“…Niobates and tantalates in the A O− A 2 ′O− M 2 O 5 − system ( A = Ca 2+ , Sr 2+ , Ba 2+ ; A ′ = Li + , Na + , Rb + ; M = Nb 5+ /Nb 4+ , Ta 5+ /Ta 4+ ) commonly crystallize in the perovskite or perovskite-related structure types, including Ca 2 A′M 3 O 10 ( A′ = Li + , Na + , K + , Rb + , Cs + , NH 4 + , Tl + ; M = Nb 5+ , Ta 5+ ), − Ca 2 A′ 2 Ta 3 O 10 ( A′ = Li, Na), Li 2 x Ca 0.5− x TaO 3 , Li 0.2 (Ca 1− y Sr y ) 0.4 TaO 3 , Ca 4 NaNb 5 O 17 , , Ca 2 Na 2 Nb 4 O 13 , , Sr x Na 1− x NbO 3 , Ba 4 LiM 3 O 12 , − and A 3 Na M O 6 ( M = Nb, Ta), , as well as in less commonly observed structure types including Ruddlesden−Popper-related compounds (Li 4 Sr 3 Nb 6 O 20 , Li 2 SrNb 2 O 7 ), anion-deficient pyrochlores (SrNaNb 2 O 6.5 ), rock salt structures (Ca 2 Na 3 TaO 6 ), and tetragonal tungsten bronzes (Ba 2 NaNb 5 O 15 ) . In almost all cases, polycrystalline samples of these oxides were synthesized by the traditional solid-state or ion-exchange methods, ,, while single crystals were obtained from sulfate and carbonate fluxes .…”