trioctahedral structure
Quick Summary
In chemistry, "trioctahedral" describes a structure where all three available octahedrally coordinated positions are occupied. This term is particularly relevant in the context of clay minerals, specifically the serpentine group. In these minerals, the general structural formula involves cations in an octahedral sheet. For trioctahedral species, these cations are typically magnesium, iron, manganese, or nickel. Examples of trioctahedral clay minerals include chrysotile, antigorite, and lizardite, all with the formula Mg3Si2O5(OH)4. The arrangement and fit between the tetrahedral and octahedral sheets influence the morphology of these minerals.12
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