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arXiv 2106.12980astro-ph.IM
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地下实验室稀有事件搜索实验用gamma ray、宇宙μ子和剩余中子本底通量的测量

Measurements of gamma ray, cosmic muon and residual neutron background fluxes for rare event search experiments at an underground laboratory

Sayan Ghosh, Shubham Dutta, Naba Kumar Mondal, Satyajit Saha

摘要:

环境辐射背景的穿透宇宙射线粒子和岩石材料中存在的放射性核素的贡献已被测量在地下实验室位于矿井内的555米深。该实验室的设立旨在探索稀有事件搜寻过程,如直接暗物质搜寻、无中微子双β衰变、轴子搜寻、超新星中微子探测等,这需要对辐射环境的性质和范围有具体的了解,以便评估敏感度范围,并为有针对性的实验制定减少敏感度的计划。伽马射线背景主要由原始放射性核素及其衰变链产物贡献,已在实验室内测量,发现$E_γ\lesssim 3 \,{\rm MeV}$主要由岩石放射性贡献。还评价了用于实验的这些残留伽马射线的屏蔽。在实验室内用大面积塑料闪烁体望远镜测量的宇宙μ子通量为:$(2.051 \pm 0.142 \pm 0.009) \times 10^{-7}\, {\rm cm}^{-2}.{\rm sec}^{-1}$,与模拟结果相当吻合。测量了放射性中子的中子本底通量,发现:无阈切时为$(1.61 \pm 0.03) \times 10^{-4} \, {\rm cm}^{-2}.{\rm sec}^{-1}$。对辐射中子和宇宙中子进行了详细的GEANT4模拟。研究了围岩和洞壁内两种类型中子的多次散射效应,发现放射性中子的结果与实验结果相当吻合。据报道,宇宙起源的中子所贡献的中子通量是能量阈值的函数。

英文摘要:

Ambient radiation background contributed by the penetrating cosmic ray particles and the radionuclides present in the rock materials have been measured at an underground laboratory located inside a mine at 555 m depth. The laboratory is being set up to explore rare event search processes, such as direct dark matter search, neutrinoless double beta decay, axion search, supernova neutrino detection, etc., that require specific knowledge of the nature and extent of the radiation environment in order to assess the sensitivity reach and also to plan for its reduction for the targeted experiment. The gamma ray background, which is mostly contributed by the primordial radionuclides and their decay chain products, have been measured inside the laboratory and found to be dominated by rock radioactivity for $E_γ\lesssim 3 \,{\rm MeV}$. Shielding of these residual gamma rays for the experiment was also evaluated. The cosmic muon flux, measured inside the laboratory using large area plastic scintillator telescope, was found to be: $(2.051 \pm 0.142 \pm 0.009) \times 10^{-7}\, {\rm cm}^{-2}.{\rm sec}^{-1}$, which agrees reasonably well with simulation results. The neutron background flux has been measured for the radiogenic neutrons and found to be: $(1.61 \pm 0.03) \times 10^{-4} \, {\rm cm}^{-2}.{\rm sec}^{-1}$ for no threshold cut. Detailed GEANT4 simulation for the radiogenic neutrons and the cosmogenic neutrons have been carried out. Effects of multiple scattering of both the types of neutrons within the surrounding rock and the cavern walls were studied and the results for the radiogenic neutrons are found to be in reasonable agreement with experimental results. Neutron fluxes contributed by those neutrons of cosmogenic origin have been reported as function of the energy threshold.

机构、总结、中文摘要均由AI分析而来,可能存在错误,请以论文正文为准。

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