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Katoite

A valid IMA mineral species
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About KatoiteHide

Formula:
Ca3Al2[◻(OH)4]3
The formula for general "hydrogrossular" is derived by the progressive exchange of grossular's Si with vacancies (◻), while maintaining local charge balance by attaching one H+ to each of the four adjacent oxygens (so 4H+ in total) per each one Si4+ lost. This progressive exchange can also be represented as Ca3Al2(SiO4)3-x(OH)4x. In end-member katoite, the replacement is complete (so x = 3).

Previously, the mineral "hibschite" (no longer an IMA-approved species) was considered an intermediate member of the grossular-katoite series, and was defined as Ca3Al2(SiO4)3-x(OH)4x, where x = 0.2-1.5; compositions where x < 0.2 were still considered grossular, whereas compositions where x > 1.5 were considered katoite. Now, based on the modern "50% rule", what was previously called "hibschite" would now be considered grossular (or perhaps more descriptively as "OH-bearing grossular"), although "hibschite", "hydrogrossular" and "hydrogarnet" are still all informally in common use.
Colour:
Colourless
Lustre:
Vitreous
Hardness:
5 - 6
Specific Gravity:
3.013 (Calculated)
Crystal System:
Isometric
Name:
Named in 1984 by E. Passaglia and R. Rinaldi in honor of Akira Kato (加藤 昭) (b. 19 June 1931, Tokyo prefecture, Japan), Department of Geology, National Science Museum, Ueno, Tokyo, Japan. Former president of the International Mineralogical Association. In addition to his academic positions, Dr Kato was the founder of one of the most active Tokyo clubs for mineral collectors and amateur mineralogists and he was always willing to help amateurs with their studies.
Grossular-Katoite Series. Compare also the tetragonal-pseudocubic Holtstamite.
Ungrouped member of the Garnet Supergroup.

For x = 3, i.e. the end member, the species is also known as C3AH6 ("Tricalcium aluminate hydrate") in hydrated cement.
See also hydrogarnet.

Note that the "hydrogarnet" exchange is not limited to only grossular-rich garnets, and has also been observed involving andradite ("hydro-andradite") and sometimes uvarovite ("hydro-uvarovite") as well. A related exchange, where Si is also replaced by vacancies but the local charge balance is instead maintained by replacing the four adjacent oxygen by fluorine, is particularly notable in some igneous spessartine-rich garnets ("fluor-spessartine"), but occurs in other garnet varieties as well; mixed exchanges (e.g. "fluor-hydro-andradite") are also known.

Katoite from Tadano bears both hexa- and tetravalent sulfur.



Unique IdentifiersHide

Mindat ID:
2167
Long-form identifier:
mindat:1:1:2167:4
GUID
(UUID V4):
40b4f0fb-5606-4003-9e65-86689c0ab3c5

IMA Classification of KatoiteHide

Approved
IMA Formula:
Ca3Al2(OH)12
Approval year:
1982

Classification of KatoiteHide

4.FF.

4 : OXIDES (Hydroxides, V[5,6] vanadates, arsenites, antimonites, bismuthites, sulfites, selenites, tellurites, iodates)
F : Hydroxides (without V or U)
F : Hydroxides with OH, without H2O; various polyhedra
51.4.3d.2

51 : NESOSILICATES Insular SiO4 Groups Only
4 : Insular SiO4 Groups Only with cations in [6] and >[6] coordination
16.9.17

16 : Silicates Containing Aluminum and other Metals
9 : Aluminosilicates of Ca

Mineral SymbolsHide

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

Please only use the official IMA–CNMNC symbol. Older variants are listed for historical use only.

SymbolSourceReference
KtoIMA–CNMNCWarr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43
KtoThe Canadian Mineralogist (2019)The Canadian Mineralogist (2019) The Canadian Mineralogist list of symbols for rock- and ore-forming minerals (December 30, 2019). download

Physical Properties of KatoiteHide

Vitreous
Colour:
Colourless
Streak:
White
Hardness:
5 - 6 on Mohs scale
Density:
3.013(5) g/cm3 (Calculated)

Optical Data of KatoiteHide

Type:
Isotropic

Chemistry of KatoiteHide

Mindat Formula:
Ca3Al2[◻(OH)4]3

The formula for general "hydrogrossular" is derived by the progressive exchange of grossular's Si with vacancies (◻), while maintaining local charge balance by attaching one H+ to each of the four adjacent oxygens (so 4H+ in total) per each one Si4+ lost. This progressive exchange can also be represented as Ca3Al2(SiO4)3-x(OH)4x. In end-member katoite, the replacement is complete (so x = 3).

Previously, the mineral "hibschite" (no longer an IMA-approved species) was considered an intermediate member of the grossular-katoite series, and was defined as Ca3Al2(SiO4)3-x(OH)4x, where x = 0.2-1.5; compositions where x < 0.2 were still considered grossular, whereas compositions where x > 1.5 were considered katoite. Now, based on the modern "50% rule", what was previously called "hibschite" would now be considered grossular (or perhaps more descriptively as "OH-bearing grossular"), although "hibschite", "hydrogrossular" and "hydrogarnet" are still all informally in common use.
Common Impurities:
Mg,S

Chemical AnalysisHide

Empirical formulas:
Sample IDEmpirical Formula
1{Ca3[(Al1.61Fe3+0.21Mg0.06Ti0.02)4+Σ1.90S0.10]Σ2.00(◻1.87Si1.12S6+0.01)Σ3.00[(OH)7.19O4.61F0.15Cl0.05]Σ12.00

Crystallography of KatoiteHide

Crystal System:
Isometric
Class (H-M):
m3m (4/m 3 2/m) - Hexoctahedral
Space Group:
Ia3d
Setting:
Ia3d
Cell Parameters:
a = 12.24095(8) Å
Unit Cell V:
1,834.19 ų (Calculated from Unit Cell)
Z:
8
Comment:
Synthetic katoite has a = 12.5731(2) A (Lager et al., 2002).

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0001827KatoiteLager G A, Von Dreele R B (1996) Neutron powder diffraction study of hydrogarnet to 9.0 GPa American Mineralogist 81 1097-110419960.0001293
0001828KatoiteLager G A, Von Dreele R B (1996) Neutron powder diffraction study of hydrogarnet to 9.0 GPa American Mineralogist 81 1097-110419960.78293
0001829KatoiteLager G A, Von Dreele R B (1996) Neutron powder diffraction study of hydrogarnet to 9.0 GPa American Mineralogist 81 1097-110419963.6293
0001830KatoiteLager G A, Von Dreele R B (1996) Neutron powder diffraction study of hydrogarnet to 9.0 GPa American Mineralogist 81 1097-110419966.1293
0001831KatoiteLager G A, Von Dreele R B (1996) Neutron powder diffraction study of hydrogarnet to 9.0 GPa American Mineralogist 81 1097-110419967.9293
0001832KatoiteLager G A, Von Dreele R B (1996) Neutron powder diffraction study of hydrogarnet to 9.0 GPa American Mineralogist 81 1097-110419969293
0002791KatoiteLager G A, Downs R T, Origlieri M J, Garoutte R (2002) High-pressure single-crystal X-ray diffraction study of katoite hydrogarnet: Evidence for a phase transition from Ia-3d - I-43d symmetry at 5 GPa American Mineralogist 87 642-64720020293
0002792KatoiteLager G A, Downs R T, Origlieri M J, Garoutte R (2002) High-pressure single-crystal X-ray diffraction study of katoite hydrogarnet: Evidence for a phase transition from Ia-3d - I-43d symmetry at 5 GPa American Mineralogist 87 642-64720022.15293
0002793KatoiteLager G A, Downs R T, Origlieri M J, Garoutte R (2002) High-pressure single-crystal X-ray diffraction study of katoite hydrogarnet: Evidence for a phase transition from Ia-3d - I-43d symmetry at 5 GPa American Mineralogist 87 642-64720024.21293
0002794KatoiteLager G A, Downs R T, Origlieri M J, Garoutte R (2002) High-pressure single-crystal X-ray diffraction study of katoite hydrogarnet: Evidence for a phase transition from Ia-3d - I-43d symmetry at 5 GPa American Mineralogist 87 642-64720025.09293
0002795KatoiteLager G A, Downs R T, Origlieri M J, Garoutte R (2002) High-pressure single-crystal X-ray diffraction study of katoite hydrogarnet: Evidence for a phase transition from Ia-3d - I-43d symmetry at 5 GPa American Mineralogist 87 642-64720026293
0002796KatoiteLager G A, Downs R T, Origlieri M J, Garoutte R (2002) High-pressure single-crystal X-ray diffraction study of katoite hydrogarnet: Evidence for a phase transition from Ia-3d - I-43d symmetry at 5 GPa American Mineralogist 87 642-64720026293
0002797KatoiteLager G A, Downs R T, Origlieri M J, Garoutte R (2002) High-pressure single-crystal X-ray diffraction study of katoite hydrogarnet: Evidence for a phase transition from Ia-3d - I-43d symmetry at 5 GPa American Mineralogist 87 642-64720027.09293
0002798KatoiteLager G A, Downs R T, Origlieri M J, Garoutte R (2002) High-pressure single-crystal X-ray diffraction study of katoite hydrogarnet: Evidence for a phase transition from Ia-3d - I-43d symmetry at 5 GPa American Mineralogist 87 642-64720027.78293
0003740KatoiteLager G A, Marshall W G, Liu Z, Downs R T (2005) Re-examination of the hydrogarnet structure at high pressure using neutron powder diffraction and infrared spectroscopy American Mineralogist 90 639-64420050.08293
0003741KatoiteLager G A, Marshall W G, Liu Z, Downs R T (2005) Re-examination of the hydrogarnet structure at high pressure using neutron powder diffraction and infrared spectroscopy American Mineralogist 90 639-64420050.8293
0003742KatoiteLager G A, Marshall W G, Liu Z, Downs R T (2005) Re-examination of the hydrogarnet structure at high pressure using neutron powder diffraction and infrared spectroscopy American Mineralogist 90 639-64420051.72293
0003743KatoiteLager G A, Marshall W G, Liu Z, Downs R T (2005) Re-examination of the hydrogarnet structure at high pressure using neutron powder diffraction and infrared spectroscopy American Mineralogist 90 639-64420052.98293
0003744KatoiteLager G A, Marshall W G, Liu Z, Downs R T (2005) Re-examination of the hydrogarnet structure at high pressure using neutron powder diffraction and infrared spectroscopy American Mineralogist 90 639-64420054.05293
0003745KatoiteLager G A, Marshall W G, Liu Z, Downs R T (2005) Re-examination of the hydrogarnet structure at high pressure using neutron powder diffraction and infrared spectroscopy American Mineralogist 90 639-64420055.4293
0003746KatoiteLager G A, Marshall W G, Liu Z, Downs R T (2005) Re-examination of the hydrogarnet structure at high pressure using neutron powder diffraction and infrared spectroscopy American Mineralogist 90 639-64420056.65293
0003747KatoiteLager G A, Marshall W G, Liu Z, Downs R T (2005) Re-examination of the hydrogarnet structure at high pressure using neutron powder diffraction and infrared spectroscopy American Mineralogist 90 639-64420057.55293
0003748KatoiteLager G A, Marshall W G, Liu Z, Downs R T (2005) Re-examination of the hydrogarnet structure at high pressure using neutron powder diffraction and infrared spectroscopy American Mineralogist 90 639-64420058.56293
0003749KatoiteLager G A, Marshall W G, Liu Z, Downs R T (2005) Re-examination of the hydrogarnet structure at high pressure using neutron powder diffraction and infrared spectroscopy American Mineralogist 90 639-64420059.42293
0006980KatoiteFerro O, Galli E, Papp G, Quartieri S, Szakall S, Vezzalini G (2003) A new occurrence of katoite and re-examination of the hydrogrossular group European Journal of Mineralogy 15 419-42620030200
0006981KatoiteFerro O, Galli E, Papp G, Quartieri S, Szakall S, Vezzalini G (2003) A new occurrence of katoite and re-examination of the hydrogrossular group European Journal of Mineralogy 15 419-42620030200
0016002KatoiteCohen-Addad C, Ducros P, Bertaut E (1967) Etude de la substitution du groupement SiO4 par (OH)4 dans les composes Al2Ca3(OH)12 et Al2Ca3(SiO4)2.16 (OH)3.36 de type grenat _cod_database_code 1008060 Acta Crystallographica 23 220-23019670293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
2.763 Å(100)
2.257 Å(58)
2.004 Å(58)
3.089 Å(50)
5.046 Å(37)
1.6507 Å(37)
3.303 Å(32)
Comments:
Campomorto quarry, Italy. The data are from Passaglia and Rinaldi (1984).

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Stage 3b: Earth’s earliest hydrosphere>4.45
16 : Low-𝑇 aqueous alteration of Hadean subaerial lithologies (see also #23)
Near-surface Processes
22 : Hydration and low-𝑇 subsurface aqueous alteration (see also #23)
Stage 10a: Neoproterozoic oxygenation/terrestrial biosphere<0.6
51 : Pyrometamorphic minerals (see also #54 and #56)<0.36

Type Occurrence of KatoiteHide

Synonyms of KatoiteHide

Other Language Names for KatoiteHide

German:Katoit
Russian:Катоит
Spanish:Katoita

Varieties of KatoiteHide

Relationship of Katoite to other SpeciesHide

Other Members of this group:
Berzeliite GroupX3Z2[TO4]3
Bitikleite GroupCa3Z2[TO4]3
CryolithioniteNa3Al2(LiF4)3Iso. m3m (4/m 3 2/m) : Ia3d
Garnet GroupX3Z2(SiO4)3
Henritermierite GroupCa3Z2(SiO4)2[◻(OH)4]
MonteneveiteCa3Sb5+2(Fe3+2Fe2+)O12Iso. m3m (4/m 3 2/m) : Ia3d
NikmelnikoviteCa12(Fe2+Fe3+3Al3◻)[SiO4]6[◻(OH)4]54Trig. 3 : R3
Priscillagrewite-(Y)(Ca2Y)Zr2(AlO4)3Iso.
Schorlomite GroupCa3Z2[SiO4][TO4]2
UM1984-37-SiO:CrMnMn2+3Cr3+2(SiO4)3
XuiteCa3Fe3+2[(AlO3(OH)]3Iso. m3m (4/m 3 2/m)
YafsoaniteCa3Te6+2(ZnO4)3Iso. m3m (4/m 3 2/m) : Ia3d
Forms a series with:

Common AssociatesHide

Associated Minerals Based on Photo Data:
3 photos of Katoite associated with AfwilliteCa3(HSiO4)2 · 2H2O
1 photo of Katoite associated with MagnetiteFe2+Fe3+2O4
1 photo of Katoite associated with TobermoriteCa4Si6O17(H2O)2 · (Ca · 3H2O)
1 photo of Katoite associated with HydrocalumiteCa4Al2(OH)12(Cl,CO3,OH)2 · 4H2O

Related Minerals - Strunz-mindat GroupingHide

4.FF.05HydroromarchiteSn3O2(OH)2Tet. 4 2m : P4 21c

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 KatoiteHide

References for KatoiteHide

Reference List:

Localities for KatoiteHide

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.
Antarctica
 
  • Eastern Antarctica
    • Victoria Land
      • Ross Archipelago
        • Ross Island
Kammerer (2011)
Germany
 
  • Bavaria
    • Lower Franconia
      • Haßberge District
        • Maroldsweisach
Wittern (2001)
  • Rhineland-Palatinate
    • Mayen-Koblenz
      • Vordereifel
        • Ettringen
Blass et al. (2004)
Galuskin et al. (2016)
Hungary
 
  • Pest County
    • Szentendre District
      • Dunabogdány
Topographia Mineralogica Hungariae VI. +2 other references
  • Veszprém County
    • Tapolca District
      • Uzsa
Israel
 
  • Southern District (HaDarom District)
    • Tamar Regional Council
Galuskin et al. (2015)
Galuskin et al. (2016)
Galuskin +1 other reference
Italy
 
  • Lazio
    • Metropolitan City of Rome Capital
      • Rome
        • Valleranello
Carlini et al. (2018)
    • Viterbo Province
      • Montalto di Castro
        • Pietra Massa Locality
Passaglia et al. (1982)
Japan
 
  • Fukushima Prefecture
    • Koriyama City
      • Tadano
Banno et al. (2023)
Middle East
 
Gross (1977)
Norway
 
  • Telemark
    • Skien
Jamtveit et al. (1997)
Palestine
 
  • West Bank
    • Bethlehem Governorate
Galuskina et al. (2019)
    • Quds Governorate
Galuskin et al. (2015)
Romania
 
  • Caraş-Severin County
    • Prigor
Marincea et al. (2015)
Russia
 
  • Kabardino-Balkaria
    • Baksan Valley
      • Upper Chegem volcanic caldera (Verkhnechegemskaya caldera)
        • Lakargi Mountain
Galuskina et al. (2013)
Slovakia
 
  • Prešov Region
    • Vranov nad Topľou District
      • Vechec
Zajzon N. et al. (2021)
 
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