Abstract
The ferroelectric Sillen-Aurivillius phase Bi 5PbTi 3O 14Cl, a layered structure containing three-layer perovskite-type blocks, has been modified by substituting magnetic transition metal cations M 3+ = Cr 3+, Mn 3+, or Fe 3+ for 1/ 3 of the Ti 4+ cations, accompanied by co-doping of Bi 3+ for Pb 2+. The aim of the modification was to produce naturally layered ferroelectromagnetic compounds. Rietveld refinements against high-temperature synchrotron X-ray powder diffraction data show that the resulting new compounds Bi 6Ti 2MO 14Cl undergo non-centrosymmetric (P2an) to centrosymmetric (P4/mmm) ferroelectric phase transitions for Bi 6Ti 2CrO 14Cl at 974.6(2) K, Bi 6Ti 2MnO 14Cl at 913.5(6) K, and Bi 6Ti 2FeO 14Cl at 1044.8(1) K. Ferroelectric properties were measured on Bi 6Ti 2FeO 14Cl using piezoresponse force microscopy which showed typical ferroelectric hysteresis behavior in the polarization with varying field strength as well as a piezoelectric strain. Combined Rietveld refinements against X-ray and neutron powder diffraction data indicate a statistical 1:2 distribution of M 3+ and Ti 4+ across all three perovskite layers, resulting in highly strained structures (enhancing the ferroelectricity compared to Bi 5PbTi 3O 14Cl) and pronounced spin-glass (cluster glass-type) behavior below T irr(0) = 4.46 K that we have characterized by detailed magnetic susceptibility and heat capacity measurements.
Original language | English |
---|---|
Pages (from-to) | 3932-3942 |
Number of pages | 11 |
Journal | Chemistry of Materials |
Volume | 24 |
Issue number | 20 |
DOIs | |
Publication status | Published - 23 Oct 2012 |