“…A key feature of these apatite oxide ion conductors is that their conduction mechanism is driven by the presence of interstitial oxide ions, contrary to the traditional fluorite and perovskite systems, where oxide ion vacancies are responsible [13]. For the silicates it has been shown that oxygen excess in the range, 0 ≤ x ≤ 0.5 is possible, while higher oxygen content, 0 ≤ x ≤ 1.0 has been achieved for the germanates [13,18,20,21]. For the silicate series, the exact location of extrastoichiometric oxygen, x, has attracted some controversy, with reports of interstitial sites close to the SiO4 tetrahedra, while in other studies, mobile oxygen at the centre of the channels has been claimed [4,8,9,10,12,13,23,27,35,36].…”