Rare-earth orthochromites, RCrO
3 (R = rare-earth and Y) with magnetic R-ions are reported to exhibit ferroelectricity at the magnetic ordering temperature of Cr
3+-ions (Rajeswaran, B.; Khomskii, D. I.; Zvezdin, A. K.; Sundaresan, A.; Rao, C. N. R.
arXiv2012,
1201, 0826v1 ). Interestingly, we observe ferroelectricity at the N茅el temperature of orthochromites containing a nonmagnetic R-ion (Y) upon introducing cation-disorder at the Cr-site by incorporation of another magnetic ion of nonequivalent spin. For example, the weakly ferromagnetic perovskite, YCr
0.5Fe
0.5O
3, where the Cr
3+ (
S = 3/2) and Fe
3+ (
S = 5/2) ions at the B-site are disordered, exhibits ferroelectricity at
TN = 260 K. Ferroelectricity is observed not only when the relative proportions of Fe
3+ and Cr
3+ ions as in YCr
1鈥?i>xFe
xO
3 are varied but also when Y
3+ ions are replaced by other nonmagnetic R-ion and the transition metal ions changed as in YCr
1鈥?i>xMn
xO
3. While the local polarization cancels out in the weakly ferromagnetic YMO
3 (M = Cr and Fe), a nonzero polarization in these materials seem to arise due to disordered transition metal ions of nonequivalent spins.
Keywords:
ferroelectricity; cation disorder; weak ferromagnetism; multiferroics; orthochromites