Chrysotile Structure, Clays And Asbestos Sheet Silicates

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Chrysotile is a fibrous mineral that belongs to the serpentine mineral group. As such it is distinct from other asbestiform minerals in the amphibole group. There is a large variety of asbestos minerals but the most important is chrysotile which represents more than 90 of the asbestos used.
chrysotile structure

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The structure of chrysotile.

Large coloring pages to print. The given formula however represents only the ratio of the components and a more exact formula would be mg 3 si 2 o 5oh 4. Witittater technical division ferodo ltd chapel enlefrith stoclcport england received 15 april 1953 it has been shown in a previous communication whit taker 1951 that there exist two varieties of chrysotile of which the better known form is monoclinic and the. Chrysotile mg3si2h4o9 or h4mg3o9si2 cid 25477 structure chemical names physical and chemical properties classification patents literature biological.

It is a hydrated magnesium silicate 3mgo2sio 2 2h 2 o. Chrysotile or white asbestos is the most commonly encountered form of asbestos accounting for approximately 95 of the asbestos in the united states and a similar proportion in other countries. All serpentine group minerals share the same chemical composition mg 3 si 2 o 5 oh 4 but they have different crystal structureschrysotile is the only one among them with a fibrous habit.

It is a soft fibrous silicate mineral in the serpentine subgroup of phyllosilicates. Other members of the group are lizardite and antigorite.

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Chrysotile Structure, Clays And Asbestos Sheet Silicates

The structure of chrysotile.

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