“…The calculated mean values of <α AE > for 54 common minerals and 650 minerals and synthetic compounds differ by less than 3% from the observed values. Using dynamic polarizabilities, we observed systematic deviations in: (1) M 2+ SO 4 •nH 2 O, blödite (Na 2 M 2+ (SO 4 ) 2 •4H 2 O), and kieserite-related minerals (Gagné et al 2018), (2) fast-ion conductors (Shannon et al, 2019), (3) crystal structures containing corner-shared octahedra such as MTiO 3 (M = Ca, Sr, Ba), KNbO 3 , KTaO 3 , Ba .25 Sr .75 Nb 2 O 6 and KTiOPO 4 , and (4) crystal structures containing edge-shared Fe 3+ , Mn 3+ , Ti 4+ , Mo 6+ , and W 6+ octahedra such as MnWO 4 (hübnerite) (Shannon and Fischer, 2016).…”