The effect of isotope substitution on the electrical resistance, magneticsusceptibility and neutron diffraction patterns of nearly half-dopedR1−xSrxMnO3 manganites was studied for ceramic samples withR = Sm (x = 0.425–0.525),Nd/Tb (x = 0.45)and Nd/Eu (x = 0.45). In Nd/Tb and Nd/Eu manganites, the composition was chosen to yield the same mean ionicradius as in the Sm compound, but the samples differed in the cation disorder parameterσ. The oxygen isotope substitution leads to fundamental changes in the phase diagram of themanganites studied, favouring enhanced inhomogeneity, stabilizing the insulatingantiferromagnetic (AFM) state and even causing a metal–insulator transition (MIT). TheMIT induced by the oxygen isotope substitution was found here for the first time inmanganites with A-type AFM; earlier this unusual phenomenon was observed only forcompounds with the CE-type AFM structure. This suggests that such a MIT is closelyrelated to the ferro–AFM crossover independently on the specific nature of the AFM phaseand related orbital order.
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