“… 13 In addition, the crystallographic visualization also helps to distinguish these two structures based on occupancy of Wyckoff positions by cations and anions in three different ways, 14 (i) the A and B -site cations in pyrochlore structure occupy 16 c and 16 d sites, respectively while in the fluorite structure both A and B -site cations occupy a single 4 a site, (ii) the oxygen anions in pyrochlore structure lie at 48 f site with coordinates ( x , 1/8,1/8) while in fluorite structure, it lies at 8 c site with coordinates (1/4,1/4,1/4), and (iii) the oxygen anion which lies at 8 b site in pyrochlore structure moves to 4 a site in fluorite structure. 15 Due to these differences, the A and B -site cations are surrounded by 8 and 6 anions, respectively, in pyrochlore structure which transforms to an average of 7 coordinates in fluorite structure. This structural flexibility of AB O-type materials makes them prominent to be utilized in photoluminescence, anti-erosion applications, thermal barrier coating, magnetic devices, nuclear waste management, electrical device, gas sensors, and high-temperature catalysts.…”