Some ions may have a distinct preference on the octahedral site which is dependent on the d-electron count.

There are five distinct octahedral sites and two different tetrahedral sites.

The octahedral sites form chains along the b axis by sharing opposite edges (Allman and Donnay, 1973).

Within an octahedral sheet, there are three octahedral sites in a unit structure; however, not all of the sites may be occupied.

X-ray diffraction analyzed cations sharing on octahedral sites.

The Fe species will occupy some of the octahedral sites and there will only be Fe at the tetrahedral sites.

Hydrogen to nickel atomic ratios are up to one, with hydrogen occupying an octahedral site.

The rock salt structure [2] is generated by filling all octahedral sites with cations in an oxygen anion fcc array.

There are three distinct octahedral sites, M1, M2, and M3, and a single tetrahedral site.

The cations occupy two different octahedral sites which are M1 and M2 and form ionic bonds with the silicate anions.