Aurivillius structured Bi6Ti3Fe1.5Mn0.5O18 (B6TFMO) has emerged as a
rare room
temperature multiferroic, exhibiting reversible magnetoelectric switching
of ferroelectric domains under cycled magnetic fields. This layered
oxide presents exceptional avenues for advancing data storage technologies
owing to its distinctive ferroelectric and ferrimagnetic characteristics.
Despite its immense potential, a comprehensive understanding of the
underlying mechanisms driving multiferroic behavior remains elusive.
Herein, we employ atomic resolution electron microscopy to elucidate
the interplay of octahedral tilting and atomic-level structural distortions
within B6TFMO, associating these phenomena with functional properties.
Fundamental electronic features at varying bonding environments within
this complex system are scrutinized using electron energy loss spectroscopy
(EELS), revealing that the electronic nature of the Ti4+ cations within perovskite BO6 octahedra is influenced
by position within the Aurivillius structure. Layer-by-layer EELS
analysis shows an ascending crystal field splitting (Δ) trend
from outer to center perovskite layers, with an average increase in
Δ of 0.13 ± 0.06 eV. Density functional theory calculations,
supported by atomic resolution polarization vector mapping of B-site
cations, underscore the correlation between the evolving nature of
Ti4+ cations, the extent of tetragonal distortion and ferroelectric
behavior. Integrated differential phase contrast imaging unveils the
position of light oxygen atoms in B6TFMO for the first time, exposing
an escalating degree of octahedral tilting toward the center layers,
which competes with the magnitude of BO6 tetragonal distortion.
The observed octahedral tilting, influenced by B-site cation arrangement,
is deemed crucial for juxtaposing magnetic cations and establishing
long-range ferrimagnetic order in multiferroic B6TFMO.