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Francoanellite

A valid IMA mineral species
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About FrancoanelliteHide

00552300017271923248346.jpg
Franco Anelli
Formula:
K3Al5(PO3OH)6(PO4)2 · 12H2O
Colour:
Yellowish white
Hardness:
1 - 2
Specific Gravity:
2.26
Crystal System:
Trigonal
Name:
Named for Franco Anelli (18 October 1899, Lodi, Lombardy, Italy - 23 October 1977, Bari, Apulia, Italy), professor of geography and speleologist, University of Bari, Italy, who discovered the Castellana Caves in which the mineral was found.
Can be considered as a partially dehydrated taranakite.


Unique IdentifiersHide

Mindat ID:
1593
Long-form identifier:
mindat:1:1:1593:2

IMA Classification of FrancoanelliteHide

Classification of FrancoanelliteHide

8.CH.25

8 : PHOSPHATES, ARSENATES, VANADATES
C : Phosphates without additional anions, with H2O
H : With large and medium-sized cations, RO4:H2O < 1:1
39.3.5.2

39 : HYDRATED ACID PHOSPHATES,ARSENATES AND VANADATES
3 : Miscellaneous
19.8.8

19 : Phosphates
8 : Phosphates of Al and other metals

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

Physical Properties of FrancoanelliteHide

Transparency:
Translucent
Colour:
Yellowish white
Streak:
White
Hardness:
1 - 2 on Mohs scale
Comment:
soft
Tenacity:
Waxy
Density:
2.26(2) g/cm3 (Measured)    2.295 g/cm3 (Calculated)

Optical Data of FrancoanelliteHide

Type:
Uniaxial (+)
RI values:
nω = 1.510(2) nε = 1.515(2)
Max. Birefringence:
δ = 0.005
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

Chemistry of FrancoanelliteHide

Mindat Formula:
K3Al5(PO3OH)6(PO4)2 · 12H2O
Element Weights:
Element% weight
O57.039 %
P20.077 %
Al10.931 %
K9.504 %
H2.450 %

Calculated from ideal end-member formula.

Crystallography of FrancoanelliteHide

Crystal System:
Trigonal
Cell Parameters:
a = 8.71 Å, c = 82.5 Å
Ratio:
a:c = 1 : 9.472
Unit Cell V:
5,420.27 ų (Calculated from Unit Cell)
Z:
6
Comment:
Point Group: 3 2/m or 3m Space Group: R3c or R3c (synthetic).

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0015844FrancoanelliteDick S, Zeiske T (1998) Francoanellit K3Al5(HPO4)6(PO4)2*12H2O: struktur und synthese durch topochemische entwasserung von taranakit Zeitschrift fur Naturforschung B53 711-7191998synthetic0293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
13.83 Å(100)
3.40 Å(65)
2.799 Å(62)
7.44 Å(60)
2.773 Å(51)
6.86 Å(50)
5.57 Å(37)

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Stage 7: Great Oxidation Event<2.4
47a : [Near-surface hydration of prior minerals]
47c : [Carbonates, phosphates, borates, nitrates]
Stage 10a: Neoproterozoic oxygenation/terrestrial biosphere<0.6
52 : Guano- and urine-derived minerals<0.4

Type Occurrence of FrancoanelliteHide

Place of Conservation of Type Material:
Mineralogical Museum, University of Bari, Bari, Italy.
National School of Mines, Paris, France.
Geological Setting of Type Material:
Limestone cave.
Associated Minerals at Type Locality:

Synonyms of FrancoanelliteHide

Other Language Names for FrancoanelliteHide

Related Minerals - Strunz-mindat GroupingHide

8.CH.05Natrowalentaite[Fe3+0.5Na0.5(H2O)6][NaAs3+2(Fe3+2.33W6+0.67)(PO4)2O7]Orth. mmm(2/m2/m2/m) : Imma
8.CH.05Walentaite[Mn2+(H2O)6][◻As3+3Fe3+3(PO4)2O7]Orth. mmm(2/m2/m2/m) : Imma
8.CH.05Halilsarpite[Mg(H2O)6][CaAs3+2(Fe3+2.67Mo6+0.33)(AsO4)2O7]Orth. mmm(2/m2/m2/m) : Imma
8.CH.10AnapaiteCa2Fe2+(PO4)2 · 4H2OTric. 1 : P1
8.CH.15PicropharmacoliteCa4Mg(AsO4)2(HAsO4)2 · 11H2OTric. 1 : P1
8.CH.20Dittmarite(NH4)Mg(PO4) · H2OOrth. mm2 : Pmn21
8.CH.20Niahite(NH4)Mn2+(PO4) · H2OOrth. mm2 : Pmn21
8.CH.25TaranakiteK3Al5(PO3OH)6(PO4)2 · 18H2OTrig. 3m(32/m) : R3c
8.CH.25Macivorite(NH4)3Al5(PO3OH)6(PO4)2 · 18H2OTrig. 3m(32/m) : R3c
8.CH.30Schertelite(NH4)2MgH2(PO4)2 · 4H2OOrth. mmm(2/m2/m2/m) : Pbca
8.CH.35Hannayite(NH4)2Mg3H4(PO4)4 · 8H2OTric. 1 : P1
8.CH.40HazeniteKNaMg2(PO4)2 · 14H2OOrth. mmm(2/m2/m2/m)
8.CH.40Struvite-(K)KMg(PO4) · 6H2OOrth. mm2 : Pmn21
8.CH.40Struvite(NH4)Mg(PO4) · 6H2OOrth. mm2 : Pmn21
8.CH.45Rimkorolgite(Mg,Mn)5(Ba,Sr,Ca)(PO4)4 · 8H2OOrth.
8.CH.50BakhchisaraitseviteNa2Mg5(PO4)4 · 7H2OMon. 2/m : P21/b
8.CH.55SmolyaninoviteCo3Fe3+2(AsO4)4 · 11H2OOrth.
8.CH.55FahleiteCaZn5Fe3+2(AsO4)6 · 14H2OOrth.
8.CH.60Barahonaite-(Fe)(Ca,Cu,Na,Fe3+,Al)12Fe3+2(AsO4)8(OH,Cl)x · nH2OMon. 2/m : P2/b
8.CH.60Barahonaite-(Al)(Ca,Cu,Na,Fe3+,Al)12Al2(AsO4)8(OH,Cl)x · nH2OMon. 2/m : P2/b
8.CH.70EpifanoviteNaCaCu5(PO4)4[AsO2(OH)2] · 7H2OMon. 2/m : P21/m
8.CH.75Esdanaite-(Ce)NaMnCe(PO4)2 · 4H2OOrth. 222 : P212121

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) 9.5037% 2,946 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 FrancoanelliteHide

References for FrancoanelliteHide

Localities for FrancoanelliteHide

Showing 12 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.
Australia
 
  • Australian Capital Territory
    • Paddy's River District
McQueen et al. (1988)
      • Paddy's River Mine
McQueen +3 other references
Brazil
 
  • Pará
    • Parauapebas
      • Carajás iron complex
        • N4WS Pit
Piló et al. (2023)
Iran
 
  • Kurdistan Province
    • Divandarreh County
Amin et al. (2022)
Italy (TL)
 
  • Apulia
    • Metropolitan City of Bari
      • Castellana Grotte
Balenzano et al. (1976)
      • Polignano a Mare
Balenzano et al. (1979) +1 other reference
    • Taranto Province
      • Martina Franca
Dell'Anna et al. (1989)
  • Friuli Venezia Giulia
    • Gorizia Province
      • Sagrado
        • San Martino del Carso
Cancian (1984)
Romania
 
  • Constanța County
Dumitras D et al. (2004)
  • Mehedinti County
    • Dubova
Marincea et al. (2004)
  • Sălaj County
    • Ileanda
      • Răstoci
Onac et al. (2003)
South Korea
 
  • Gangwon Province
    • Yeongwol County
Jun +4 other references
 
and/or  
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