TY - JOUR
T1 - Structural Change Caused by Substitution of Nd for Sm in (Nd, Sm)AlO3
T2 - Application of Synchrotron High-Resolution Powder X-ray Diffraction
AU - Saitow, Akihiro
AU - Yoshikawa, Akira
AU - Horiuchi, Hiroyuki
AU - Shishido, Toetsu
AU - Fukuda, Tsuguo
AU - Tanaka, Masahiko
AU - Mori, Takeharu
AU - Sasaki, Satoshi
PY - 1998/10
Y1 - 1998/10
N2 - Structural change caused by substitution of Nd for Sm in perovskite (Nd, Sm)AlO3 was analysed by application of high-resolution powder X-ray diffraction using synchrotron radiation. The parallel, well monochromated and bright incident X-rays improved the full width at half-maximum (FWHM) to 0.027° in a wide 2θ range for the standard Si powder. Applying this high-resolution optical system, the lattice parameters of the solid solution (Ndx, Sm1-x)AlO3 were precisely analysed for the phases from x = 0.0 to 1.0 with an interval of 0.2. The lattice parameters of a series of RAlO3 vary system-atically with the average ionic radii of R3+, accompanying a structural change from orthorhombic to a trigonal system at around R3+ = 1.11 Å corresponding to average ionic radii of 0.7Nd3+ + 0.3Sm3+. In orthorhombic phases, deformation of the crystal lattice from its ideal cubic lattice is minimized at around x = 0.0-0.2 in (Ndx, Sm1-x)AlO3 and increased with increasing average ionic radii of Nd3+ and Sm3+. The structure changes from orthorhombic to trigonal at around x = 0.7.
AB - Structural change caused by substitution of Nd for Sm in perovskite (Nd, Sm)AlO3 was analysed by application of high-resolution powder X-ray diffraction using synchrotron radiation. The parallel, well monochromated and bright incident X-rays improved the full width at half-maximum (FWHM) to 0.027° in a wide 2θ range for the standard Si powder. Applying this high-resolution optical system, the lattice parameters of the solid solution (Ndx, Sm1-x)AlO3 were precisely analysed for the phases from x = 0.0 to 1.0 with an interval of 0.2. The lattice parameters of a series of RAlO3 vary system-atically with the average ionic radii of R3+, accompanying a structural change from orthorhombic to a trigonal system at around R3+ = 1.11 Å corresponding to average ionic radii of 0.7Nd3+ + 0.3Sm3+. In orthorhombic phases, deformation of the crystal lattice from its ideal cubic lattice is minimized at around x = 0.0-0.2 in (Ndx, Sm1-x)AlO3 and increased with increasing average ionic radii of Nd3+ and Sm3+. The structure changes from orthorhombic to trigonal at around x = 0.7.
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U2 - 10.1107/S0021889898001629
DO - 10.1107/S0021889898001629
M3 - Article
AN - SCOPUS:0000262647
SN - 0021-8898
VL - 31
SP - 663
EP - 671
JO - Journal of Applied Crystallography
JF - Journal of Applied Crystallography
IS - 5
ER -