论文标题
贝加尔的海岸阴影效应
Shore Shadow Effect in Baikal
论文作者
论文摘要
一级宇宙射线引起的延长空气淋浴(EAS)中的单个带电颗粒的测量提供了重要的区分参数,以识别宇宙主要颗粒的化学组成。对于像Baikal-GVD这样的中微子望远镜实验,水下隆隆通量的估计对于研究大气压非常重要。在本文中,提出了基于GEANT4的模拟,以估计以Baikal-GVD为例的大气下助力通量。 Baikal-GVD实验在贝加尔湖的位置提供了一个独特的机会,可以研究Muons通过其北岸和水的通道。与从南部到达的人相比,从北方到达的兆恩斯将失去更多的能量。在Geant4几何形状中还模拟了北岸的近似值,并将模拟结果与NT-96检测器的测量结果进行了比较。模拟的结果与NT-96中测量值中观察到的海岸阴影一致。这种方法也可以用来在水,冰,地球等物质中长距离传播诸如Corsika之类的发电机的MUON,以在此类实验中进行模拟。
The measurement of the individual charged particles especially muons in an extended air shower (EAS) resulting from primary cosmic rays provides important distinguishing parameters to identify the chemical composition of the cosmic primary particles. For Neutrino Telescope experiments like Baikal-GVD, the estimation of underwater muon flux is of importance to study atmospheric muons. In this paper, a GEANT4-based simulation is presented to estimate the atmospheric muon flux underwater taking Baikal-GVD as an example. The location of the Baikal-GVD experiment at Lake Baikal provides a unique opportunity to study the passage of muons through its northern shore and the water. The muons arriving from the north direction will lose more energy as compared to those arriving from the south. An approximation for the northern shore is also simulated in the GEANT4 geometry and the results of the simulation are compared with the measurements from the NT-96 detector. The results of the simulations are consistent with the shore shadow observed in the measurements in the NT-96. This approach can also be used to propagate the muons from generators like CORSIKA through long distances in matter like water, ice, earth, etc. for simulations in such experiments.