Lévy Flights and Leaky Boxes: Anomalous Diffusion of Cosmic Rays
Naixin Liang, Siang Peng Oh
TL;DR
This work probes whether cosmic ray transport in turbulent galactic environments can be described by anomalous diffusion (sub- or superdiffusion) and how finite galactic sizes truncate Lévy flights, forcing a reversion to standard diffusion on the escape timescale.Using Monte-Carlo particle-tracking, the authors implement fractional diffusion with stable distributions (parameters α for space and β for time) and examine the impact of finite pathlengths, absorbing boundaries, and advection/streaming, revealing that gaussianization is a robust outcome except in systems with very long confinement times.Key findings show that in bounded or wind-influenced settings, CR profiles converge to standard diffusion with an effective κ_eff ≈ κα l_max^{2−α}, while in unbounded cases, pure fractional diffusion yields distinctive CR distributions such as P_CR ∝ r^{α} in 3D spheres and heavy-tailed PDFs in 1D/2D.Practically, the results imply that conventional diffusion modeling remains broadly valid for most CR applications, but environments with long escape times (e.g., CGM/ICM) or unusual trapping structures could retain anomalous diffusion signatures, motivating a shift in both interpretation and diagnostics, such as using width scaling γ ∝ t^{1/α} instead of ⟨x^2⟩ when truncation is present.
Abstract
In classical diffusion, particle step-sizes have a Gaussian distribution. However, in superdiffusion, they have power-law tails, with transport dominated by rare, long Lévy flights. Similarly, if the time interval between scattering events has power-law tails, subdiffusion occurs. Both forms of anomalous diffusion are seen in cosmic ray (CR) particle tracking simulations in turbulent magnetic fields. They also likely occur if CRs are scattered by discrete intermittent structures. Anomalous diffusion mimics a scale-dependent diffusion coefficient, with potentially wide-ranging consequences. However, the finite size of galaxies implies an upper bound on step-sizes before CRs escape. This truncation results in eventual convergence to Gaussian statistics by the central limit theorem. Using Monte-Carlo simulations, we show that this occurs in both standard finite-thickness halo models, or when CR diffusion transitions to advection or streaming-dominated regimes. While optically thick intermittent structures produce power-law trapping times and thus subdiffusion, gaussianization also eventually occurs on timescales longer than the maximum trapping time. Anomalous diffusion is a transient, and converges to standard diffusion on the (usually short) timescale of particle escape, either from confining structures (subdiffusion), or the system as a whole (superdiffusion). Thus, standard assumptions of classical diffusion are physically justified in most applications, despite growing simulation evidence for anomalous diffusion. However, if escape times are long, this is no longer true. For instance, anomalous diffusion in the CGM or ICM would change CR pressure profiles. Finally, we show the standard diagnostic for anomalous diffusion, $\langle d^2 \rangle \propto t^α$ with $α\neq 1$, is not justified for truncated Lévy flights, and propose an alternative robust measure.
