论文标题
碰撞冲击波时的粒子加速度
Particle acceleration at colliding shock waves
论文作者
论文摘要
我们在两个碰撞冲击波系统中对颗粒的扩散冲击加速度进行了建模,并提出了一种在测试粒子近似和高能量极限中分析时间依赖时间依赖性问题的方法。特别是,我们表明,在此限制中,可以在自相似解决方案的帮助下分析问题。 While a number of recent works predict hard ($E^{-1}$) spectra for the accelerated particles in the stationary limit, or the appearance of spectral breaks, we found instead that the spectrum of accelerated particles in a time-dependent collision follows quite closely the canonical $E^{-2}$ prediction of diffusive shock acceleration at a single shock, except at the highest energy, where a hardening appears, originating a在指数截止之前,颠簸的功能。我们还调查了通过两种冲击系统进行预先存在的宇宙射线的重新连接的效果,并发现在某些条件下,截止区域可能会出现光谱特征。最后,此处介绍的数学方法非常笼统,可以轻松地应用于各种天体物理情况,包括在积聚流中站立冲击,散落的冲击,通过更快的冲击以及风风浪费或冲击或冲击碰撞的慢速冲击的向后碰撞。
We model the diffusive shock acceleration of particles in a system of two colliding shock waves and present a method to solve the time-dependent problem analytically in the test-particle approximation and high energy limit. In particular, we show that in this limit the problem can be analysed with the help of a self-similar solution. While a number of recent works predict hard ($E^{-1}$) spectra for the accelerated particles in the stationary limit, or the appearance of spectral breaks, we found instead that the spectrum of accelerated particles in a time-dependent collision follows quite closely the canonical $E^{-2}$ prediction of diffusive shock acceleration at a single shock, except at the highest energy, where a hardening appears, originating a bumpy feature just before the exponential cutoff. We also investigated the effect of the reacceleration of pre-existing cosmic rays by a system of two shocks, and found that under certain conditions spectral features can appear in the cutoff region. Finally, the mathematical methods presented here are very general and could be easily applied to a variety of astrophysical situations, including for instance standing shocks in accretion flows, diverging shocks, backward collisions of a slow shock by a faster shock, and wind-wind or shock-wind collisions.