On the Flat Proton Spectra at Interplanetary Shocks

M. Malkov
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Abstract

Spacecraft observations of interplanetary shocks have revealed signi(cid:28)cant deviations in energetic particle spectra from the di(cid:27)usive shock acceleration (DSA) theory predictions. Within almost two decades of particle energy, spanning about seven e-folds upstream, the particle (cid:29)ux is almost energy independent. Although at and behind the shock, it falls o(cid:27) as ϵ − 1 (as predicted by DSA for reasonably strong shocks), the (cid:29)ux decreases with the coordinate close to the shock upstream progressively steeper at lower energies, which leads to a (cid:29)at energy distribution. Within a standard DSA solution under a (cid:28)xed turbulence spectrum, pre-existing or self-excited by accelerated particles, a (cid:29)at particle spectrum over an extended upstream area means that the particle di(cid:27)usivity must be energy-independent, contrary to most transport models. We propose a resolution of this paradox by invoking a strongly nonlinear solution upstream under a self-driven but short-scale turbulence, in which the particle di(cid:27)usivity increases with energy as ∝ ϵ 3 / 2 , but also decays with the wave energy as 1 /E w , which compensate for the ϵ 3 / 2 rise. The main di(cid:27)erence with the traditional DSA is that the wave-particle interaction is nonresonant, and the turbulence is not saturated at the Bohm level (that would require δB ∼ B 0 turbulence saturation amplitude). A steep, energy-dependent (cid:28)nal drop in the particle (cid:29)ux far ahead of the shock to its background level in the solar wind is likely due to a quick particle escape upstream
关于行星际激波中的平坦质子谱
航天器对行星际冲击的观测揭示了高能粒子光谱与冲击加速度(DSA)理论预测的显著(cid:28)偏差。在粒子能量的近20年里,跨越了大约7 e倍的上游,粒子(cid:29)ux几乎与能量无关。尽管在激波处和激波后,它随着λ−1(如DSA预测的那样)下降为0 (cid:27),但在较低能量下,(cid:29)ux随着靠近激波上游的坐标逐渐变陡而减小,这导致能量分布为(cid:29)。在(cid:28)混合湍流谱下的标准DSA溶液中,预先存在或由加速粒子自激,在扩展的上游区域上的粒子谱a (cid:29)意味着粒子di(cid:27)活度必须与能量无关,这与大多数输移模型相反。我们通过在自驱动但短尺度湍流下调用上游的强非线性解来解决这一悖论,其中粒子di(cid:27)活度随能量∝λ λ λ δ 3 / 2而增加,但也随波能量δ 1 /E w而衰减,这补偿了λ λ 3 / 2的上升。与传统DSA的主要差异(cid:27)是波粒相互作用是非共振的,并且湍流在Bohm水平上不饱和(这需要δB ~ b0湍流饱和振幅)。在太阳风中,粒子(cid:29)的急剧、能量依赖(cid:28)的nal下降(cid:29)远远早于激波到其背景水平,这可能是由于粒子在上游的快速逃逸
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