1. Introduction
The subject of a charge moving when coupled to a lattice vibration has a long history [
1,
2]. This phenomenon is very different from Ohmic conductivity in metals and semiconductors, where electrons in the conduction band or holes in the valence band move freely within a crystal. In insulators, where all the bands are either occupied or empty, but also in metals and semiconductors, an extra charge outside the bands may be attached to some atom or ion and have a low probability of moving to another position. The deformation it produces in the lattice can travel, and is known as a polaron [
3,
4,
5]. The charge—electron, or hole—changes its position to the same state in a neighboring atom. Polarons were first conceived as either a static solution or coupled to phonons, which were set in motion by an external electric field, but there are other possibilities as explained below. There is a probability that a charge may change to the neighboring site due to the overlapping of the electron wavefunctions in each atom, described by the transfer integral. It is clear that if the distance between atoms decreases, there will be an increase in the transition probability, and vice versa. Even for a symmetric vibration, the increase in the transition probability is much larger for shorter distances than the other way around, leading to an exponential dependence on the change in the potential barrier [
6].
The level of description in which an electron or hole can be ascribed to a single atom is called the tight-binding approximation. It allows for a semiclassical treatment, in which the heavier atoms are described classically and the much lighter electron is described as a quantum particle. A system can be described in terms of the atomic states, and the quantum Hamiltonian is expressed in terms of the energies of these states and the transfer matrices; the latter often depend on the distance exponentially.
Large displacements of the atoms or ions in a crystal imply that the linear description is no longer valid. This nonlinearity may lead to the apparition of localized entities or, when traveling, solitary waves. Notable examples at the macroscopic scale are tsunamis, which travel thousands of kilometers at jet speed in a different manner to usual sea waves. Only slightly less impressive are tidal bores, solitary waves that travel upriver when the incoming tide encounters the outcoming one. Moreover, rogue waves in the sea appearing apparently from nowhere have been proven to exist by systematic satellite observations.
These solitary waves can be kinks, solitons [
7,
8], or breathers, also called intrinsic localized modes [
9,
10,
11]. Solitons and kinks have a constant profile in the moving frame, where solitons become zero at
, while kinks only at one of
, and tend to a constant at the other infinity. Breathers also have a vibrating profile. Sometimes the distinction depends on the variables used. Important steps in breather theory were the mathematical proof of their existence [
12,
13] and Floquet and band theory for breathers [
14,
15,
16], which later expanded to dark breathers [
17,
18] and multibreathers [
19,
20]. They have been obtained with classical molecular dynamics [
21,
22] and ab initio molecular dynamics [
23,
24]. Recently, the spectral theory of exact moving breathers was developed, showing that breathers admit a very simple description in their moving frame, where they have usually a single frequency [
25,
26]. On the one hand, this makes possible the interpretation of numerical spectra, and on the other, it facilitates the integration methods.
The large displacements bringing neighboring atoms closer and increasing the probability of charge transfer between atoms in semiclassical systems lead to a strong coupling between charge and vibrations. The combined entities are called polarobreathers [
27,
28,
29], or solectrons in some systems [
30,
31]. The mathematical methods are often within the Born–Oppenheimer approximation [
32], that is, supposing that the electrons are always in an equilibrium state with the configuration of atoms around them, due to their dynamics being much faster than the dynamics of the atoms. The authors have overcome this limitation by developing efficient numerical methods for semiclassical systems, based on splitting methods that conserve the charge probability at each step of time integration [
33]. On the experimental side of polarobreathers, it was recently discovered that by bombarding layered silicates and other materials with alpha particles, it was possible to measure electrical currents in the absence of an electric field; the electrons or holes were carried by nonlinear lattice excitations [
34,
35].
The purpose of this paper is to apply the theory of exact polarobreathers in their moving frame to a semiclassical system, using numerical integration methods developed in Ref. [
33]. In this way, we clarify the polarobreather spectra, facilitate their description, develop the mathematical methods for obtaining numerically exact polarobreathers, and compare their spectra with the approximate ones. The results can help to identify bands in the spectra of some materials where nonlinear vibrations couple to nonfree charges. The lattice part of the model without the charge is given by a Frenkel–Kontorova model [
36,
37] with the Lennard-Jones interaction potential, because it has been proven extremely good for producing long-lived breathers in two-dimensional systems [
38,
39].
The layout of the article is as follows.
Section 2 presents the semiclassical system and its transformation into a Hamiltonian one.
Section 3 deals with an important problem of the charge description: that the charge frequencies are not an observable of the system. In
Section 4, a review of the theory of exact traveling excitations is presented. The linearization of the system is performed in
Section 5. Very useful calculations, known as tail analysis, which advance many properties of nonlinear excitations, are presented in
Section 6 and
Section 7 for stationary and moving polarobreathers, respectively. In
Section 8, the developed numerical methods to solve dynamical equations and obtain exact polarobreathers are described.
Section 9 and
Section 10 analyze stationary and moving polarobreathers, respectively, following a similar pattern: generation, description of the spectrum of approximate polarobreathers, obtainment of exact solutions and interpretation of their spectra, stability analysis, and path continuation. The article ends with the conclusions.
2. The Model
We consider a model of
N particles, atoms or ions, with a classical and a quantum Hamiltonian imposing periodic boundary conditions. The classical Hamiltonian is given by
In this equation, the variable
is the separation of the particle
n from the equilibrium position using the lattice unit as length unit;
represents the momentum of the particle
n,
equal to
because the mass of the particle is chosen as the mass unit. Therefore,
is the kinetic energy of the system.
, is the sum of the on-site energies of the classical system with respect to their equilibrium positions. It represents the interaction of the system with other systems, as other layers in silicates, or simply other atom chains in a crystal. Due to the periodicity of the crystal, the simplest form for the on-site energy for a particle is given by the first-order Fourier series, with the condition that
is a stable equilibrium with zero energy:
, known as the Frenkel–Kontorova model. The depth of the potential well is taken as unit of energy, i.e.,
, and the period
of small oscillations of a particle in the potential well
is taken as time unit, i.e.,
. The interaction energy
is the sum of interaction energies between the particles of the system, that is, the energy of the interaction of the system with itself, described as pairs of Lennard-Jones potential between nearest neighbors. The Lennard-Jones potential has the generic physical property of growing to infinity when the distance between particles becomes zero and tending to a constant value, i.e., with zero derivative or zero force, when the particles separate. The Lennard-Jones potential is given by:
The interaction potential has a minimum at
with depth
, being the ratio between the interaction energy and the on-site energy. We use
, a value that brings about the extraordinary mobility of breathers, both in the system without charge [
38,
39] and with it [
33]. We consider
, that is, also equal to the lattice constant, which is justified by the fact that there are no forces on the lattice particles at the equilibrium position. We also add the well depth
to the interaction potential in order to have zero energy at the equilibrium distance.
The quantum Hamiltonian [
40] for an electron or hole added to the system is given by:
with the expectation value:
which is real, since
.
is the probability that the charge is located at site
n with energy
, and the sum of probabilities adds to one, i.e.,
The complex variable is the n-th component of , where |n〉 represents the state for which the charge is completely localized at site n. The possibility of expanding the wave function in a basis of localized states |n〉, that is, states for which the electron is tight-bound to a single atom of the system, consists of the tight-binding approximation.
The evolution of the wave function
is described by the Schrödinger equation
. The Hamiltonian
in (
2), acting on
, leads to:
where
. The left hand side of the Schrödinger equation becomes
. Identifying the components on the basis of vectors
in both sides of the evolution equation, we obtain the following evolution equation for the probability amplitudes
’s:
where
is the reduced Planck constant
in scaled units, with
h being the Planck constant. In Refs. [
25,
41], which study a particular model for the movement of potassium ions in a silicate layer, the scaled units for length, energy, mass, and time are
Å, the interatomic distance;
eV, the electric potential energy between two ions with unit charge
e;
amu, the mass of an ion; and
ps, the derived unit from the previous ones. In those units,
0.00119. In this article, we do not refer to a specific model, but we use
to have a correct order of magnitude. Note that the ratio of masses between a proton and an electron, approximately 2000, is coherent with the fastest movement of the electron with respect to the atoms in the lattice by a factor of
.
Equation (
3) is the expected value of the Hamiltonian
(
2) when the system is in the state
, i.e.,
.
is represented on the basis of |
n〉 by a matrix with elements
.
are, therefore, the diagonal elements. The off-diagonal matrix elements, also called the transfer matrix elements, are
, and are related with the probability of transition between the sites
n and
m. We suppose that they are zero, except for the nearest-neighbor particles, and that they depend on the distance between particles in the form:
Therefore, the transfer elements and the probability of transition between sites increase rapidly when the particles become closer. The parameter values are
, a value corresponding to the
orbitals; and
, a good value for an insulator at equilibrium. Both values are also very convenient for producing traveling polarobreathers [
33].
represents the charge energy at the
n-th site, and in general, it may depend on the variables of the lattice. We keep it in the general notation, but in the present paper, we consider it uniform and constant, which makes possible to set it to zero. However, the nonzero value is useful, as explained below in
Section 3.
The expected Hamiltonian for the lattice and the charge is given by
, with Hamiltonian equations for the lattice variables:
Therefore, the system of governing mathematical equations of the charge–lattice interactions reads as:
where we have omitted the explicit dependence on
t from the variables.
Considering the time-dependent variables
and
, the real and imaginary parts of
, where the normalization is required, the governing Equations (
8) and (9) can be written in the canonical Hamiltonian form with the Hamiltonian:
which is the sum of the lattice and charge Hamiltonians (
1) and (
3), respectively, in variables
,
,
, and
. For the components
,
,
, and
of the canonical variables, the canonical Hamiltonian equations derived from (
10) are:
for all
. Note that the total probability (
4) is conserved along the solutions of Equations (
11)–(14) as the sum:
is conserved. We solve the canonical Hamiltonian Equations (
11)–(14) with the exact charge probability (
4) conserving, symplectic numerical method of Ref. [
33] described in
Section 8.1, to obtain the solution for the charge amplitude
and its probability
. In addition, in
Section 8.2, we describe the numerical algorithm based on nonlinear least squares for the computation of numerically exact time-periodic stationary and moving polarobreathers.
3. Frequency Shift of the Charge Amplitudes
Let us define new probability amplitudes
with real
that does not depend on
n. This change conserves the density matrix [
40], that is, the products
do not change. Consider a state vector
and a quantum observable, corresponding to a Hermitian operator
. The expected value of the observable is given by
. It is obvious that
and
bring about the same expected values as well as derivatives of the expected values, as in (
8). There is no physical form to detect the difference between the two sets of probability amplitudes; the kets
and
represent the same state. They are not, however, solutions of the same Equation (9), as can be seen by supposing that
is a solution, and substituting
in (9) we obtain:
Multiplying (
15) by
, we arrive at the equation:
where
. Therefore, multiplying the solution
of (9) by
brings about a new solution to Equation (9), but with the energy level shifted up by
.
This is a valuable property; exact solutions of (9) do not need to be periodic, but there may exist a solution , which is periodic and a solution of the same evolution Equation (9) with the energy shift to , and therefore, with a frequency shift for all the frequencies. As we have seen above, the magnitude does not appear in any physical observable. It is equivalent to fixing the gravitational potential energy at some specific height.
The actual solution could be obtained as
from (
16), but this is actually irrelevant, since we simply can obtain the actual energies and frequencies of the original system (9) by subtracting
and
from the energy and frequency values, respectively.
5. Linear Approximations
In this section we obtain, the linearized equations corresponding to the dynamical Equations (
8) and (9). We will use them to obtain the dispersion relations (DRs), also called the phonon bands, both for the variables
and
, while there is no dispersion relation for
. They provide the vibrational modes at small amplitude, the phonons, and they are necessary to understand the spectrum of larger-amplitude polarobreathers formed with modes that separate from the linear ones, as observed in
Section 9 and
Section 10. In general, the larger the amplitude, the larger the separation from the phonon band.
The dispersion relations are also useful for the tail analysis used in
Section 6 and
Section 7, which supposes that a localized nonlinear solution has a core of large amplitude that decreases at sites further away from the core, forming a tail of decreasing amplitude. A few sites away from the core, when the amplitude is small enough, the lattice variables would abide by the linear dispersion relations, with a decreasing exponential solution valid only to one side of the core and at some distance from it. This simple method is extremely useful for predicting the properties of nonlinear excitations, such as the increase or decrease in frequency with respect to phonons with the same wavenumber. In this way, the properties of the polarobreathers in
Section 9 and
Section 10 can be easily understood.
If we expand the terms in the dynamical Equations (
8) and (9) to the first order in their variables, using
,
, and
and also seeing (
6), we obtain:
Keeping only the linear terms in (
18) and (19), the lattice and the charge decouple, and we obtain a fully linearized system of equations:
The solutions of linear equations have an exponential form with imaginary exponents if they are bounded, that is, they have the form
and
. The substitution of these expressions into the equations above leads to the dispersion relations:
We have included these dispersion relations in
Figure 1 and in all
plots for reference. Note that the variables
and
become decoupled at the linear limit. Note also that wavenumbers
and
correspond to stationary solutions. For
, the particles vibrate in phase with the same frequency, and for
, they vibrate with an alternate pattern.
There could be some doubt about which variables the linearization should be performed in (
18), because only the density matrix elements
appear. However, the linearization with respect to
and
results in the linear terms on
becoming zero, and (
8) does not change. There is no such problem for (19), as it is already linear in
terms.
In
Section 6 and
Section 7, using the system of linearized Equations (20) and (21), we perform the tail analysis of stationary and moving localized excitations, respectively. We will compare the results in these sections with the present one.
6. Tail Analysis of Stationary Localized Excitations
For the tail of a stationary localized excitation, we propose the ansatz:
which is valid for
(for
, we change the sign in front of
n in the first exponentials). Note that both
implies no localization and extended waves. With the ansatz (24) and assumption of the constant charge energy
, for all
n, from the Equations (20) and (21) we obtain the following equations for the lattice and charge frequencies:
respectively, where
q is the wavenumber. The momentum is given by
, with
or
ℏ in physical units. However, we will use both terms for
q when there is no confusion, as they represent the same physical observable in different units.
If the frequencies
are not real, that will imply decaying solutions; therefore, either both
, where we obtain extended solutions and the linear dispersion relations for the lattice and charge (22) and (23), or
, i.e.,
or
, and for
from (25) and (26), we obtain:
From (27), it can be seen that the localization drives the frequencies below the linear spectrum (above for negative ), and further away the larger the localization is.
For
, there is the opposite effect, i.e., localization increases the frequencies above the linear spectrum (below for negative
). From (25) and (26):
Note that the localization parameters
do not need to be the same in (25) and (26) and (27) and (28) for the lattice and the charge. A good estimate would be
, as in the lattice Equation (
8), the charge amplitude
products
appear. Furthermore,
has the same pattern as
As the
modes are not actually traveling, the two modes will appear mixed, i.e.,
and
where
. In this way, we can obtain the time dependence on the charge probability
, i.e.,
If we write
for
, we obtain:
In this way, we will observe in the charge probability spectrum two frequencies: , corresponding to a stationary deformation, and , where the charge probability spectrum is independent of the value. Note that as is an observable, its frequencies can be measured; from them, we can deduce the difference in frequencies from the and modes of , but not their actual value, because there are no physical means of knowing which is the shift of the frequencies. We choose for our convenience the value of that makes periodic with a commensurate period with the lattice one. However, that selection has no physical consequences, and we will plot the spectrum corresponding to for simplicity.
7. Tail Analysis of Moving Localized Excitations
We can repeat the tail analysis above for the moving solutions. In this case, the trial solutions in (24) are changed to:
These ansätze are valid for
or for
changing
to
. Considering first the ansatz (29) for
, in the moving frame
, the frequency is
, with
that is,
is vibrating with the same frequency
but with a smaller amplitude and a difference of phase
q. The general solution for a traveling breather would be a sum of terms as
in (29), with the same frequency
in the moving frame. The parameter
would be also dependent on each mode. The larger
is, the more localized the specific localized mode would be, and likewise for
with the ansatz (30).
We also assume that the general solution is exact, that is, it repeats after some fundamental time
displaced an integer number of sites
, called the step. Then, all the modes (29) have the same properties, that is,
,
, and step
s. The fundamental frequency is defined as
. The exactness condition implies that
for the integers
and
. See Ref. [
25] for more details. The fundamental period
could, in principle, be different for the lattice and the charge amplitude, but for the common system to be exact, there should be integer multiples of both periods to obtain a common fundamental period
and step
s.
Substituting the ansatz (29) for
into the linear Equation (20), we obtain:
Compare (31) with Equation (25) of
Section 6. Expanding the left hand side of (31), we arrive at two equations for the real and imaginary part:
For compactness, we use the laboratory frequency:
of the moving mode with wavenumber
q.
For delocalized waves, with
, from (32), we recover the lattice dispersion relation (22) and the group velocity of the linear extended waves:
The latter equation indicates that there is only one mode with a given : the one where the slope of the dispersion relation is precisely . This is why it is not possible to have a coherent wave at the linear limit, as every mode has a different velocity.
As
and increases with the localization parameter
, in addition, if
,
, and if
,
, then from the first equation of (32), we find that
Therefore, it can be seen that is above the linear frequency for the same . However, when becomes smaller than , the two terms of the nonlinear correction have different signs, but they are also clearly above the linear frequency in a close proximity to , at which point the negative term is zero. The main conclusion is that a solution such as the one proposed is possible below the linear spectrum, closer to , and above the linear spectrum, closer to . The latter would be the case for our system.
Let us analyze the ansatz for
, given by (30). The substitution into Equation (21) with the constant
leads to the following equation:
where the charge amplitude laboratory frequency is given by:
For the comparison with the stationary case, compare Equation (33) with (26) of the previous section.
Equation (33) leads to two equations for the real and imaginary part:
The first equation gives the energy of the system, and the second gives the velocity. Note that a change in frequency , corresponding to , is the frequency with the corresponding energy for the system with .
For
, we recover the linear dispersion relation (23) together with the group velocity:
Again, there is only one linear mode for a given velocity , and coherent wave packages of are not possible at the linear limit or close to it.
The modes with a higher localization
value correspond to faster propagating modes compared to the corresponding linear ones, since
for
. From the equivalent considerations above, for
, the localization energies
are above the linear energies
, and vice versa for
, i.e.,
9. Stationary Polarobreathers
9.1. Generation of Approximate Stationary Polarobreathers
The methods used to produce polarobreathers in this model (solving (
11)–(14)) are extremely efficient; they have been used in previous works in one and two dimensions [
33,
38,
39]. In this section, we present the method for the stationary case; the moving polarobreather case will be presented in the following
Section 10.
We introduce nonzero initial conditions only for the velocities or momenta:
The parameter
is related with the kinetic energy delivered to the system as
. The reference index
can be arbitrary because the system is periodic, but we usually take
, for visual plotting purposes. The charge wave function is located initially with probability one, with the pattern:
That is, the charge is completely localized at with probability one. This combined pattern (50) and (51) proves to be very efficient in obtaining quite good stationary solutions with long life. Other methods and patterns have also been investigated, for example, producing a local compression, which often brings about a stationary breather and two traveling ones in opposite directions. Moreover, different patterns for the positions and momenta have been considered. Many of them work quite well, but this is the preferred one for simplicity and for obtaining results. We describe the results for , corresponding to the kinetic energy , in scaled units. Other values of bring about qualitatively similar results.
We perform the 2D discrete Fourier transform in positions and time (
) of time-series data on the variables
,
, and
, which are represented in
Figure 2-top. For reference, the dispersion relations (22) and (23) for
and
are also plotted with gray solid and dashed lines, respectively. Numerical results were obtained, setting all
in (
11)–(14).
As the first two quantities are real, for the
components, it holds that
and
, which is a symmetry that can be observed in the corresponding two upper plots. Usually, in this case, the negative frequencies are not represented, but here, they are included for comparison with the
of
, where the symmetry does not hold, as
is complex. Some main features from the top plots of
Figure 2 can be discerned:
For the
of
, there appear two horizontal lines at
, centered around
, and some frequency
above the dispersion relation and centered around
. This means that the
breather is composed of a soliton, that is, a static deformation with a displacement largely in phase and a staggered vibration above the
phonon spectrum, i.e., a nonlinear vibration, as demonstrated in
Section 6. The static solution appears due to the asymmetry of the Lennard-Jones potential well, which makes compression harder than expansion, and therefore, oscillations with respect to the equilibrium distance are larger for expansion than for compression.
For
, two horizontal lines appear, one at zero frequency, a stationary soliton close to
, that is, with nearest neighbors in phase; and also at frequency
, close to the modes
, that is, with a staggered profile. The soliton here is necessary, as
is a positive quantity, so the vibration has an alternating pattern around a stationary one. This means that there is a small change in probability between neighboring particles with the frequency
. This was also explained in
Section 6. Depending on the nonlinearity and the system, the interchange of probability will be larger or smaller.
For
, we find three main frequencies, two of them
, close to the
phonon spectrum, one above and the other below. The upper one is around
, i.e., with a staggered profile; and the lower one is around
, that is, with a bell profile. These two frequencies are explained in
Section 6. The other two are located at
. These appear because the quantum Hamiltonian has the time periodicity of
, which appears in the transfer matrix elements.
As deduced in
Section 6 the
frequency is equal to the difference between the phonon frequencies
, in this case being
. For
, the two frequencies would be
. See
Section 3 for details.
There are some other lines of weaker intensity in
of
, but especially for
. We can observe some phonons for
and even more for
, where they occupy the whole
-phonon band, but not for
, as there is no dispersion relation for
, because its evolution depends on the other terms of the density matrix
[
40]. Results on the density matrix for polarobreathers will be discussed and published elsewhere.
9.2. Exact Stationary Polarobreathers
The approximate solution described above is good enough to be used as a seed in the numerical algorithm of
Section 8.2 for obtaining numerically exact polarobreathers. The two main frequencies are
and
, with corresponding periods:
and
. The frequencies of
are analyzed in a different way, which is explained below. We can observe that the periods and frequencies are approximately commensurate:
. Therefore,
is a good estimate for the common period for both
and
, and it is the fundamental time or period taken for the whole system [
25].
We suppose that
in Equations (12) and (14), with initial value
, where
are the upper and lower frequencies above and below the
-phonon band; see the top right plot of
Figure 2. We recall that the value of
also gets adjusted and found in the damped Gauss–Newton method of
Section 8.2. This is an essential degree of freedom to obtain exact periodic solutions with the desired numerical accuracy
.
The profile of the exact polarobreathers and their (lack of) change with time for
and
can be seen in
Figure 3, where the solution is visualized in time after five fundamental periods. The small asymmetry of
in
Figure 3b can be observed. The
of the exact solution is plotted in
Figure 2-bottom; the main features are as follows:
All the phonons have disappeared from the dispersion bands.
Extra bands have also disappeared, except for the ones described above, which have become much more defined.
In the
of
, the zero-frequency component corresponding to the stationary soliton and the frequency
slightly above the positive phonon band, centered at
(also the symmetric band at
), have remained. These features are in accordance with the theory described in
Section 6.
In the
of
, already shifted to
by the numerically found
value, only two bands—
slightly above the
phonon band at
and below at
, which correspond to a hard potential case—have remained; see
Section 6.
Furthermore, for the of , there is a weak negative frequency corresponding to the forcing by the matrix transfer elements , which change with , the frequency. The corresponding band is symmetric in q, but does not include . This means that it is a stationary wave: the sum of waves traveling in opposite directions with wavenumbers around or wavelength . With greater initial kinetic energy, the positive frequencies also appear above the positive phonon band and are centered at .
In the plot of charge probability , only the bands with frequencies at zero and have remained, due to the election of , (as well as , due to the symmetry).
We conclude that although are not observable, their difference is indeed observable, and appears in the spectrum of the charge probability. Thus, may appear in the spectrum of physical systems, providing a valuable insight into the states of extra electrons or holes of the system.
9.3. Stability of Exact Stationary Solutions: The Switching Mode
We can numerically obtain the Floquet matrix, that is, the at the exact solution. As the system is symplectic, if there is an eigenvalue , then is also an eigenvalue. As the system is also real, if is an eigenvalue, then so are and as the conjugate of . Therefore, the eigenvalues come in quadruplets if they are complex with , and in pairs if , or if is real. The perturbation of the system with an eigenvector results in the perturbation growing as with r periods. Therefore, the (linearized) system is only stable if for all eigenvalues. When changing a parameter as the frequency, the complex eigenvalues have to leave the unit circle as a quadruplet; therefore, for nonreal , two pairs of complex eigenvalues in the unit circle have to first collide for an instability to appear. This will be a Hopf bifurcation to a set of solutions with different periods . Most of these eigenvalues correspond to phonons outside the core of the polarobreather. However, two eigenvalues colliding at can get out of the unit circle in a period-doubling bifurcation. Two eigenvalues can collide at and get out of the circle as two real eigenvalues: one larger than one and another smaller, corresponding to two eigenvectors: one growing and other contracting to conserve the area in the phase space.
The system structurally has four eigenvalues at , corresponding to two growth modes, i.e., small changes in amplitude in or ; and two phase modes, corresponding to two small changes in phase or time origin. Their meaning is that solutions also exist with almost the same period and slightly different amplitudes or phases.
There is a peculiarity in our Floquet matrix calculation: it is performed at ; therefore, an eigenvalue for the variables with period appears as , and for , it appears as compared to the period for . This means that instability eigenvalues appear much more grown or contracted than usual, and the numerical imprecision for the eigenvalues at is amplified.
We can observe the eigenvalues of the exact polarobreathers in
Figure 4a. The reference circle appears populated with the phonon eigenvalues, and the four structural eigenvalues exist at +1. However, there is also a pair of real instability eigenvalues, which are very unstable, as just explained. For the breather period, they would be reduced to around
and
. The corresponding two eigenvectors appear in
Figure 4b for
, together with the solution at
. We observe a small asymmetry in the profile of
, and the eigenvectors tend to increase the probability at the neighboring particles away from the center of localization.
Long-time simulations confirm this interpretation. After some time, the polarobreather switches a position; after some time, it switches back, and so on. Therefore, in spite of the instability, which gets stabilized by the nonlinearity of the lattice, the breather and charge probability are stationary. They do not disperse or travel, but experience quasi-periodic switches between two neighboring sites.
Figure 5 shows the switching behavior of a polarobreather in a long-time simulation.