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Aluminite

Sulfate mineral


Sulfate mineral

FieldValue
nameAluminite
categorySulfate mineral
imageAluminite - Newhaven, Sussex, England.jpg
imagesize260px
captionAluminite from Newhaven, Sussex, England
formulaAl2SO4(OH)4·7H2O
IMAsymbolA
strunz7.DC.05
systemMonoclinic
classPrismatic (2/m)
(same H-M symbol)
symmetry*P*21/c
unit cella = 7.44, b = 15.583
c = 11.7 [Å]; β = 110.18°; Z = 4
colorWhite to grayish white
habitNeedles and fibrous masses
cleavageNone
fractureIrregular/uneven
tenacityFriable
mohs1 - 2
lusterDull to earthy
streakWhite
diaphaneityTranslucent, opaque if massive
gravity1.66–1.82
opticalpropBiaxial (+)
refractivenα = 1.459 nβ = 1.464 nγ = 1.470
birefringenceδ = 0.011
2VMeasured: 90°, calculated: 86°
references

(same H-M symbol) c = 11.7 [Å]; β = 110.18°; Z = 4 | length fast/slow =

Aluminite is a hydrous aluminium sulfate mineral with formula: Al2SO4(OH)4·7H2O. It is an earthy white to gray-white monoclinic mineral which almost never exhibits crystal form. It forms botryoidal to mammillary clay-like masses. It has a very soft Mohs hardness of 1–2 and a specific gravity of 1.66–1.82.

It forms in clay and lignite deposits as an oxidation product of pyrite and marcasite along with aluminium silicates. It also occurs in volcanic sublimates, in native sulfur deposits and rarely in caves. It occurs in association with basaluminite, gibbsite, epsomite, gypsum, celestine, dolomite and goethite.

It was first described in 1807 from Halle, Saxony-Anhalt, Germany and named for its aluminium content. It is also known as alley stone, halite and websterite (named after Orcadian geologist Thomas Webster).

Aluminite is used by tile and masonry workers to reduce the setting time of mortars.

References

References

  1. Warr, L.N.. (2021). "IMA–CNMNC approved mineral symbols". Mineralogical Magazine.
  2. "Handbook of Mineralogy".
  3. "Mindat w/ locations".
  4. "Webmineral".
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