SuperTIGER Ultra-Heavy Galactic Cosmic Ray Atmospheric Propagation Corrections and Uncertainty Analysis

B. Rauch, N. Walsh, W. Zober
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Abstract

The SuperTIGER (Super Trans-Iron Galactic Element Recorder) balloon-borne ultra-heavy galactic cosmic-ray (UHGCR) detector has flown twice in the stratosphere over Antarctica at altitudes up to ∼ 130,000 ft. Corrections for propagating through the last ∼ 0.5% of the atmosphere are based on those developed for the preceding TIGER instrument. Changes due to nuclear interactions are determined by finding top of the atmosphere (TOA) elemental abundances that yield those measured in the instrument after solving networks of equations for all elements with partial and total charge changing cross sections stepping through fine slabs of material. Varying rates of energy loss in the atmosphere for different elements yield different TOA minimum energies for the acrylic Cherenkov detector threshold ( ∼ 350 MeV/nuc). TOA abundances corrected for nuclear interactions for each element are scaled with the fraction of the integral energy spectrum for its TOA minimum energy, using the iron spectrum for the UHGCR. Statistical uncertainties are derived at the TOA by shifting the abundance of each element individually up and down by the measured uncertainty in the instrument and calculating the TOA abundance of that element. Systematic uncertainties previously were estimated by simultaneously shifting the partial and then the total cross sections for all elements up and down by their uncertainties and finding TOA abundances compared to the nominal values. Here we present a Monte Carlo study of the systematic impact of simultaneously randomly varying atmospheric propagation parameters over many trials to find the normal range of variation in the resulting TOA element abundances. Total
超级老虎超重银河宇宙射线大气传播修正与不确定度分析
SuperTIGER(超级跨铁银河元素记录仪)气球载超重银河宇宙射线(UHGCR)探测器已经在南极洲上空的平流层飞行了两次,高度高达~ 130,000英尺。通过最后~ 0.5%大气传播的修正是基于先前TIGER仪器开发的修正。核相互作用引起的变化是通过寻找大气顶部(TOA)元素丰度来确定的,这些丰度是在解决所有元素的方程网络后产生的,这些元素具有部分和总电荷变化的横截面,穿过细板的材料。不同元素在大气中不同的能量损失率产生不同的丙烯酸切伦科夫探测器阈值的TOA最小能量(~ 350 MeV/nuc)。对每种元素的核相互作用校正后的TOA丰度用其TOA最小能量的积分能谱的分数进行缩放,使用UHGCR的铁谱。统计不确定度是通过仪器中测量的不确定度将每个元素的丰度单独上下移动并计算该元素的TOA丰度而得出的。系统不确定度以前是通过同时将所有元素的部分截面和总截面向上和向下移动,并与标称值比较TOA丰度来估计的。在这里,我们提出了一个蒙特卡罗研究,在许多试验中同时随机变化的大气传播参数的系统影响,以找到所产生的TOA元素丰度的正常变化范围。总计
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