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arXiv 2011.10317astro-ph.IM
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Hitomi卫星硬X射线成像仪在轨仪器背景的起源

Origin of the in-orbit instrumental background of the Hard X-ray Imager onboard Hitomi

Kouichi Hagino, Hirokazu Odaka, Goro Sato, Tamotsu Sato, Hiromasa Suzuki, Tsunefumi Mizuno, Madoka Kawaharada, Masanori Ohno, Kazuhiro Nakazawa, Shogo B. Kobaya… 展开作者

Kouichi Hagino, Hirokazu Odaka, Goro Sato, Tamotsu Sato, Hiromasa Suzuki, Tsunefumi Mizuno, Madoka Kawaharada, Masanori Ohno, Kazuhiro Nakazawa, Shogo B. Kobayashi, Hiroaki Murakami, Katsuma Miyake, Makoto Asai, Tatsumi Koi, Greg Madejski, Shinya Saito, Dennis H. Wright, Teruaki Enoto, Yasushi Fukazawa, Katsuhiro Hayashi, Jun Kataoka, Junichiro Katsuta, Motohide Kokubun, Philippe Laurent, Francois Lebrun, Olivier Limousin, Daniel Maier, Kazuo Makishima, Kunishiro Mori, Takeshi Nakamori, Toshio Nakano, Hirofumi Noda, Masayuki Ohta, Rie Sato, Hiroyasu Tajima, Hiromitsu Takahashi, Tadayuki Takahashi, Shin'ichiro Takeda, Takaaki Tanaka, Yukikatsu Terada, Hideki Uchiyama, Yasunobu Uchiyama, Shin Watanabe, Kazutaka Yamaoka, Yoichi Yatsu, Takayuki Yuasa

AI总结:

本文利用Hitomi卫星HXI的多层探测器观测数据,确定各层在轨背景分别由低能电子、反照中子和质子诱发放射性活化主导,并通过蒙特卡洛模拟定量验证,提出增加电子屏蔽体以降低背景。

摘要:

理解并降低在轨仪器背景对于在硬X射线天文观测中实现高灵敏度至关重要。Hitomi卫星上的硬X射线成像仪(HXI)的观测数据为背景成分提供了有用信息,这得益于其具有不同原子序数的多层结构:HXI由四层Si(Z = 14)探测器叠层和一层CdTe(Z = 48, 52)探测器组成,并被井型BGO(Bi4Ge3O12)有源屏蔽体包围。基于观测数据,推断顶层Si层、下面三层Si层和CdTe层的背景分别由不同成分主导,即低能电子、反照中子和质子诱发放射性活化。对HXI在轨背景的蒙特卡洛模拟很好地重现了每一层的观测背景谱,从而定量验证了上述假设。此外,我们建议加入电子屏蔽体以降低背景。

英文摘要:

Understanding and reducing the in-orbit instrumental backgrounds are essential to achieving high sensitivity in hard X-ray astronomical observations. The observational data of the Hard X-ray Imager (HXI) on board the Hitomi satellite provides useful information on the background components, owing to its multi-layer configuration with different atomic numbers: the HXI consists of a stack of four layers of Si (Z = 14) detectors and one layer of CdTe (Z = 48, 52) detector surrounded by well-type BGO (Bi4Ge3O12) active shields. Based on the observational data, the backgrounds of top Si layer, the three underlying Si layers, and the CdTe layer are inferred to be dominated by different components, namely, low-energy electrons, albedo neutrons, and proton-induced radioactivation, respectively. Monte Carlo simulations of the in-orbit background of the HXI reproduce the observed background spectrum of each layer well, thereby verifying the above hypothesis quantitatively. In addition, we suggest the inclusion of an electron shield to reduce the background.

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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