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Rewitzerite

A valid IMA mineral species
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About RewitzeriteHide

Formula:
[K(H2O)]Mn2Al3(PO4)4(OH)2 · 14H2O
Colour:
colorless
Specific Gravity:
2.33 (Calculated)
Crystal System:
Monoclinic
Name:
After Christian Rewitzer (1955 - ), professional German pharmacist from Furth im Wald, Bavaria. Specialist for minerals of Hagendorf and the mineralogy of the Iberian Peninsula. Faculty Member of Ludwig-Maximilians-Universität München, active mineral collector and Mindat user.
The hydroxyl analogue of fluor-rewitzerite. Also related to pleysteinite.

Compare dickinsonite-(KMnNa).


Unique IdentifiersHide

Mindat ID:
470779
Long-form identifier:
mindat:1:1:470779:6

IMA Classification of RewitzeriteHide

Approved
IMA Formula:
K(H2O)Mn2+2(Al2Ti4+)(PO4)4[O(OH)](H2O)10·4H2O
Approval year:
2023
Approval history:
IMA no. 2023-005

Classification of RewitzeriteHide

8.DG.05

8 : PHOSPHATES, ARSENATES, VANADATES
D : Phosphates, etc. with additional anions, with H2O
G : With large and medium-sized cations, (OH, etc.):RO4< 0.5:1

Mineral SymbolsHide

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

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

Physical Properties of RewitzeriteHide

Colour:
Colorless
Density:
2.33 g/cm3 (Calculated)

Optical Data of RewitzeriteHide

Type:
Biaxial (+)
RI values:
nα = 1.585(2) nβ = 1.586(2) nγ = 1.615(2)
2V:
Measured: 25° (2)
Max. Birefringence:
δ = 0.030
Based on recorded range of RI values above.

Interference Colours:
The colours simulate birefringence patterns seen in thin section under crossed polars. They do not take into account mineral colouration or opacity.

Michel-Levy Bar The default colours simulate the birefringence range for a 30 µm thin-section thickness. Adjust the slider to simulate a different thickness.

Grain Simulation You can rotate the grain simulation to show how this range might look as you rotated a sample under crossed polars. Each grain retains its interference colour (retardation) while its brightness falls to black at extinction and reaches a maximum between extinction positions.

Surface Relief:
Moderate
Dispersion:
none
Pleochroism:
Non-pleochroic

Chemistry of RewitzeriteHide

Mindat Formula:
[K(H2O)]Mn2Al3(PO4)4(OH)2 · 14H2O
Element Weights:
Element% weight
O57.763 %
P13.555 %
Mn12.021 %
Al8.856 %
K4.278 %
H3.529 %

Calculated from ideal end-member formula.

Chemical AnalysisHide

Crystallography of RewitzeriteHide

Crystal System:
Monoclinic
Class (H-M):
2/m - Prismatic
Space Group:
P21/b
Setting:
P21/c
Cell Parameters:
a = 10.444(2) Å, b = 20.445(2) Å, c = 12.269(1) Å
β = 90.17(3)°
Ratio:
a:b:c = 0.511 : 1 : 0.6
Unit Cell V:
2,619.76 ų (Calculated from Unit Cell)
Z:
4

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
10.26 Å(53)
7.44 Å(55)
6.16 Å(92)
5.19 Å(40)
3.703 Å(57)
3.111 Å(97)
2.862 Å(100)
2.600 Å(46)
Comments:
collections of (1) the Natural History Museum of Los Angeles County, 900 Exposition Boulevard, Los Angeles, CA 90007, USA, catalogue numbers 76280 (holotype), and (2) the Mineralogical State Collection, Theresienstraße 39, 80333 Munich, Germany, catalogue number MSM38037 (cotype)

Type Occurrence of RewitzeriteHide

General Appearance of Type Material:
clusters of colourless elongated hexagonal-shaped prisms, up to 0.1 mm long
Place of Conservation of Type Material:
The holotype specimen is housed in the mineralogical collections of the Natural History Museum of Los Angeles County, catalogue number 76280. Portions of the original holotype specimen, used for
the initial characterisation using energy-dispersive X-ray analysis, and for the colour images are registered as cotype specimens at the Mineralogical State Collection Munich (SNSB), registration number MSM38037.
Associated Minerals at Type Locality:

Synonyms of RewitzeriteHide

Other Language Names for RewitzeriteHide

Relationship of Rewitzerite to other SpeciesHide

Other Members of Paulkerrite Group:
Benyacarite(H2O)2Mn2Ti2Fe3+(PO4)4(OF)(H2O)10 · 4H2OOrth. mmm(2/m2/m2/m) : Pbca
Bergbauerite(H2O)2Mn2(Fe2Ti)(PO4)4(OH)2(H2O)10 · 4H2OOrth. mmm(2/m2/m2/m) : Pbca
Fluor-rewitzerite[(H2O)K]Mn2(Al2Ti)(PO4)4(OF)(H2O)10 · 4H2OMon. 2/m : P21/b
Fluormacraeite [(H2O)K]Mn2(Fe2Ti)(PO4)4(OF)(H2O)10 · 4H2OMon. 2/m : P21/b
HochleitneriteMn2Ti3(PO4)4O2(H2O)2 · 14H2OOrth. mmm(2/m2/m2/m) : Pbca
Hydroxylbenyacarite(H2O)2Mn2(Ti2Fe)(PO4)4[O(OH)](H2O)10 · 4H2O Orth. mmm(2/m2/m2/m) : Pbca
MacraeiteK(H2O)Mn2(Fe2Ti)(PO4)4[O(OH)](H2O)10 · 4H2OMon. 2/m : P21/b
MantienneiteKMg2Al2Ti(PO4)4(OH)3 · 15H2OOrth. mmm(2/m2/m2/m) : Pbca
PaulkerriteK(Mg,Mn2+)2(Fe3+,Al,Ti,Mg)2Ti(PO4)4(OH)3 · 15H2OMon. m
Pleysteinite[(H2O)0.5K0.5]2Mn2Al3(PO4)4F2 · 14H2OOrth. mmm(2/m2/m2/m) : Pbca
Sperlingite (H2O)K(Mn2+Fe3+)(Al2Ti)(PO4)4[O(OH)] [(H2O)9(OH)] · 4H2OMon. 2/m : P21/b

Related Minerals - Strunz-mindat GroupingHide

8.DG.JasonsmithiteMn2+4ZnAl(PO4)4(OH)(H2O)7 · 3.5H2OMon. 2/m : P21/b
8.DG.Davidbrownite-(NH4)(NH4)5(V4+O)2(C2O4)[PO2.75(OH)1.25]4 · 3H2OMon. 2/m : P21/b
8.DG.Relianceite-(K)K4Mg(V4+O)2(C2O4)(PO3OH)4(H2O)10Mon. m : Pb
8.DG.Pleysteinite[(H2O)0.5K0.5]2Mn2Al3(PO4)4F2 · 14H2OOrth. mmm(2/m2/m2/m) : Pbca
8.DG.05Fluor-rewitzerite[(H2O)K]Mn2(Al2Ti)(PO4)4(OF)(H2O)10 · 4H2OMon. 2/m : P21/b
8.DG.05LavendulanNaCaCu5(AsO4)4Cl · 5H2OMon. 2/m
8.DG.05LemanskiiteNaCaCu5(AsO4)4Cl · 3H2OMon. 2/m : P21/m
8.DG.05SampleiteNaCaCu5(PO4)4Cl · 5H2OOrth. mmm(2/m2/m2/m) : Cmmm
8.DG.05ZdenĕkiteNaPbCu5(AsO4)4Cl · 5H2OMon. 2/m : P21/b
8.DG.10DacostaiteK(Mg2Al)[Mg(H2O)6]2(AsO4)2F6 · 2H2OMon. 2/m : B2/m

RadioactivityHide

Radioactivity:
Element % Content Activity (Bq/kg) Radiation Type
Uranium (U) 0.0000% 0 α, β, γ
Thorium (Th) 0.0000% 0 α, β, γ
Potassium (K) 4.2775% 1,326 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

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 RewitzeriteHide

References for RewitzeriteHide

Localities for RewitzeriteHide

Showing 2 localities.

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.
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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.
Germany
 
  • Bavaria
    • Lower Bavaria
      • Regen District
        • Zwiesel
          • Rabenstein
Grey et al. (2026) +1 other reference
    • Upper Palatinate
      • Neustadt an der Waldnaab District
        • Waidhaus
          • Hagendorf
            • Hagendorf South Pegmatite
Bosi et al. (2023) +1 other reference
 
and/or  
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