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arXiv 2202.09211astro-ph.HE
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冰内宇宙射线空气簇射诱导粒子级联的模拟

Simulation of in-ice cosmic ray air shower induced particle cascades

Simon De Kockere, Krijn D. de Vries, Nick van Eijndhoven, Uzair A. Latif

AI总结:

本文结合 CORSIKA 与 Geant4 模拟宇宙射线空气簇射在极地冰层中的级联,参数化电荷分布并分析 Askaryan 发射及 RADAR 探测可行性。

摘要:

我们提出了高能宇宙射线空气簇射穿透极地地区可见的高海拔冰层的详细微观模拟。我们结合使用 CORSIKA 蒙特卡洛代码和 Geant4 模拟工具包,并聚焦于在冰中发展的粒子级联,以描述其最显著的特征。我们讨论了冰层对随空气簇射深度变化的粒子总数的影响,并给出了级联前锋中电荷分布随宇宙射线空气簇射 Xmax 变化的通用参数化,该参数化可用于对冰内粒子级联的预期 Askaryan 无线电发射进行解析和半解析计算。我们表明,宇宙射线空气簇射的核心在冰内传播过程中占主导地位,因此产生的冰内粒子级联与中微子诱导的粒子级联非常相似。最后,我们给出了冰内粒子级联 Askaryan 无线电发射的微观模拟结果,表明该发射由簇射核心主导,并讨论了利用 RADAR 回波技术探测粒子级联在冰中产生的等离子体的可行性。

英文摘要:

We present detailed microscopic simulations of high-energy cosmic-ray air showers penetrating high-altitude ice layers that can be found at the polar regions. We use a combination of the CORSIKA Monte Carlo code and the Geant4 simulation toolkit, and focus on the particle cascade that develops in the ice to describe its most prominent features. We discuss the impact of the ice layer on the total number of particles in function of depth of the air shower, and we give a general parameterization of the charge distribution in the cascade front in function of Xmax of the cosmic ray air shower, which can be used for analytical and semi-analytical calculations of the expected Askaryan radio emission of the in-ice particle cascade. We show that the core of the cosmic ray air shower dominates during the propagation in ice, therefore creating an in-ice particle cascade strongly resembling a neutrino-induced particle cascade. Finally, we present the results of microscopic simulations of the Askaryan radio emission of the in-ice particle cascade, showing that the emission is dominated by the shower core, and discuss the feasibility of detecting the plasma created by the particle cascade in the ice using RADAR echo techniques.

机构、总结、中文摘要均由AI分析而来,可能存在错误,请以论文正文为准。

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