JpGU-AGU Joint Meeting 2017

講演情報

[EE]Eveningポスター発表

セッション記号 P (宇宙惑星科学) » P-PS 惑星科学

[P-PS02] [EE] Small Bodies: Exploration of the Asteroid Belt and the Solar System at Large

2017年5月22日(月) 17:15 〜 18:30 ポスター会場 (国際展示場 7ホール)

[PPS02-P20] Detectability Performance of Thermal Infrared Imager TIR on Hayabusa2

*岡田 達明1,8福原 哲哉2田中 智1田口 真2荒井 武彦3千秋 博紀4小川 佳子5出村 裕英5北里 宏平5中村 良介6神山 徹6関口 朋彦7長谷川 直1松永 恒雄3和田 武彦1今村 剛8滝田 隼1,8坂谷 尚哉9堀川 大和1,10遠藤 憲5ヘルバート ヨルン11ミュラー トマス12ハゲルマン アクセル13 (1.宇宙航空研究開発機構宇宙科学研究所、2.立教大学、3.国立環境研究所、4.千葉工業大学、5.会津大学、6.産業技術総合研究所、7.北海道教育大学、8.東京大学、9.明治大学、10.総合研究大学院大学、11.ドイツ航空宇宙センター、12.マックスプランク地球外物理学研究所、13.オープン大学)

キーワード:asteroid exploration, Hayabusa2, Thermo-physical property, thermal infrared imager, thermal inertia

The thermal infrared imager TIR [1] onboard the JAXA’s second asteroid explorer Hayabusa2 is a thermal camera based on two-dimensional uncooled micro-bolometer array, inherited from the Longwave Infrared Camera (LIR) on Akatsuki (formerly PLANET-C) Venus climate orbiter [2]. TIR is to observe the thermal emission from the target body, C-type near-Earth asteroid 162173 Ryugu (formerly 1999JU3) to investigate its surface thermo-physical properties that are strongly related to representative grain size and porosity. Such information enables us to understand its formation process and surface evolution processes. The data from TIR will be used to select the landing sites for sample collection and for the surface lander and rovers both from scientific and technical viewpoints. Typical grain size derived from the thermal inertia map determined by TIR data is scientifically essential to select the suitable sites for collection by the sampling device and for the analysis of returned samples. Typical boulder abundance and predicted thermal environments are technically essential for safety and hazard-free landing operations.
TIR has been checked in flight by observations of the deep sky as backgrounds, and of the Earth and the Moon as known targets during the Earth swing-by operation campaign. The first and longest distance observation of the Earth and the Moon was carried out on 14 October 2015, at about 2 x 107 km from the Earth. There were opportunities that TIR observed the Earth and the moon 7 times before and 18 times after the Earth Swing-by on 3 December 2015. During that period, the distance changed by two orders of magnitude, and the distance dependency of TIR response is now derived for the thermal brightness of the Earth and the Moon. The dependency is inversely proportional to the square of distance, for the diameter of the Moon corresponding to 0.2 to 6 pixels of TIR images. From this trend, the detection limit (> 10 DN for the target body) is at about 1.5 x 108 km for the Moon [3].
This result indicates the possible detection of unknown asteroids closely passing by the Hayabusa2 spacecraft. For the 100 m sized asteroid of C-type (its geometric albedo ~ 0.05), the detection limit (> 10 DN) is estimated about 2 x 103 km from the spacecraft. During April to June in 2017, Hayabusa2 will be around the L5 point of the sun-earth Lagrange point, gravitationally meta-stable point, so that unknown small bodies may be detected if they pass within such a distance. Before arrival at asteroid Ryugu which is of rounded shape and with diameter of 0.88 km, it will be detected at 1.5 x 104 km distance. Ryugu will be investigated during the approach phase and its light-curve of brightness temperature will be investigated before arrival. Around Ryugu, TIR is estimated to detect small moons encircling Ryugu at Home Position (20 km from the target asteroid) if they have diameter larger than 1 m, and their orbits are traced by continual imags taken with TIR.
Acknowledgments
The authors appreciate Hayabusa2 Project team for their continuous support. This research is partly supported by the Grant-in-Aid for Scientific Research (B), No. 26287108, of the Japan Society for the Promotion of Science.
References
[1] Okada T. et al. (2016) Space Sci. Rev. doi:10.1007/ s11214-016-0286-8.
[2] Fukuhara T. et al. (2011) Earth Planets Space, 63, 1009-1018.
[3] Okada T. et al. (2017) Lunar Planet. Sci. Conf. 48, #1818.