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Simulation of muon-induced neutral particle background for a shallow depth Iron Calorimeter detector

机译:模拟muon-induced中性粒子背景浅深度铁量热计探测器

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The Iron Calorimeter (ICAL) detector at the India based Neutrino Observatory (INO) is planned to be set up in an underground cavern with a rock overburden of more than 1 km. This overburden reduces the cosmic muon flux by a factor of 10~6 with respect to that at the sea level. In this paper, we examine the possibility of a 100m shallow depth ICAL (SICAL) detector. The cosmic muons would have to be detected in a veto detector with an efficiency of 99.99% in order to have the same level of muon background leaking undetected through the veto detector as at the 1 km depth underground site. However, an additional background arises from interactions of cosmic muons with the rock. Since the neutral particles produced in such interactions can pass through the veto detector without any interaction, they can possibly mimic neutrino events in the ICAL. In this paper, the results of a GEANT4 based simulation study to estimate the background signals due to muon induced interactions with the rock for the SICAL is presented.
机译:铁量热计(ICAL)探测器在印度根据天文台(间接宾语)计划设置在一个地下洞穴岩石上覆岩层的超过1公里。减少了宇宙μ介子通量10 ~ 6倍在海平面。篇文章中,我们检查100的可能性浅深度ICAL(调查)检测器。在否决μ介子必须检测探测器的效率为99.99%相同级别的μ介子背景泄漏吗1通过否决探测器未被发现公里深度地下站点。背景来自宇宙的相互作用μ介子的岩石。在这样的交互可以通过生产否决探测器没有任何互动,他们能模仿ICAL中微子事件。本文基于GEANT4的结果模拟研究来估计背景由于子诱导相互作用的信号岩石的调查。

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