifiersHide

Mindat ID:
3570
Long-form identifier:
mindat:1:1:3570:1

IMA Classification of SchmitteriteHide

Classification of SchmitteriteHide

4.JK.70

4 : OXIDES (Hydroxides, V[5,6] vanadates, arsenites, antimonites, bismuthites, sulfites, selenites, tellurites, iodates)
J : Arsenites, antimonites, bismuthites, sulfites, selenites, tellurites; iodates
K : Tellurites without additional anions, without H2O
Dana 7th ed.:
34.1.7.1
34.1.6.1

34 : SELENITES, TELLURITES AND SULFITES
1 : A(XO3)
28.3.19

28 : Selenites, Selenates, Tellurites, and Tellurates
3 : Tellurites

Mineral SymbolsHide

As of 2021 there are now IMA–CNMNC approved mineral symbols (abbreviations) for each mineral species, useful for tables and diagrams.

SymbolSourceReference
SciIMA–CNMNCWarr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43

Physical Properties of SchmitteriteHide

Pearly
Transparency:
Translucent
Colour:
Very pale straw yellow, colourless to pale yellow
Hardness:
Tenacity:
Waxy
Cleavage:
Poor/Indistinct
{100}
Density:
6.878 g/cm3 (Measured)    6.916 g/cm3 (Calculated)

Optical Data of SchmitteriteHide

Type:
Biaxial (-)
Comments:
X = c; Y = b; Z = a
α = n.d.; β = 2.05; γ > 2.11

Chemistry of SchmitteriteHide

Mindat Formula:
(UO2)(TeO3)
Element Weights:
Element% weight
U53.415 %
Te28.634 %
O17.952 %

Calculated from ideal end-member formula.

Crystallography of SchmitteriteHide

Crystal System:
Orthorhombic
Class (H-M):
mmm (2/m 2/m 2/m) - Dipyramidal
Cell Parameters:
a = 7.860(4) Å, b = 10.089(2) Å, c = 5.363(2) Å
Ratio:
a:b:c = 0.779 : 1 : 0.532
Unit Cell V:
425.28 ų (Calculated from Unit Cell)
Z:
4
Comment:
Space Group: P21ab (synthetic).

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0009479SchmitteriteMeunier G, Galy J (1973) Structure cristalline de la schmitterite synthetique UTeO5 Acta Crystallographica B29 1251-12551973synthetic0293
0009637SchmitteriteLoopstra B O, Brandenburg N P (1978) Uranyl selenite and uranyl tellurite Acta Crystallographica B34 1335-13371978Synthetic0293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
3.682 Å(100)
5.35 Å(90)
3.099 Å(90)
4.73 Å(80)
3.170 Å(80)
1.971 Å(70)
1.549 Å(60)

Geological EnvironmentHide

Paragenetic Mode(s):

Type Occurrence of SchmitteriteHide

Place of Conservation of Type Material:
Institute of Geology, National University of Mexico, Mexico City, Mexico.
Smithsonian Institution, U.S. National Museum, Washington, D.C., specimen 122475.
Associated Minerals at Type Locality:

Synonyms of SchmitteriteHide

Other Language Names for SchmitteriteHide

Common AssociatesHide

Associated Minerals Based on Photo Data:
24 photos of Schmitterite associated with EmmonsiteFe3+2(TeO3)3 · 2H2O
5 photos of Schmitterite associated with MoctezumitePb(UO2)(TeO3)2
5 photos of Schmitterite associated with QuartzSiO2
2 photos of Schmitterite associated with MackayiteFe3+(Te4+2O5)(OH)
1 photo of Schmitterite associated with ZemanniteMg0.5ZnFe3+(Te4+O3)3 · 4.5H2O
1 photo of Schmitterite associated with BaryteBaSO4

Related Minerals - Strunz-mindat GroupingHide

4.JK.MatthiasweilitePbTe4+O3Tric. 1 : P1
4.JK.05Walfordite(Fe3+,Te6+)Te4+3O8Iso. m3 (2/m 3) : Ia3
4.JK.05WinstanleyiteTiTe4+3O8Iso. m3 (2/m 3) : Ia3
4.JK.10ZincospiroffiteZn2Te4+3O8Mon. 2/m : B2/b
4.JK.10SpiroffiteMn2+2Te4+3O8Mon. 2/m : B2/b
4.JK.15BalyakiniteCu(TeO3)Orth. mmm (2/m 2/m 2/m)
4.JK.20RajiteCu(Te4+2O5)Mon. 2/m : P21/b
4.JK.25CarlfriesiteCaTe4+2Te6+O8Mon. 2/m : B2/b
4.JK.30ChenzhangruiteMnFe2+Te4+4O10Tet. 4/mmm (4/m 2/m 2/m) : P42/nbc
4.JK.30StankeithiteMn2+Mn2+Te4+4 O10Tet. 4 : P42
4.JK.30Denningite(Mn2+,Ca,Zn)Te4+2O5Tet. 4/mmm (4/m 2/m 2/m) : P42/nbc
4.JK.35ChekhovichiteBi2Te4+4O11Mon. 2/m
4.JK.40SmirniteBi2Te4+O5Orth. mm2
4.JK.45Choloalite(Cu,Sb)3(Pb,Ca)3(TeO3)6ClIso. 4 3 2 : P41 3 2
4.JK.50FairbankitePb2+12(Te4+O3)11(SO4)Tric. 1 : P1
4.JK.55PlumbotelluritePb(TeO3)Mon. 2/m : B2/b
4.JK.60Magnolite[Hg2]2+[Te4+O3]Orth. mm2
4.JK.65MoctezumitePb(UO2)(TeO3)2Mon. 2/m : P21/b
4.JK.75Cliffordite(UO2)Te4+3O7Iso. m3 (2/m 3) : Pa3

RadioactivityHide

Radioactivity:
Element % Content Activity (Bq/kg) Radiation Type
Uranium (U) 53.4145% 13,353,625 α, β, γ
Thorium (Th) 0.0000% 0 α, β, γ
Potassium (K) 0.0000% 0 β, γ

For comparison:

  • Banana: ~15 Bq per fruit
  • Granite: 1,000–3,000 Bq/kg
  • EU exemption limit: 10,000 Bq/kg

Note: Risk is shown relative to daily recommended maximum exposure to non-background radiation of 1000 µSv/year. Note that natural background radiation averages around 2400 µSv/year so in reality these risks are probably extremely overstated! With infrequent handling and safe storage natural radioactive minerals do not usually pose much risk.

Interactive Simulator:

Note: The mass selector refers to the mass of radioactive mineral present, not the full specimen, also be aware that the matrix may also be radioactive, possibly more radioactive than this mineral!

Activity:

DistanceDose rateRisk
1 cm
10 cm
1 m

The external dose rate (D) from a radioactive mineral is estimated by summing the gamma radiation contributions from its Uranium, Thorium, and Potassium content, disregarding daughter-product which may have a significant effect in some cases (eg 'pitchblende'). This involves multiplying the activity (A, in Bq) of each element by its specific gamma ray constant (Γ), which accounts for its unique gamma emissions. The total unshielded dose at 1 cm is then scaled by the square of the distance (r, in cm) and multiplied by a shielding factor (μshield). This calculation provides a 'worst-case' or 'maximum risk' estimate because it assumes the sample is a point source and entirely neglects any self-shielding where radiation is absorbed within the mineral itself, meaning actual doses will typically be lower. The resulting dose rate (D) is expressed in microsieverts per hour (μSv/h).

D = ((AU × ΓU) + (ATh × ΓTh) + (AK × ΓK)) / r2 × μshield

Other InformationHide

Notes:
Radioactive
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 SchmitteriteHide

References for SchmitteriteHide

Reference List:

Localities for SchmitteriteHide

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

- 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.
Czech Republic
 
  • Ústí nad Labem Region
    • Teplice District
      • Moldava
Pauliš P. et al. (Kutna Hora, issue 1)
DR Congo
 
  • Haut-Katanga
    • Kambove Territory
      • Shinkolobwe
Deliens (1996)
Mexico
 
  • Sonora
    • Moctezuma Municipality
Lapis 2001 (1)
Gaines (1971)
Lapis 2001 (1)
Thorne (n.d.)
Norway
 
  • Trøndelag
    • Oppdal
      • Gråurdfjellet
Rumsey et al. (2018)
 
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