Abstract  Collisionless shocks are wellknown structures in astrophysical environments which dissipate bulk flow kinetic energy and accelerate large fraction of particle. Spacecrafts have firmly established the existence of the socalled terrestrial foreshock region magnetically connected to the shock and filled by two distinct populations in the quasiperpendicular shock region (i.e. for 45° ? ?Bn ? 90°, where ?Bn is the angle between the shock normal and the upstream magnetic field) : (i) the fieldaligned ion beams or « FAB » characterized by a gyrotropic distribution, and (ii) the gyrophase bunched ions or « GPB » characterized by a NON gyrotropic distribution. The present work is based on the use of two dimensional PIC simulation of a curved shock and associated foreshock region where full curvature effects, time of flight effects and both electrons and ions dynamics are fully described by a self consistent approach.
Our previous analysis (Savoini et Lembege, 2015) has evidenced that these two types of backstreaming populations can originate from the shock front itself without invoking any local diffusion by ion beam instabilities. Present results are focussed on individual ion trajectories and evidence that "FAB" population is injected into the foreshock mainly along the shock front whereas the "GPB" population penetrates more deeply the shock front. Such differences explain why the "FAB" population loses their gyrophase coherency and become gyrotropic which is not the case for the "GPB". The impact of these different injection features on the energy gain for each ion population will be presented in détails.
Savoini, P. and B. Lembege (2015), « Production of nongyrotropic and gyrotropic backstreaming ion distributions in the quasiperpendicular ion foreshock région », J. Geophys. Res., 120, pp 71547171, doi = 10.1002/2015JA021018.
