TY - JOUR
T1 - A neutron diffraction investigation into the rhombohedral phases of the perovskite series PbZr1-xTixO3
AU - Corker, D. L.
AU - Glazer, A. M.
AU - Whatmore, R. W.
AU - Stallard, A.
AU - Fauth, F.
PY - 1998/7/20
Y1 - 1998/7/20
N2 - Rietveld refinements using neutron powder profiles are reported for a series of PbZr1-xTxO3 samples (commonly known as PZT), with x ranging from ≈0.12 to ≈0.40. Cation shifts, octahedral distortion and tilts are determined with varying composition across the ferroelectric rhombohedral regions, FR(LT) and FR(HT), of the PZT phase diagram. These parameters are then used in conjunction with a simple Landau-Devonshire model to investigate the nature of the FR(LT)-FR(HT) phase transition. It is found that the cation shifts, octahedral distortion and tilt angles decrease with increasing Ti content, but, surprisingly, the octahedral strain, as indicated by the rhombohedral angle, increases. This is in contrast to the case for all other known rhombohedral perovskites. Furthermore, the refined anisotropic displacement parameters of the cations are anomalous and cannot be accounted for by the average crystal structure. A model is presented in which a domain-type 'local' structure is considered, containing 'ordered' additional cation displacements, consistently with the reports of extra reflections observed in electron microscopy studies by Viehland et al, Dai et al and Ricote et al.
AB - Rietveld refinements using neutron powder profiles are reported for a series of PbZr1-xTxO3 samples (commonly known as PZT), with x ranging from ≈0.12 to ≈0.40. Cation shifts, octahedral distortion and tilts are determined with varying composition across the ferroelectric rhombohedral regions, FR(LT) and FR(HT), of the PZT phase diagram. These parameters are then used in conjunction with a simple Landau-Devonshire model to investigate the nature of the FR(LT)-FR(HT) phase transition. It is found that the cation shifts, octahedral distortion and tilt angles decrease with increasing Ti content, but, surprisingly, the octahedral strain, as indicated by the rhombohedral angle, increases. This is in contrast to the case for all other known rhombohedral perovskites. Furthermore, the refined anisotropic displacement parameters of the cations are anomalous and cannot be accounted for by the average crystal structure. A model is presented in which a domain-type 'local' structure is considered, containing 'ordered' additional cation displacements, consistently with the reports of extra reflections observed in electron microscopy studies by Viehland et al, Dai et al and Ricote et al.
UR - https://www.scopus.com/pages/publications/0032115555
U2 - 10.1088/0953-8984/10/28/007
DO - 10.1088/0953-8984/10/28/007
M3 - Article
AN - SCOPUS:0032115555
SN - 0953-8984
VL - 10
SP - 6251
EP - 6269
JO - Journal of Physics Condensed Matter
JF - Journal of Physics Condensed Matter
IS - 28
ER -