首页> 外文期刊>Nuclear Instruments & Methods in Physics Research. Section A, Accelerators, Spectrometers, Detectors and Associated Equipment >Near-space operation of compact CsI, CLYC, and CeBr_3 sensors: Results from two high-altitude balloon flights
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Near-space operation of compact CsI, CLYC, and CeBr_3 sensors: Results from two high-altitude balloon flights

机译:紧凑型CsI,CLYC和CeBr_3传感器的近空间操作:两次高空气球飞行的结果

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Three different types of gamma-ray sensors (CsI, CLYC, and CeBr3) were flown on balloon flights as hosted payloads. Two CsI sensors were flown from a September 2014 flight from Fort Sumner, New Mexico for 18 h; CLYC and CeBr3sensors were flown from Antarctica in December 2016 for 22 days. The data from these flights were used to test and characterize the operation of these sensors in a near-space environment. All sensors returned excellent data. Gamma rays, neutrons, and energetic galactic cosmic rays (GCRs) were measured. Expected atmospheric features, such as the Regener–Pfotzer maximum, were observed, and gamma-ray line emission from materials near the sensors, as well as atmospheric oxygen and nitrogen, were detected. The measured data were compared to simulations of energetic protons, neutrons, and 0.511 MeV gamma rays produced by GCR interactions with the atmosphere. While the simulated protons and neutrons generally matched the data, there were fewer simulated 0.511 MeV gamma rays than measured with the data. This mismatch is likely due to additional 0.511 MeV gamma rays produced in material near the sensors that were not taken into account in the simulations. Discussion is provided for how these types of measurements in space-based missions can be used to characterize upper atmospheric densities at planets with dense atmospheres like the Earth.
机译:三种不同类型的伽马射线传感器(CsI,CLYC和CeBr3)在气球飞行中作为宿主有效载荷飞行。 2014年9月,从新墨西哥州萨姆纳堡起飞的两个CsI传感器飞行了18小时; CLYC和CeBr3传感器于2016年12月从南极飞行了22天。这些飞行的数据用于测试和表征这些传感器在近太空环境中的运行。所有传感器均返回了出色的数据。测量了伽马射线,中子和高能银河宇宙射线(GCR)。观察到了预期的大气特征,例如Regener–Pfotzer最大值,并检测了传感器附近材料发出的伽马射线线以及大气中的氧气和氮气。将测得的数据与高能质子,中子和GCR与大气相互作用产生的0.511 MeV伽马射线的模拟进行了比较。尽管模拟的质子和中子通常与数据匹配,但模拟的0.511 MeV伽玛射线比使用数据测得的少。这种失配很可能是由于在传感器附近的材料中产生了额外的0.511 MeV伽马射线所致,而在模拟中并未考虑这些射线。讨论了如何将天基任务中的这些类型的测量结果用于表征大气层密度较高的行星(如地球)的高层大气密度。

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