Z. El-Fadli, E. Coret, F. Sapiña, E. Martinez, A. Beltrán, D. Beltrán and F. Lloret
Single-phase perovskites in the solid solution series La0.85(Na1–xKx)0.15MnO3 (0≤x≤1) have been obtained using a soft treatment, which makes possible strict stoichiometric control. X-Ray powder diffraction patterns of these compounds have been completely indexed with a rhombohedral perovskite cell. The crystal structures have been refined in space group R-3c, in the hexagonal setting, from room-temperature data. Substitution of Na+ by larger K+ ions produces a cell expansion and a decrease in the structural distortion from the ideal cubic structure. The critical temperature for the paramagnetic-ferromagnetic transition, Tc, is found to be practically constant, ca. 333 K, along the entire series. This behaviour is unexpected, taking into account previous correlations established for the alkaline-earth La0.7(Ca1–xSrx)0.3MnO3 series (Tc increases with the mean size of cations at the A positions, 〈rA〉) which expands over a similar 〈rA〉 range. We can therefore discuss these results in terms of two counterweighting contributions: increasing Tc values could be expected as a consequence of the increase with x of the 〈rA〉 value, but the concomitant disorder introduced at the A positions [as represented by the variance of the A cations radial distribution, σ2(〈rA〉)] would cause a decrease in Tc. An approach to the understanding of the contribution that the electronic energy makes to this last effect is advanced.