Wollastonite

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Wollastonite
General
Category	Silicate mineral
Chemical formula	Calcium silicate, CaSiO3
Identification
Color	white, colorless or gray, monoclinic
Crystal habit	rare tabular crystals - commonly massive in lamellar, radiating, compact and fibrous aggregates.
Crystal system	triclinic bar 1
Cleavage	perfect in two directions at near 90 degrees
Fracture	splintery to uneven
Mohs Scale hardness	4.8
Luster	vitreous or dull to pearly on cleavage surfaces
Refractive index	a=1.628, b=1.639, g=1.642
Streak	White
Specific gravity	2.82
Melting point	1540 °C
Solubility	soluble in HCl, insoluble in water

Wollastonite is a calcium inosilicate mineral (CaSiO₃) that may contain small amounts of iron, magnesium, and manganese substituting for calcium. It is usually white. It forms when impure limestone or dolostone is subjected to high temperature and pressure sometimes in the presence of silica-bearing fluids as in skarns or contact metamorphic rocks. Associated minerals include garnets, vesuvianite, diopside, tremolite, epidote, plagioclase feldspar, Pyroxene and calcite. It is named after the English chemist and mineralogist William Hyde Wollaston (1766-1828).

Some of the properties that make wollastonite so useful are its high brightness and whiteness, low moisture and oil absorption, and low volatile content. Wollastonite is used primarily in ceramics, friction products (brakes and clutches), metalmaking, paint filler, and plastics.

Despite its chemical similarity to the compositional spectrum of the pyroxene group of minerals - where magnesium and iron substitution for calcium ends with diopside and hedenbergite respectively - it is structurally very different, with a third SiO₄ tetrahedron^[1] in the linked chain (as opposed to two in the pyroxenes).

Contents 1 Production trends 2 Uses 3 Composition 4 Geologic Occurrence 5 Structure 6 Physical & Optical Properties 7 See also 8 References

[edit] Production trends

In 2005, China was the top producer of wollastonite with at least 50% world share followed by India and the USA, reports the British Geological Survey.

In the United States, wollastonite is mined in Willsboro, New York and Gouverneur, New York. Deposits have also been mined commercially in North Western Mexico.

[edit] Uses

Wollastonite has industrial importance worldwide. It is used in many industries, mostly by tile factories which have incorporated it into the manufacturing of ceramic to improve many aspects, and this is due to its fluxing properties, freedom from volatile constituents, whiteness, and acicular particle shape(Deer, Howie and Zussman, 1997). It also can be used in paint, paper, and vinyl tile manufacture. In some industries, it is used in different percentages of impurities such as its use as, a fabricator of mineral wool insulation, or as an ornamental building material (Andrews, R. W, 1970).

[edit] Composition

There are two main constituents that form the mineral wollastonite, they are, CaO, and SiO₂. In a pure CaSiO₃, each component forms nearly half of the mineral by weight percentage. The CaO has a weight percentage of 48.3 %, and the SiO₂ has a weight percentage of 51.7%. In some cases, small amounts of iron (Fe), and manganese (Mn), and lesser amounts of magnesium (Mg) substitute for Calcium (Ca) in the mineral molecules (Andrews, R. W, 1970). Wollastonite can form a series of solid solutions in the system CaSiO₃-FeSiO₃, or hydrothermal synthesis of phases in the system MnSiO₃-CaSiO₃ ( Deer, Howie and Zussman, 1997).

[edit] Geologic Occurrence

Wollastonite usually occurs as a common constituent of a thermally metamorphosed impure limestone, it also could occur when the silicon is due to metamorphism in contact altered calcareous sediments, or to contamination in the invading igneous rock. In most of these occurrences it is the result of the reaction: CaCO₃+SiO₂=>CaSiO₃+CO₂ (Deer, Howie and Zussman, 1997). Wollastonite could also develop in a diffusion reaction skarn, it develops when limestone within a sandstone is metamorphosed by a dyke, which results in the formation of wollastonite in the sandstone as a result of outward migration of Ca (Deer, Howie and Zussman, 1997).

[edit] Structure

Wollastonite was once classed structurally among the pyroxene group, because both of these groups have a ratio of Si:O = 1:3. Then came Warren and Biscoe (1931), and showed that the unit cell of wollastonite is different than that in the pyroxene group, and they classified this mineral within a group known as the pyroxenoids (Deer, Howie and Zussman, 1997). It has been shown that the pyroxenoid chains are more kinked than those of pyroxene group, and exhibit longer repeat distance. The structure of wollastonite consist of infinite chains, parallel to the c axis, with a unit repeat of three twisted tetrahedra . The smallest repeat distance of the unit cell in the wollastonite chains is 7.1Å(The manual of mineral science, p 451).

[edit] Physical & Optical Properties

Wollastonite has a triclinic crystal structure, with α=90˚, β=95˚16', γ=103˚22'. It also has bladed crystal masses, and acicular particles shape. Wollastonite usually exhibits a white color, but sometimes cream, grey or very pale green.

The streak of wollastonite is white, and its hardness on mohs' scale ranges between 4.5-5. Its specific gravity ranges between 2.87-3.09. There are more than one cleavage planes for it, there is a perfect cleavage on {100}, good cleavages on {001}, and {¯102}, and an imperfect cleavage on {101}. It is common for wollastonite to have a twin axis [010], a composition plane (100), and rarely to have a twin axis [001]. And the luster is usually vitreous to pearly. The melting point of wollastonite is about 1,540˚C.

[edit] See also

• List of minerals
• List of minerals named after people

[edit] References

• Hurlbut, Cornelius S.; Klein, Cornelis, 1985, Manual of Mineralogy, 20th ed., ISBN 0-471-80580-7
• Mindat
• Webmineral
• Mineral galleries
• Oxford University MSDS sheet
• Andrews, R. W. Wollastonite. London, Her majesty's stationary office, 1970.
• Deer, Howie and Zussman. Rock Forming Minerals; Single Chain Silicates, Vol. 2A, Second Edition, London, The geological society, 1997.
• Klein, Cornelis, and Barbara Dutrow. The Manual of Mineral Science. New York : J. Wiley, c2002.