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EntityQ422316· pop 10· linked from 5 articles

Also known as bilinite

Bílinite (Fe2+Fe23+(SO4)4·22H2O) is an iron sulfate mineral. It is a product of the oxidation of pyrite in water. It is an acidic mineral that has a pH of less than 3 and is harmful to the environment when it comes from acid rock drainage (Keith et al., 2001).

Key facts

Mineral.name
Bílinite
Mineral.category
Sulfate mineral
Mineral.image
Bilinite.jpg
Mineral.formula
Fe2+Fe3+2(SO4)4·22H2O
Mineral.IMAsymbol
Bli
Mineral.strunz
7.CB.85
Mineral.dana
29.07.03.05
Mineral.system
Monoclinic
Mineral.class
Prismatic (2/m) (same H-M symbol)
Mineral.symmetry
P21/c
Mineral.color
White to yellowish
Mineral.habit
Fibrous in radial aggregates
Mineral.mohs
2
Mineral.luster
Vitreous - silky
Mineral.streak
White
Mineral.diaphaneity
Semitransparent
Mineral.gravity
1.87
Mineral.opticalprop
Biaxial (+/-)

via Wikipedia infobox

Wikidata facts

Image
Bilinite.jpg
Show 5 more facts
Nickel-Strunz 9th edition (updated 2009)
7.CB.85
IMA Mineral Symbol
Bli
Commons category
Bílinite
Strunz 8th edition (series ID, updated)
VI/C.06
Nickel-Strunz '10th ed', review of (9th ed/ 2009 update)
7.CB.85
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Article

4 sections
Contents
  • Composition
  • Related minerals
  • Special characteristics
  • References

Bílinite (Fe2+Fe23+(SO4)4·22H2O) is an iron sulfate mineral. It is a product of the oxidation of pyrite in water. It is an acidic mineral that has a pH of less than 3 and is harmful to the environment when it comes from acid rock drainage (Keith et al., 2001).

Bílinite was first discovered near Bílina, Czech Republic which is why the mineral was named 'bílinite' (Palache, et al., 1969). This mineral possibly occurs on Mars.

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