在宇宙射线背景中寻找超高频中微子

Abha R. Khakurdikar, Washington R. Carvalho. Jr, Jörg R. Hörandel
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摘要

探测超高能(UHE)中微子的主要挑战是在超高能核引发的阵雨背景中区分中微子引发的阵雨。中微子引发的阵雨与强子引发的阵雨具有不同的特征,因为中微子比强子更深地穿透大气层。本研究重点模拟了天顶角超过75^\circ$的高倾斜中微子诱发的阵雨,探索了从1\text{EeV}$到120 \text{EeV}$的广泛能量范围。这些模拟阵雨与每个天顶角对应的相互作用深度范围各不相同,这给探测带来了不同的挑战。我们的方法利用射电天线的定时数据来计算中微子和原子核诱发的大范围空气阵雨的阵雨前沿。此外,我们还结合了水切伦科夫探测器获得的信号,以及在水切伦科夫探测器和射电天线中记录信号的台站的空间分布。我们的目标是通过利用吉尼杂质法的决策树分类器,对中微子诱发的辐照和源于原子核的背景事件进行分类。我们的框架在分离中微子和背景方面具有极高的准确性。这项研究的发现为超高辐射中微子探测领域带来了重大进展,在超高辐射原子核的复杂背景中揭示了与这些难以捉摸的粒子相关的天体物理现象。
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Search for UHE neutrinos in the background of cosmic rays
The main challenge in detecting ultra-high energy (UHE) neutrinos is discriminating a neutrino-induced shower in the background of showers initiated by ultra-high energy nuclei. The resulting shower development from neutrinos exhibits different characteristics from hadron-induced showers because neutrinos penetrate the atmosphere more deeply than hadrons. This study focuses on simulations of highly inclined neutrino-induced showers above $75^\circ$ zenith angles, exploring an extensive energy range from $1 \text{EeV}$ to $120 \text{EeV}$. These simulated showers have different ranges of interaction depths corresponding to each zenith angle, presenting diverse detection challenges. Our methodology utilises timing data from radio antennas for the shower front calculation for extensive air showers induced by neutrinos and nuclei. Furthermore, we incorporate signals obtained from Water Cherenkov detectors and the spatial distribution of stations registering signals in both Water Cherenkov detectors and radio antennas. We aim to classify neutrino-induced showers and background events stemming from nuclei by harnessing a decision tree classifier employing the Gini impurity method. Our framework yields excellent accuracy for separating the neutrinos from the background. The findings of this study offer significant advancements in the domain of UHE neutrino detection, shedding light on astrophysical phenomena associated with these elusive particles amidst the complex background of UHE nuclei.
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