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Silicate radical is( SiO4) and its valency is -4
Yes, each silicate mineral group is defined by its unique silicate structure. For example, the structure of feldspar group minerals is based on interconnected silica tetrahedra, while the structure of pyroxene group minerals is made up of single chains of silica tetrahedra.
The valency of the silicate ion is -4, meaning it has a charge of -4. This is because the silicate ion is made up of one silicon atom (which has a valency of +4) and four oxygen atoms (each with a valency of -2).
Silicate has an oxidation state of -4 because the silicon atom in silicate typically exhibits a valence of +4, while each oxygen atom has a valence of -2. To maintain electrical neutrality, the overall oxidation state of silicate is -4.
The charge of a silicate ion is typically -4. This is because silicon generally has a 4+ charge, and it bonds with oxygen atoms which each have a 2- charge. This results in a net charge of -4 for the silicate ion.
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== == Yes.
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