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Brookite information


Brookite
Brookite from Balochistan
General
CategoryOxide minerals
Formula
(repeating unit)
TiO2
Strunz classification4.DD.10 (10 ed)
4/D.15-10 (8 ed)
Dana classification4.4.5.1
Crystal systemOrthorhombic
Crystal classDipyramidal (mmm)
H-M symbol: (2/m 2/m 2/m)
Space groupPbca
Unit cella = 5.4558 Å,
b = 9.1819 Å,
c = 5.1429 Å; Z = 8
Identification
Formula mass79.88 g/mol[1]
ColorDeep red, reddish brown, yellowish brown, brown, or black
Crystal habitTabular and striated, pyramidal or pseudohexagonal
TwinningOn {120}, uncertain
CleavagePoor on {120}, in traces on {001}
FractureSubconchoidal to irregular
TenacityBrittle
Mohs scale hardness5+12 to 6
LusterSubmetallic
StreakWhite, greyish or yellowish
DiaphaneityOpaque to translucent
Specific gravity4.08 to 4.18
Optical propertiesBiaxial (+)
Refractive indexnα = 2.583 nβ = 2.584 nγ = 2.700
Birefringenceδ = 0.117
PleochroismVery weak, yellowish, reddish, orange to brown
2V angleCalculated: 12° to 20°
Dispersion0.131 (compare to diamond at 0.044)
Ultraviolet fluorescenceNon-fluorescent
References[1][2][3][4]

Brookite is the orthorhombic variant of titanium dioxide (TiO2), which occurs in four known natural polymorphic forms (minerals with the same composition but different structure). The other three of these forms are akaogiite (monoclinic), anatase (tetragonal) and rutile (tetragonal). Brookite is rare compared to anatase and rutile and, like these forms, it exhibits photocatalytic activity.[5] Brookite also has a larger cell volume than either anatase or rutile, with 8 TiO2 groups per unit cell, compared with 4 for anatase and 2 for rutile.[6] Iron (Fe), tantalum (Ta) and niobium (Nb) are common impurities in brookite.[3]

Brookite was named in 1825 by French mineralogist Armand Lévy[3] for Henry James Brooke (1771–1857), an English crystallographer, mineralogist and wool trader.[1]

Arkansite is a variety of brookite from Magnet Cove, Arkansas, US. It is also found in the Murun Massif on the Olyokma-Chara Plateau of Eastern Siberia, Russia, part of the Aldan Shield.[7]

At temperatures above about 750 °C, brookite will revert to the rutile structure.[8]

  1. ^ a b c Brookite. Webmineral.com. Retrieved on 2011-10-14.
  2. ^ Gaines et al (1997) Dana’s New Mineralogy Eighth Edition. Wiley
  3. ^ a b c Brookite. Mindat.org (2011-09-17). Retrieved on 2011-10-14.
  4. ^ Brookite. Handbook of Mineralogy. (PDF) . Retrieved on 2011-10-14.
  5. ^ Di Paola, A; Addamo, M.; Bellardita, M.; Cazzanelli, E.; Palmisano, L. (2007). "Preparation of photocatalytic brookite thin films". Thin Solid Films. 515 (7–8): 3527–3529. Bibcode:2007TSF...515.3527D. doi:10.1016/j.tsf.2006.10.114.
  6. ^ Anatase and Brookite Archived 2012-03-17 at the Wayback Machine. Wikis.lib.ncsu.edu (2007-05-08). Retrieved on 2011-10-14.
  7. ^ Arkansite on Mindat
  8. ^ Brookite (Titanium Oxide). Galleries.com. Retrieved on 2011-10-14.

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Rarer polymorphs of TiO2 are known, including anatase, akaogiite, and brookite. Rutile has one of the highest refractive indices at visible wavelengths...

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dioxide (TiO2). It is a high-pressure polymorph of TiO2, along with anatase, brookite and another high-pressure phase called "TiO2 II". Rutile is the stable...

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other rare and unusual minerals occur in the area of the shield, such as brookite, frankamenite, tausonite and yuksporite. Akitkan Arctica List of shields...

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name is from Greek ψευδής, for false, and brookite because of its misleading similar appearance to brookite. Pseudobrookite forms as pneumatolytic deposition...

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group minerals, quartz, zircon, certain feldspars, analcime, anatase, brookite, rutile, siderite and apatite. Xenotime is also known to be diagenetic:...

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Armalcolite

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