
Polaron dynamics
109
7D
2
3
;;;;;
Figure 4.4. A one-dimensional model of a small polaron on the chain interacting with the
ion displacements of another chain.
wide region of the adiabatic parameter ω/T (a) and coupling was calculated with
the continuous-time path-integral quantum Monte Carlo (QMC) algorithm [94].
This method is free from any systematic finite-size, finite-time-step and finite-
temperature errors and allows for an exact (in the QMC sense) calculation of the
ground-state energy and the effective mass of the lattice polaron for any electron–
phonon interaction described by the Hamiltonian (4.51).
At large λ (>1.5), the SFP was found to be much lighter than the SHP, while
the large Fr¨ohlich polaron (i.e. at λ<1) was heavier than the large Holstein
polaron with the same binding energy (figure 4.5). The mass ratio m
∗
FP
/m
∗
HP
is
a non-monotonic function of λ. The effective mass of Fr
¨
ohlich polarons, m
∗
FP
(λ)
is well fitted by a single exponent, which is e
0.73λ
for ω
0
= T (a) and e
1.4λ
for
ω = 0.5T (a). The exponents are remarkably close to those obtained with the
Lang–Firsov transformation, e
0.78λ
and e
1.56λ
, respectively. Hence, in the case
of the Fr¨ohlich interaction the transformation is perfectly accurate even in the
moderate adiabatic regime, ω/T (a) ≤ 1forany coupling strength. This is not the
case for the Holstein polaron. If the interaction is short range, the same analytical
technique is applied only in the non-adiabatic regime ω/T (a)>1.
Another interesting point is that the size of the SFP and the length over which
the distortion spreads are different. In the strong-coupling limit, the polaron is
almost localized on one site m. Hence, the size of its wavefunction is the atomic
size. In contrast, the ion displacements, proportional to the displacement force
f (m − n), spread over a large distance. Their amplitude at a site n falls with
distance as |m − n|
−3
in our one-dimensional model. The polaron cloud (i.e.
lattice distortion) is more extended than the polaron itself [66, 72, 100]. Such a
polaron tunnels with a larger probability than the Holstein polaron due to a smaller
relative lattice distortion around two neighbouring sites. For a short-range e–ph
interaction, the entire lattice deformation disappears at one site and then forms at
its neighbour, when the polaron tunnels from site to site. Therefore, γ = 1and
the polaron is very heavy already at λ ≈ 1. In contrast, if the interaction is long-
ranged, only a fraction of the total deformation changes every time the polaron
tunnels from one site to its neighbour and γ is smaller than 1. The fact that the
Lang–Firsov transformation is rather accurate for the long-range interaction in
a wide region of parameters, allows us to generalize this result. Including all