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Brookite is the orthorhombic variant of (TiO2), which occurs in four known natural polymorphic forms (minerals with the same composition but different structure). The other three of these forms are (monoclinic), (tetragonal) and (tetragonal). Brookite is rare compared to anatase and rutile and, like these forms, it exhibits activity. 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. Anatase and Brookite . Wikis.lib.ncsu.edu (2007-05-08). Retrieved on 2011-10-14. (Fe), (Ta) and (Nb) are common impurities in brookite.

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

Arkansite is a variety of brookite from Magnet Cove, Arkansas, US. It is also found in the on the Olyokma-Chara Plateau of Eastern , Russia, part of the . Arkansite on Mindat

At temperatures above about 750 °C, brookite will revert to the rutile structure. Brookite (Titanium Oxide). Galleries.com. Retrieved on 2011-10-14.


Unit cell
Brookite belongs to the orthorhombic dipyramidal crystal class 2/m 2/m 2/m (also designated mmm). The is Pcab and the unit cell parameters are a = 5.4558 Å, b = 9.1819 Å and c = 5.1429 Å. The is TiO2, with 8 formula units per unit cell.


Structure
The brookite structure is built up of distorted with a at the center and ions at each of the six vertices. Each octahedron shares three edges with adjoining octahedra, forming an orthorhombic structure. The Crystal Structure of Brookite. paulingblog.wordpress.com. 12 January 2010


Appearance
Brookite crystals are typically tabular, elongated and striated parallel to their length. They may also be pyramidal, pseudo- or prismatic. Brookite and may grow together in an relationship.

Brookite is usually brown in color, sometimes yellowish or reddish brown, or even black. Beautiful, deep red crystals (seen above-right) similar to and garnet are also known. Brookite displays a submetallic luster. It is opaque to translucent, transparent in thin fragments and yellowish brown to dark brown in transmitted light.


Optical properties
Brookite is , as are all orthorhombic minerals, and it is . are very high, above 2.5, which is even higher than at 2.42. For comparison, ordinary window glass has a refractive index of about 1.5.

Brookite exhibits very weak , yellowish, reddish and orange to brown. It is neither nor radioactive.


Physical properties
Brookite is a mineral, with a subconchoidal to irregular fracture and poor cleavage in one direction parallel to the c crystal axis and traces of cleavage in a direction perpendicular to both the a and the b crystal axes. is uncertain. The mineral has a of to 6, between and . This is the same hardness as anatase and a little less than that of rutile (6 to ). The is 4.08 to 4.18, between that of anatase at 3.9 and rutile at 4.2.


Occurrence and associations
Brookite is an accessory mineral in alpine veins in and ; it is also a common detrital mineral. Associated minerals include its polymorphs and , and also , , , , , and .

The type locality is Twll Maen Grisial, Fron Olau, , , . In 2004, brookite crystals were found in the , in , Pakistan.


See also
  • List of minerals
  • List of minerals recognized by the International Mineralogical Association
  • List of minerals named after people


External links

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