Gadolinium iron garnet/zirconia (GIG/ZrO2) samples of 1:9 wt. ratio are rea
ction sintered at 1300 degreesC for 8 h and studied by analytical electron
microscopy. The GIG grain was found to transform into a Zr4+-doped hematite
core surrounded by Gd-stabilized cubic-ZrO2 polycrystals shell. The hemati
te core is a single crystal nearly free of Gd3+. Iron zirconate was found t
o precipitate within the hematite core, and it is the same as that first fo
und in the aged alpha -Fe2O3-ZrO2 composite. The size of the iron zirconate
precipitates decrease from core center toward the edge. The probable proce
ss leading to the microstructure and phase changes is discussed. (C) 2001 E
lsevier Science B.V. All rights reserved.