The effect of internal pressure on charge-ordered rare earth manganates of the compositionLn
1−x
A
x
MnO3(Ln=La, Pr, Nd andA=Ca, Sr) has been studied by varying the average radius of theAsite cations (〈r
A
〉). Increasing 〈r
A
〉 is generally accompanied by an increase in the ferromagnetic transition temperature and a decrease in the charge-ordering transition temperature. On increasing the size of theAsite cations by appropriate substitution, charge-ordered insulators such as Pr0.7Ca0.3MnO3and Nd0.5Ca0.5MnO3become ferromagnetic, accompanied by an insulator-metal transition. In Pr0.5Sr0.5MnO3, substitution of La in place of Pr destroys the antiferromagnetic transition and favors the ferromagnetic metallic state.
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