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Brookite

Another Homologous Mineral of Titanium Dioxide
Bantase is titania Another kind of isomorphic mineral. Chemical composition: TiO two , containing 59.95% titanium. Orthorhombic system. It is trihedral with rutile and anatase. The crystals are plate and leaf shaped. Light yellow, brown to black, streaked light yellow, light gray to brown, transparent or translucent, Adamantine luster Or semi metallic luster.
Bantase mainly occurs in the Alpine vein in metamorphic rocks, but also in hydrothermal alteration, contact metamorphism and placer ores.
Chinese name
Brookite
Foreign name
Brookite
Profile
The crystals are plate shaped, light yellow, brown to black
Crystal system
Orthorhombic system
Density
3.9~4.1g/cm3
Composition
Mainly titanium dioxide
Purpose
Titanium extraction

brief introduction

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refine titanium Of Mineral raw materials titania Another kind of Homomorphism Minerals. Chemical composition: TiO two It contains 59.95% titanium. Orthorhombic system It is formed with rutile and anatase Homomorphic triad The crystals are plate and leaf shaped. Pale yellow, brown to black. Stripes are light yellow, light gray to brown. transparent or translucent Adamantine luster or Semi metallic luster Mohs hardness 5.6~6。 density 3.9~4.1g/cm three Produced in Regional metamorphic rock In quartz vein, or as igneous rock Of Accessory mineral , sometimes in contact Metamorphic rock Medium, also sedimentary rock One of Rock forming mineral Alpine type mainly occurring in metamorphic rocks Lode , also seen in Hydrothermal alteration Contact metamorphism Function and placer Medium. The famous places of origin are U.S.A Magnet cove, Arkansas Switzerland Tirol, Urals of Russia, Brazil, Britain, etc. Transparent semitransparent crystal, because of high dispersion and strong fire, the color of a few bright red crystals is better than Ruby Some light yellow ones can be used as Diamonds Substitutes. [1]

Bantase TiO2

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Crystal chemical properties

Bantase Orthorhombic system In the crystal structure of brookite, O forms distorted four layers most closely Stacking , layer parallel to (100) crystal plane, Ti in octahedral void , each [TiO six ]The octahedron has three edges and angles with the surrounding three [TiO six ]Octahedron share, these shared edges and corners are shorter than other edges and corners, Ti slightly deviates from the center of the octahedron, forming a distorted octahedron. [TiO six ]The octahedron is parallel to the c-axis to form a zigzag chain, and the chain and the chain are connected in parallel (100) to form a layer.

chemical property

The molecular formula of brookite is also the same as that of rutile, and the chemical formula is TiO two Ti 59.95%,O 40.05%。 The composition contains a small amount of Fe 3+ , sometimes Fe two O three Up to 4.5%; Containing a small amount of Nb two O five And Ta two O five Only plate crystals are distinguished from rutile and anatase. In the composition, Ti can be 3+ 、Nb 5+ 、Ta 5+ Replace. Those rich in Fe are called iron plate titanium ore, and those rich in Nb are called niobium plate titanium ore.

physical property

The brookite crystal is in the shape of plate and blade. The color is light yellow, brown to black. Stripes are light yellow, light gray to brown. Transparent or translucent. Diamond luster or semi metallic luster. Mohs hardness is 5.6~6. Density 3.9~4.1g/cm three

optical properties

It is yellowish brown, golden brown or reddish brown in the thin section, with Abnormal interference color , very high protuberance. Biaxial crystal (positive gloss), parallel extinction. High refractive index: n p =2.583,n m =2.584~2.586,n g =2.700~2.741,n g - n p =0.117~0.156, weak polychromaticity, n g : bright yellow, light greenish brown, n m : bright yellow, orange brown, n p : colorless, olive, yellow brown. Under the reflected light, the slate in the light sheet is gray, and the unique growth cone can be distinguished according to the darker color.

Optical characteristics

Yellowish brown, reddish brown or brownish black; Yellow brown or golden brown in thin slices. Polychromatic weak n p - orange, light yellowish brown, n m - orange purple brown, n g A lemon yellow, purple brown. Absorption: n g > n m >n p Or n m >n g >n p Positive pole high protrusion. The roughness is very significant. The interference color is high white, and sometimes abnormal interference color can be seen, so that no real extinction can be seen anywhere. Bicrystal along (120) plane. indicatrix dispersion Extremely strong, cross axial dispersion. For red light and yellow light, the optical axis plane is parallel to (001), and the role dispersion of the optical axis is r<v; For blue light and green light, the optical axis plane is parallel to (010), and the role dispersion of the optical axis is r>v; For yellow green light, the optical axis angle is 0 °.
Optical orientation and 2V vary with temperature. When the optical axis plane is parallel to (001) under the illumination of a fixed wavelength light source, the temperature decreases and 2V decreases; When the optical axis plane is parallel to (010), the temperature decreases and 2V increases. [2]

Genetic occurrence

Bantase is a hydrothermal mineral, coexisting with quartz, albite, sphene, rutile, anatase, etc., which forms later than rutile and earlier than anatase. Bantase is stable under natural conditions and is common in ores. [3]

XRD Diagram of Bantase

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X-ray diffraction pattern
Spectrum description:
Crystal system: rhombic, space group: Pcan, Z: 8
Cell parameter: a zero =0.5448,b zero =0.9184,c zero =0.5144
Radiation condition: CoK α
Source of atlas: Materials Research and Testing Center of Wuhan University of Technology

Transformation of brookite

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Change: When the temperature is about 700 ℃, the content of Bantasite can be changed to rutile
Identification characteristics: special optical property, extremely high refractive index and birefringence, and extremely strong dispersion are excellent identification characteristics of brookite. Rutile has good cleavage And prismatic shape; The refractive index of ferrotitanium (Pseudoarkansasite) is low, the optical axis angle is large, and there is no significant dispersion; Goethite is reddish brown and has negative light property, which is different from that of brookite and can be distinguished. [2]