The Chemical Formula of Tourmaline


Tourmaline is not a single mineral, but a group of isomorphous minerals with an identical crystal lattice. Each member of the Tourmaline group has its own chemical formula, due to a slight difference in elemental distribution. The formula of the Tourmaline group is very complex, since it contains many elements and many combinations of elements. It is one of the most complicated chemical formula in the entire mineral kingdom.

A generic formula for the entire Tourmaline group is:
X1 Y3 Al6 B3 Si6 (OH)4
X
= Na and/or Ca
Y
= Mg, Li, Al, and/or Fe2+

This creates the formula:
(Na,Ca) (Mg,Li,Al,Fe2+)3 Al6 B3 Si6 (OH)4


In some rare varieties, the Al may be replaced by other elements. For example, in Uvite, the Al is partially replaced by Mg, and in Chromdravite, it is fully replaced by Cr.

This expands the formula to:
(Na,Ca) (Mg,Li,Al,Fe2+)3 (Al,Mg,Cr)6 B3 Si6 (OH)4


To add to the complexity, the rare member Buergerite contains three O atoms and one F atom in place of the OH radical. A Buergerite molecule also contains an Fe atom that is in a +3 oxidation state.

This expands the formula to:
(Na,Ca) (Mg,Li,Al,Fe2+,Fe3+)3 (Al,Mg,Cr)6 B3 Si6 (OH,O,F)4

Note that there are a few additional forms of Tourmaline that further alter the formula. Those forms are extremely rare and not applicable for this guide.
The formula for Tourmaline can be written in several ways, but it all boils down to the same thing.


The formula of individual members of the Tourmaline group are:

Schorl
Na Fe2+3 Al6 B3 Si6 (OH)4

Dravite

Na Mg3 Al6 B3 Si6 (OH)4

Elbaite

Na (Li,Al)3 Al6 B3 Si6 (OH)4

Liddicoatite

Ca (Li,Al)3 Al6 B3 Si6 (OH)4

Uvite

Ca (Mg,Fe2+)3 Al5 Mg B3 Si6 (OH)4)
(Note that the one Al atom is replaced by a Mg atom)

Chromdravite

Na Mg3 Cr6 B3 Si6 (OH)4
(Note that the Al atoms are replaced by Cr atoms)

Buergerite

Na Fe3+3 Al6 B3 Si6 O3 F
(Note that the OH radical is replaced by three O atoms and one F atom. This leaves a space open for one more positive charge, which is compensated by three Fe+3 atoms (as opposed to Fe with a +2 charge)




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