Inward Diffusion and Acceleration of Particles Driven by Turbulent Fluctuations in Magnetosphere
arXiv:1609.02373 · doi:10.1063/1.4967281
Abstract
Charged particles in a magnetosphere are spontaneously attracted to a planet while increasing their kinetic energy via inward diffusion process. A constraint on particles' micro-scale adiabatic invariants restricts the class of motions available to the system, giving rise to a proper frame on which particle diffusion occurs. We investigate the inward diffusion process by numerical simulation of particles on constrained phase space. The results reveal the emergence of inhomogeneous density gradient and anisotropic heating, which is consistent with spacecraft observations, experimental observations, and the recently formulated diffusion model on the constrained phase space.
References in corpus (5)
- Self-organization in foliated phase space: Construction of a scale hierarchy by adiabatic invariants of magnetized particles
- Observation of particle acceleration in laboratory magnetosphere
- Up-Hill Diffusion Creating Density Gradient - What is the Proper Entropy?
- A Stochastic Model of Inward Diffusion in Magnetospheric Plasmas
- Anisotropy in broad component of H line in the magnetospheric device RT-1