用冰立方和冰顶进行宇宙射线测量

Dennis Soldin
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引用次数: 1

摘要

冰立方是一个立方公里的切伦科夫探测器,位于地理南极的冰层深处。深冰探测器产生的主要事件包括穿透大气的介子,其能量大约在300 GeV以上,由宇宙射线空气阵雨产生。此外,表面阵列,冰顶,测量电磁成分和GeV介子的空气淋浴。因此,冰立方和冰顶提供了独特的机会,以前所未有的详细数据研究宇宙射线。我们将介绍冰立方和冰顶最近的合成射线测量结果。在本综述中,我们将重点介绍从250 TeV到EeV范围内的宇宙射线能谱的测量以及它们的质量组成高于3 PeV。我们还将报告最近对空气阵雨中介子含量的测量结果,并讨论它们与当前强子相互作用模型预测的一致性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Cosmic ray measurements with IceCube and IceTop
IceCube is a cubic-kilometer Cherenkov detector in the deep ice at the geographic South Pole. The dominant event yield in the deep ice detector consists of penetrating atmospheric muons with energies above approximately 300 GeV, produced in cosmic ray air showers. In addition, the surface array, IceTop, measures the electromagnetic component and GeV muons of air showers. Hence, IceCube and IceTop yield unique opportunities to study cosmic rays with unprecedented statistics in great detail. We will present recent results of comic ray measurements from IceCube and IceTop. In this overview, we will highlight measurements of the energy spectrum of cosmic rays from 250 TeV up to the EeV range and their mass composition above 3 PeV. We will also report recent results from measurements of the muon content in air showers and discuss their consistency with predictions from current hadronic interaction models.
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