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Carobbiite

A valid IMA mineral species - grandfathered
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About CarobbiiteHide

03107910017271921924701.jpg
Guido Carobbi
Formula:
KF
Colour:
Colourless
Hardness:
2 - 2½
Specific Gravity:
2.505
Crystal System:
Isometric
Member of:
Name:
Named by Hugo Strunz in 1956 in honor of Guido Carobbi (20 October 1900, Pistoia, Tuscany, Italy - 16 January 1983, Florence, Tuscany, Italy), Professor at the Institute of Mineralogy and Geochemistry, University of Florence. Carobbi (1936 and 1940) twice described the new mineral potassium fluoride, but he did not name it. Carobbi found KF in some yellowish stalactites collected on February 7, 1934 at the bottom of Vesuvius crater in a lava cave of the Dec. 1933 intracrater effusion, located in the NE quarter. The mineral was described as tiny colorless cubic crystals in association with erythrosiderite, hieratite, and mercallite.
Very rare water-soluble fluoride mineral. Poisonous!
The K analogue of villiaumite.


Unique IdentifiersHide

Mindat ID:
908
Long-form identifier:
mindat:1:1:908:9

IMA Classification of CarobbiiteHide

Approved, 'Grandfathered' (first described prior to 1959)
First published:
1936

Classification of CarobbiiteHide

3.AA.20

3 : HALIDES
A : Simple halides, without H2O
A : M:X = 1:1, 2:3, 3:5, etc.
9.1.1.4

9 : NORMAL HALIDES
1 : AX
8.1.5

8 : Halides - Fluorides, Chlorides, Bromides and Iodides; also Fluoborates and Fluosilicates
1 : Halides of the alkali metals and ammonium

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

Physical Properties of CarobbiiteHide

Transparency:
Translucent
Colour:
Colourless
Hardness:
2 - 2½ on Mohs scale
Cleavage:
Distinct/Good
On {001}.
Density:
2.505 g/cm3 (Measured)    2.528 g/cm3 (Calculated)

Optical Data of CarobbiiteHide

Type:
Isotropic
RI values:
n = 1.362
Surface Relief:
Very High (negative)
Relative to Canada balsam mounting medium (n ≈ 1.537).

This shows the grain boundary and Becke line effect under plane-polarised light, based on the contrast between this mineral's average refractive index and the mounting medium. It does not take into account mineral colouration.
In focus

Chemistry of CarobbiiteHide

Mindat Formula:
KF
Element Weights:
Element% weight
K67.299 %
F32.701 %

Calculated from ideal end-member formula.
K
F

Crystallography of CarobbiiteHide

Crystal System:
Isometric
Class (H-M):
m3m(4/m32/m) - Hexoctahedral
Space Group:
Fm3m
Setting:
Fm3m
Cell Parameters:
a = 5.34 Å
Unit Cell V:
152.27 ų (Calculated from Unit Cell)
Z:
4

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0011330CarobbiiteWyckoff R W G (1963) Second edition. Interscience Publishers, New York, New York rocksalt structure Crystal Structures 1 85-23719630293
0017895CarobbiiteBroch E, Oftedal I, Pabst A (1929) Neubestimmung der Gitterkonstanten von KF, CsCl und BaF2 _cod_database_code 1010978 Zeitschrift fur Physikalische Chemie 3 209-21419290293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
2.675 Å(100)
1.8913 Å(45)
3.088 Å(21)
1.5443 Å(10)
1.1959 Å(7)
1.6125 Å(6)
1.3370 Å(4)
Comments:
Synthetic

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Stage 7: Great Oxidation Event<2.4
45b : [Other oxidized fumarolic minerals]
Stage 10a: Neoproterozoic oxygenation/terrestrial biosphere<0.6
50 : Coal and/or oil shale minerals<0.36
Stage 10b: Anthropogenic minerals<10 Ka
54 : Coal and other mine fire minerals (see also #51 and #56)

Type Occurrence of CarobbiiteHide

General Appearance of Type Material:
As minute cubic crystals, intermixed with other minerals
Place of Conservation of Type Material:
University of Florence, Florence, Italy, 1972/l.
Geological Setting of Type Material:
stalactites in cavities in lava.
Associated Minerals at Type Locality:

Synonyms of CarobbiiteHide

Other Language Names for CarobbiiteHide

Relationship of Carobbiite to other SpeciesHide

Member of:
Other Members of Halite Group:
GriceiteLiFIso. m3m(4/m32/m) : Fm3m
HaliteNaClIso. m3m(4/m32/m) : Fm3m
SylviteKClIso. m3m(4/m32/m) : Fm3m
VilliaumiteNaFIso. m3m(4/m32/m) : Fd3m

Related Minerals - Strunz-mindat GroupingHide

3.AA.Brontesite(NH4)3PbCl5Orth. mmm(2/m2/m2/m) : Pnma
3.AA.05MarshiteCuIIso. 43m : F43m
3.AA.05NantokiteCuClIso. 43m : F43m
3.AA.05'UM1999-11:I:CuS'Cu(I,S)
3.AA.05Miersite(Ag,Cu)IIso. 43m : F43m
3.AA.10Tocornalite(Ag,Hg)I (?)Hex.
3.AA.10IodargyriteAgIHex. 6mm : P6mm
3.AA.15BromargyriteAgBrIso. m3m(4/m32/m) : Fm3m
3.AA.15ChlorargyriteAgClIso. m3m(4/m32/m) : Fm3m
3.AA.20SylviteKClIso. m3m(4/m32/m) : Fm3m
3.AA.20HaliteNaClIso. m3m(4/m32/m) : Fm3m
3.AA.20VilliaumiteNaFIso. m3m(4/m32/m) : Fd3m
3.AA.20GriceiteLiFIso. m3m(4/m32/m) : Fm3m
3.AA.25'UM1998-03-Cl:Tl'TlCl
3.AA.25NataliyamalikiteTlIOrth. mmm(2/m2/m2/m) : Cmcm
3.AA.25LafossaiteTl(Cl,Br)Iso. m3m(4/m32/m) : Pm3m
3.AA.25SalammoniacNH4ClIso. m3m(4/m32/m)
3.AA.30Calomel[Hg2]2+Cl2Tet. 4/mmm(4/m2/m2/m) : I4/mmm
3.AA.30Moschelite[Hg2]2+I2Tet. 4/mmm(4/m2/m2/m) : I4/mmm
3.AA.30KuzminiteHgBrTet. 4/mmm(4/m2/m2/m) : I4/mmm
3.AA.35NeighboriteNaMgF3Orth. mmm(2/m2/m2/m)
3.AA.35ParascandolaiteKMgF3Iso. m3m(4/m32/m) : Pm3m
3.AA.40JavorieiteKFeCl3Orth. mmm(2/m2/m2/m) : Pnma
3.AA.40ChlorocalciteKCaCl3Orth. mmm(2/m2/m2/m) : Pnma
3.AA.45KolaritePbTeCl2Orth.
3.AA.50RadhakrishnaitePbTe3(Cl,S)2Tet.
3.AA.55ChallacolloiteKPb2Cl5Mon. 2/m : P21/b
3.AA.60HephaistositeTlPb2Cl5Mon. 2/m : P21/b
3.AA.90PseudocotunniteK2PbCl4Orth.

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) 67.2987% 20,863 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:
Easily soluble in water.
Health Risks:
Although the mineral is not known to occur in sufficient natural abundances to be considered hazardous, be aware that the synthetic compound KF is poisonous (as are other water-soluble fluoride compounds such as NaF, occurring in nature as the mineral villiaumite) if ingested, inhaled or absorbed through the skin. However, lethal doses approach gram levels for humans. As is always good practice, minerals should be considered as chemicals, and so treated accordingly.

Internet Links for CarobbiiteHide

References for CarobbiiteHide

Localities for CarobbiiteHide

Showing 6 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.
Costa Rica
 
  • Alajuela Province
    • Sarchí Canton
Rodríguez et al. (2017)
Italy (TL)
 
  • Campania
    • Metropolitan City of Naples
[Russo et al. (2004)
Rend.Soc.Min.Ital. (1956) +1 other reference
Japan
 
  • Hokkaidō Prefecture
    • Iburi Subprefecture
      • Usu District
Oana (1962) +1 other reference
Poland
 
  • Silesian Voivodeship
    • Wodzisław County
Ł. Kruszewski (PXRD data) +1 other reference
Ł. Kruszewski PXRD data (to be published soon) +3 other references
 
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