A map for systems with resonant trappings and scatterings
A. V. Artemyev, A. I. Neishtadt, A. A. Vasiliev

TL;DR
This paper introduces a new map model for resonant systems with strong scatterings and trappings, capturing the transition between stochastic and regular dynamics in phase space.
Contribution
It develops a novel map for systems with strong scatterings and trappings, extending previous models to describe non-diffusive drift and fast jumps in phase space.
Findings
The map describes the transition between stochastic and regular dynamics.
Critical parameter values for phase space transition are identified.
The model applies to a wide range of physical systems with resonant phenomena.
Abstract
Slow-fast dynamics and resonant phenomena can be found in a wide range of physical systems, including problems of celestial mechanics, fluid mechanics, and charged particle dynamics. Important resonant effects that control transport in the phase space in such systems are resonant scatterings and trappings. For systems with weak diffusive scatterings the transport properties can be described with the Chirikov standard map, and the map parameters control the transition between stochastic and regular dynamics. In this paper we put forward the map for resonant systems with strong scatterings that result in non-diffusive drift in the phase space, and trappings that produce fast jumps in the phase space. We demonstrate that this map describes the transition between stochastic and regular dynamics and find the critical parameter values for this transition.
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**A map for systems with resonant trappings and scatterings
**
A. V. Artemyev1,2, A. I. Neishtadt3,2, A. A. Vasiliev2
1* Institute of Geophysics and Planetary Physics, University of California, Los Angeles, California, USA
2 Space Research Institute, Moscow, Russia
3 Department of Mathematical Sciences,
Loughborough University, UK
Abstract
Slow-fast dynamics and resonant phenomena can be found in a wide range of physical systems, including problems of celestial mechanics, fluid mechanics, and charged particle dynamics. Important resonant effects that control transport in the phase space in such systems are resonant scatterings and trappings. For systems with weak diffusive scatterings the transport properties can be described with the Chirikov standard map, and the map parameters control the transition between stochastic and regular dynamics. In this paper we put forward the map for resonant systems with strong scatterings that result in non-diffusive drift in the phase space, and trappings that produce fast jumps in the phase space. We demonstrate that this map describes the transition between stochastic and regular dynamics and find the critical parameter values for this transition.
1 Introduction
Resonant phenomena determine dynamics of many systems with two time scales: fast periodic or quasi-periodic motion and slow change of parameters of this motion. The classical examples of such systems are asteroid and planetary dynamics (e.g., [12, 1]), hydrodynamical vortices (e.g., [15]), and various plasma systems with wave-particle interaction, e.g., laboratory experiments on inertial confinement fusion (e.g., [7]), plasma acceleration (e.g., [4]), space-plasma shocks (e.g., [19, 10]), and planetary radiation belts (e.g., [17, 9]). In this paper we consider systems with multiple passages through a nonlinear resonance, where main resonant phenomena are trappings into resonance and scatterings on resonance.
Dynamics in such systems can be modeled by the Hamiltonian
[TABLE]
Here are conjugate momentum and fast rotating phase (with the frequency , ), is a slowly changing parameter (with the rate ), , , and are system characteristics depending on , and describes the perturbation of -dynamics (as a model one can take ). The resonance in system (1) occurs when the frequency drops to zero (i.e. ). To describe the resonant dynamics we introduce the new momentum and get the pendulum Hamiltonian (see Sect. 6.1.7 in [1] or [5]),
[TABLE]
where .
For this Hamiltonian around the resonance, , variables () change fast, at the rate , and parameter changes slowly, at the rate . Depending on the shape of phase trajectories plotted for frozen , the resonant systems can be formally separated into two classes: with all resonant trajectories passing through the resonance (, see Fig. 1(a)) and with some resonant trajectories oscillating around the resonance (, see Fig. 1(b)). The area of the region filled with such closed trajectories is the key characteristics of the resonant systems (see Sect. 6.4.7 in [1]).
We consider the situation when parameter changes periodically, and the system repeatedly passes through the resonance. During the period of change of the system passes through resonance several times. However, for simplicity of the exposition, we will assume that only one such a passage has a considerable effect on dynamics (value is small at the other passages). Thus, at the resonance we can use relation and consider coefficients in (2) as functions of (e.g., ). The phase variation on this period is given by the Hamiltonian equation (1): where and we use such normalizations of , functions that , (all integrals include one period of change)
Far from the resonance, stays constant up to small oscillations. Effectively, changes only due to dynamics in a narrow resonant region where . Between two consecutive passages through this region the phase changes by a value . Let be a value of the phase at the first crossing of during one period of change. Passage through the resonance can be characterized by some new phase which differs from by a -periodic function of . This new phase is a normalized value of the Hamiltonian on the phase portraits in Fig. 1 (see details in [13]). In the case of passage through resonance without trapping, experiences a change during each passage. Thus we have a map which in the principal approximation has a form [11, 16]. Here phase is defined , is -periodic in , and [13].
For systems of the first class (Fig. 1a) there is no average drift [13]. Dynamics of in such systems is described by diffusive-like scattering (with the diffusion rate ; is the averaging over phase values for an ensemble of trajectories with the same initial ), whereas the map in can be reduced to a map that is similar to the standard Chirikov map [6].
Systems of the second class (Fig. 1b) are characterized by competition of drifts and rapid jumps induced by trappings [13, 8]. Note is called scattering despite it is a deterministic shift, because for the equation (1) the scattering is a sum of its mean value and a term of the same order with the average equal to zero. When many passages through the resonance are considered, the effect of the latter term is small and is neglected here.
A trapping (with the following release from the resonance) results in a significant change of , , but only a small fraction of phase points from plane with , undergo trappings [13]. The change of between a trapping and the release is determined by conservation of the adiabatic invariant for trapped particles, i.e. a trapping and the following release occur at the same value of area , see Fig. 1(c). This fine balance between trappings (and jumps) of a small fraction of phase points and drifts (with the rate ) of untrapped points defines dynamics on long time intervals including many passages through resonances [3].
The mapping technique (i.e. construction of the map in plane) is well developed for resonant systems with , where this technique provides an effective tool for modeling the long-term system dynamics and calculating the critical system parameters that control the transition between stochastic and regular dynamics [11, 16]. However, there is no map for the resonant systems shown in Fig. 1b, i.e. for systems with . In this paper we propose a map that describes trapping and scattering, and study the transition between regular and stochastic dynamics in such systems.
2 System dynamics
Figure 1(c) shows an example of profile and directions of trapping jumps and scattering drifts. For each there is a certain range of from which the phase point will be trapped, whereas for the phase point will be scattered with change . We choose model that satisfies the asymptotic behavior of small around (see Appendix in [2]). For , the map describing the system in Fig. 1(c) can be written as
[TABLE]
where and controls the inhomogeneity of (see details below). For the map in is for any . The ratio controls the system dynamics.
The map (4) is based on two important relations between scattering and trapping effects: (1) the probability of a trapping (i.e., the relative measure of values for which trappings occur) equals to the gradient of the scattering rate ; (2) a trapping and the consequent release occur at the same value of (transition is due to the symmetric shape of chosen for simplicity). These two relations guarantee the conservation of the phase space volume (absence of dissipation) in systems with trappings and scatterings (see details in [3, 2]).
Map (4) describes changes of composed of the drift to smaller (with steps ) and jumps to larger (from to ) with a small probability of such jumps. Figure 1(d) shows a fragment of and evolution including one such jump. The long term -dynamics includes many jumps connected by drifts (see Fig. 1(e,f)). For large this long-term dynamics uniformly fills the entire plane (see Fig. 1 (g)). However, Fig. 1 (h, i) shows that with decrease of regions of more/less dense concentration of phase points appear (i.e., phase space becomes structured). For the phase space is filled with regular structures (see Fig. 1(j)) indicating a regular phase point motion (see for comparison [11, 16]). Therefore, there is a critical value separating regular and stochastic motions for the map (4).
3 Correlation decay
To estimate the critical , we consider a set of systems with different and fixed . For each system we perform iterations and plot the distribution of . Such distributions obtained for different can be combined into 2D distribution in the plane. Figure 2(a) shows this 2D distribution for (for each the -distribution is transformed to a distribution on the interval , and thus the uniform distribution has the density equals one for all ). For large , -distributions are uniform (white color in the figure), but with decrease the -distribution becomes more structured (red and blue colors show deviations from the density of the uniform distribution, i.e. from one). This transition between the uniform -distribution (i.e., stochastic -dynamics) to more structured one (i.e., more regular -dynamics, but still including elements of chaotic behavior) occurs when the correlation of and becomes essential. This change of -distributions with decrease of is well seen in Fig. 2(b), where we plot the average as a function of ( is the averaging over -distribution with fixed). The value of is close to one for uniform -distributions, but deviates from one as soon as structures appear in the -distributions. Therefore, we can use as a measure of deviation of the -distribution from the uniform one. Figures 2(c,d) show the same distribution for : with larger the -distribution deviates from the uniform one at larger .
Figure 2(e) shows as a function of and . There is the clearly seen area of (white color) that corresponds to the uniform -distributions (absence of and correlations). This area occupies ranges of large and small . The increase of (or decrease of ) leads to deviation of from one (colored area). To determine the boundary of this area, for each we evaluate corresponding to and plot these points in Fig. 2(f). The obtained dependence can be fitted by (shown in panels (e,f)), i.e., numerical calculations gives the scaling .
The transition of -dynamics from stochastic to more regular should result in similar transition of -dynamics. To show this effect, we consider six pairs of parameters. For each pair we calculate trajectories with different initial and iterations. Then we plot -distributions together with the initial -distribution given by . Bottom panels of Fig. 2 show six -distributions and corresponding locations of the system in the plane. There are two -distributions for (shown by black color), two -distributions for (shown by green color), and two -distributions for (shown by red color). The stochastic -dynamics for results in stochastic -dynamics, and final -distributions are almost uniform, i.e. phase points are uniformly distributed in the plane. For the -distributions deviate from the uniform one, but still fill the entire range. These -distributions (shown by green) contain some structures that cannot be seen in the black -distributions. More regular (or less stochastic) -dynamics at results in more regular -dynamics, and the corresponding -distributions (shown in red) do not cover the entire space. Therefore, defines the parametric boundary that separates stochastic and regular dynamics in the plane.
4 Discussion and conclusions
Although the map (4) describing the dynamics in systems with drifts and trapping is quite different from the classical maps describing the diffusive-like scattering [6, 11, 16], this map has the same property of transition between stochastic and regular dynamics. This transition occurs when the rates of nominal slow and fast motions become comparable, i.e. when . For systems with the consecutive scatterings can be considered as independent changes, and thus for such systems the Fokker-Planck-type equations for -distribution can be derived [18]. For systems with the consecutive scatterings are correlated, and such correlations prevent the application of classical kinetic equations for description of -distribution evolution. This conclusion limits the use of the random phase approximation to describe the long-term dynamics in various systems with nonlinear resonant interaction (trapping and scattering drift). Thus construction of Fokker-Planck-type equations for such systems (e.g., [14, 2]) should be constrained to the parameter ranges with .
To conclude, we have proposed the map describing dynamics in a resonant system with the effects of drifts and trappings. This map can be used to model long-term dynamics in such systems instead of the approach based on solving a kinetic (Fokker-Planck-type) equation for -distributions (e.g., [14, 3]). The main advantages of the map (4) approach are simplicity of inclusion of additional resonances (i.e., construction of , as a combination of several terms) and description of the phase-correlation effects.
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