The first theories devoted to the lattice dynamics in ferroelectric perovskites can be traced back to Cochran (1961) [
5], where he introduces a shell model description for ferroelectrics to account for the electronic polarizability of the ions, i.e. they are not describable as rigid ions but the relative displacements of their electronic shells with respect to the core have to be included. By using the adiabatic principle, the electronic and ionic degrees of freedom are decoupled, and the renormalized ionic model be considered in deeper detail. In view of the discovery that in perovskite oxides the ferroelectric phase transition is accompanied by the softening of an optic mode, the model explicitly considers anharmonicity by introducing a fourth order term in the lattice dynamical Hamiltonian [
6,
7]. The linear T dependence of the squared soft optic mode is obtained within the self-consistent phonon approximation (SPA) where the fourth order term is replaced by its cumulant expansion [
8]. However, a closer look at the temperature evolution of ω
2 reveals that such simple dependence is not realized, neither in the limit of ω
2→0 nor at T>>T
C , where saturation of ω
2 is observed [
9]. In the limit ω
2→0 very apparent deviations from the above law are commonly seen in quantum paraelectrics like e.g. SrTiO
3 [
10] where saturation of the soft mode takes place due to quantum fluctuations which are larger than the original soft mode which is related to the displacement coordinates. Both temperature regimes have been successfully described within the polarizability model [
11] where an anisotropic core-shell coupling at the oxygen ion is explicitly incorporated [
12,
13]. With respect to the rigid A ion in ABO
3 this coupling is purely harmonic. Regarding the B ion the coupling consists of an attractive harmonic term g
2 and a stabilizing anharmonic fourth order term g
4 which within the SPA is replaced by a temperature dependent pseudo-harmonic approximation, namely:
where
is the relative core-shell displacement coordinate at the oxygen ion lattice site. The Hamiltonian of the polarizability model is given by
where
are the displacement coordinates of ion
mi (i=1, 2) and shell
m1 in the n-th unit cell and
,
f and
f’ are nearest and second nearest neighbour harmonic coupling constants. Within this approach the lowest transverse optic and acoustic modes are well described as a function of momentum q and temperature T, where the latter is obtained through the SPA. The soft transverse q=0 optic mode is explicitly given by:
, with
being the reduced cell mass. While the conventional approach attains the linear in T behaviour [
9] for any temperature, this equation reproduces the quantum paraelectric behaviour as well as the saturation limit due to the T-dependence of the denominator. [Explicit consequences for quantum extensions to phase transitions were discussed in [
2]] An interesting feature appears in the limit when optic and acoustic modes start to couple, which happens as function of temperature and momentum [
14,
15,
16]. In such a case a critical momentum q
c can be defined where both modes are closest to each other. Its value moves to q=0 with decreasing temperature and defines real space regions which are identified with elastic anomalies and polar nanoregions. Both grow in size when approaching the phase transition temperature T
C to finally coalesce to a true global polar state. The onset temperature for their formation does not coincide with a Burn’s temperature T
B [
17], which is notoriously difficult to determine experimentally, but occurs well below estimated values of T
B. A precursor temperature is defined where the crossover between the high temperature saturation and the pre-transitional softening occurs. This temperature was predicted as T*≈1.1T
C. [
18]. Other values, which are in the same order magnitude, stem from Molecular Dynamics simulations [
19] and been discussed in MSB (between 1.01 T
c and 1.4 T
c). These temperatures have been observed experimentally in many perovskite oxides by Brillouin scattering [
20], dielectric spectroscopy [
21], birefringence [
22], ultrasound, RUS of elastic softening [
23,
24,
25,
26] and various other techniques. Importantly, it demonstrates that a nominally displacive system always carries an order-disorder component and thereby indicates a coexistence of both classification classes [
18,
27]. As is evident from equ. 1c a local double-well potential is inherently present in perovskite oxides which stems from the oxygen ion nonlinear polarizability which diverges as a function of its volume and is temperature dependent [
28,
29].