Chemistry:Hureaulite

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Hureaulite
Hureaulite 01.jpg
Hureaulite from the Cigana Claim, Conselheiro Pena, Minas Gerais, Brazil. Specimen size 2.8 cm.
General
CategoryPhosphate minerals
Formula
(repeating unit)
Mn2+
5
(PO
3
OH)
2
(PO
4
)
2
 · 4H2O
Strunz classification8.CB.10 (10 ed)
7/C.04-10 (8 ed)
Dana classification39.2.1.1
Crystal systemMonoclinic
Crystal classPrismatic (2/m)
(same H-M symbol)
Space groupC2/c
Unit cella = 17.594(10) Å
b = 9.086(5) Å
c = 9.404(5) Å
β = 96.67(8)°; Z = 4
Identification
Formula mass728.65 g/mol
ColourOrange, red, yellow, brown, grey or nearly colourless
Crystal habitCrystals are short prismatic parallel to (100) or equant, sometimes thick tabular, also massive or imperfectly fibrous[1]
Cleavage{100} good
FractureUneven
TenacityBrittle
Mohs scale hardness3.5
Vitreous to greasy|re|er}}Vitreous to greasy
StreakNearly white
DiaphaneityTransparent to translucent
Specific gravity3.18–3.2 (measured), 3.23 (calculated)
Optical propertiesBiaxial (−)
Refractive indexnα = 1.640 – 1.654 nβ = 1.649 – 1.659 nγ = 1.655 – 1.662
Birefringenceδ = 0.012
PleochroismX colourless, Y yellow to pale rose, Z reddish yellow to reddish brown
2V anglegreater than 60°
Dispersionr<v, very strong[2]
SolubilityEasily soluble in acids.
References[2][3][4][5]

Hureaulite is a manganese phosphate with the formula Mn2+
5
(PO
3
OH)
2
(PO
4
)
2
 · 4H2O
. It was discovered in 1825 and named in 1826 for the type locality, Les Hureaux, Saint-Sylvestre, Haute-Vienne, Limousin, France . It is sometimes written as huréaulite, but the IMA does not recommend this for English language text.[7]

A complete series exists from lithiophilite, LiMn2+PO
4
to triphylite, LiFe2+PO
4
, including hureaulite, strengite, FePO
4
 · 2H2O
, stewartite, Mn2+Fe3+
2
(OH,PO
4
)
2
 · 8H2O
, and sicklerite, (LiMn2+,Fe3+)PO
4
.[8]

Environment

Hureaulite is a secondary mineral occurring in granite pegmatites.[5] At the type locality it occurs in a zone of altered triphylite, LiMn2+PO
4
, in pegmatite. Typically occurs very late in the sequence of formation of secondary phosphate minerals.[9] Associated at the type locality with vivianite, Fe2+
3
(PO
4
)
2
 · 8H2O
; rockbridgeite, Fe2+Fe3+
4
(PO
4
)
3
(OH)
5
; heterosite, (Fe3+,Mn3+)PO
4
and cacoxenite, Fe3+
24
AlO
6
(PO
4
)
17
(OH)
12
 · 17H2O
. It can be synthesised;[10] most natural hureaulites are Mn-rich compounds but extensive (Mn,Fe) solution is known for synthetic material.[9]

Localities

The type locality is Les Hureaux, Saint-Sylvestre, Haute-Vienne, Limousin, France . Hureaulite is also found in a granite pegmatite known for its phosphates in the Aimorés pegmatite district, at the Cigana claim in Galiléia, Doce valley, Minas Gerais, Brazil , formerly known as the Jocão Mine.[3]

References

  1. Murdoch, Joseph (1942) Contributions to the Crystallography of Hureaulite. American Mineralogist 27: 228
  2. 2.0 2.1 Gaines et al (1997) Dana's New Mineralogy Eighth Edition
  3. 3.0 3.1 http://www.mindat.org/min-1952.html Mindat.org
  4. Shigley and Brown (1985) American Mineralogist 70:395
  5. 5.0 5.1 Roberts, Campbell and Rapp (1990) Encyclopedia of Minerals, 2nd edition
  6. Warr, L.N. (2021). "IMA–CNMNC approved mineral symbols". Mineralogical Magazine 85 (3): 291–320. doi:10.1180/mgm.2021.43. Bibcode2021MinM...85..291W. https://www.cambridge.org/core/journals/mineralogical-magazine/article/imacnmnc-approved-mineral-symbols/62311F45ED37831D78603C6E6B25EE0A. 
  7. Burke, E. A. J. (2008): Tidying up Mineral Names: An IMA scheme for Suffixes, Hyphens and Diacritical Marks. Mineralogical Record, 39, 134
  8. Murdoch, Joseph (1943) Crystallography of Hureaulite. American Mineralogist 28: 19-24
  9. 9.0 9.1 Moore, P B, and Araki, T (1973) Hureaulite: its atomic arrangement. American Mineralogist 58: 302-307.
  10. Gerault, Y, Riou, A, and Cudennec, Y (1987) Acta Crystallographica (C) 43:1829