Abstract

Single-phase perovskites in the solid solution series La 0.85 (Na 1– x K x ) 0.15 MnO 3 (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, T c , 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 La 0.7 (Ca 1– x Sr x ) 0.3 MnO 3 series (T c increases with the mean size of cations at the A positions, 〈r A 〉) which expands over a similar 〈r A 〉 range. We can therefore discuss these results in terms of two counterweighting contributions: increasing T c values could be expected as a consequence of the increase with x of the 〈r A 〉 value, but the concomitant disorder introduced at the A positions [as represented by the variance of the A cations radial distribution, σ 2 (〈r A 〉)] would cause a decrease in T c . An approach to the understanding of the contribution that the electronic energy makes to this last effect is advanced.

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