TY - JOUR
T1 - Cation partitioning in Mg0.70Fe0.23Al1.97O4 synthetic spinels by in situ neutron powder diffraction
AU - Artioli, G.
AU - Pavese, A.
AU - Levy, D.
AU - Russo, U.
AU - Hoser, A.
PY - 1998
Y1 - 1998
N2 - Neutron powder diffraction experiments in the temperature range 300-1770 K were performed at BENSC, Berlin, Germany, on synthetic Mg4.70Fe0.23;Al1.97O4. The cation partitioning over the crystallographic tetrahedral and octahedral sites was determined as a function of temperature through joint Rietveld refinements and advanced minimization techniques. The thermal expansion coefficients of the lattice parameter and inter-atomic bond lengths were also obtained from the full-profile structural refinements. The behaviour of the polyhedral bond-lengths, especially the T-O distances, and of the cell constant upon heating, clearly indicate that the interdiffusion of tetrahedral and octahedral Mg/Al cations starts at about 947 K. This result is straightforwardly supported by the direct analysis of the neutron site scattering factors: Fe always retains tetrahedral coordination at all temperatures, and the cation rearrangement is entirely due to Mg and Al intracrystalline diffusion.
AB - Neutron powder diffraction experiments in the temperature range 300-1770 K were performed at BENSC, Berlin, Germany, on synthetic Mg4.70Fe0.23;Al1.97O4. The cation partitioning over the crystallographic tetrahedral and octahedral sites was determined as a function of temperature through joint Rietveld refinements and advanced minimization techniques. The thermal expansion coefficients of the lattice parameter and inter-atomic bond lengths were also obtained from the full-profile structural refinements. The behaviour of the polyhedral bond-lengths, especially the T-O distances, and of the cell constant upon heating, clearly indicate that the interdiffusion of tetrahedral and octahedral Mg/Al cations starts at about 947 K. This result is straightforwardly supported by the direct analysis of the neutron site scattering factors: Fe always retains tetrahedral coordination at all temperatures, and the cation rearrangement is entirely due to Mg and Al intracrystalline diffusion.
KW - Cation Partitioning
KW - High Temperature
KW - Neutron Powder Diffraction
KW - Spinel
UR - http://www.scopus.com/inward/record.url?scp=0031633759&partnerID=8YFLogxK
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AN - SCOPUS:0031633759
SN - 0255-5476
VL - 278-281
SP - 692
EP - 697
JO - Materials Science Forum
JF - Materials Science Forum
IS - PART 2
ER -