The
polycrystalline thin films of BiFeO3 (BFO) and Bi0.90Ho0.10Fe1–xTixO
(x = 0, 0.025, 0.05, 0.10, 0.15, and 0.20) were successfully synthesized
by the simple sol–gel method. X-ray diffraction and Raman spectra
revealed the substitution of Bi and Fe by Ho and Ti, respectively,
and correspondingly a structural phase transition from the rhombohedral
phase to orthorhombic phase. The field-emission scanning electron
microscopy and transmission electron microscopy images indicated that
the average size of the particles was decreased and the surface homogeneous
agglomeration was enhanced with the increased concentration of Ti
to x = 0.05. The X-ray photoelectron spectroscopy
measurements illustrated that Fe3+ and O2– ions tended to increase with the Ti concentration increase, which
accounted for the enhanced super-exchange interaction between Fe3+ and O2–. Because of the reduced concentration
of oxygen vacancies, Ho and Ti ions with a smaller ionic radius and
denser surface structure, the Ho and Ti co-substituted films with
an appropriate concentration of Ti (x = 0.05) showed
an optimal saturation magnetization (M
s) of 44.23 emu/cm3 and remanent magnetization (M
r) of 4.62 emu/cm3, which were approximately
1.8 times and 1.9 times than that of the pure BFO, respectively. This
work opened up an effective way to modulate the structure and properties
of BFO-based materials.