The surface composition of asteroid 162173 Ryugu from Hayabusa2 near-infrared spectroscopy

K. Kitazato(University of Aizu), R. E. Milliken(Brown University), Takahiro Iwata(The Graduate University for Advanced Studies, SOKENDAI), Masanao Abe(The Graduate University for Advanced Studies, SOKENDAI), M. Ohtake(The Graduate University for Advanced Studies, SOKENDAI), Shuji Matsuura(Kwansei Gakuin University), T. Arai(Ashikaga University), Yusuke Nakauchi(Japan Aerospace Exploration Agency), T. Nakamura(Tohoku University), M. Matsuoka(Japan Aerospace Exploration Agency), H. Senshu(Chiba Institute of Technology), Naru Hirata(University of Aizu), T. Hiroi(Brown University), C. Pilorget(Université Paris-Sud), R. Brunetto(Université Paris-Sud), F. Poulet(Université Paris-Sud), L. Riu(Japan Aerospace Exploration Agency), Jean‐Pierre Bibring(Université Paris-Sud), D. Takir(Johnson Space Center), D. L. Domingue(Planetary Science Institute), F. Vilas(Planetary Science Institute), M. A. Barucci(Université de Versailles Saint-Quentin-en-Yvelines), D. Perna(Université de Versailles Saint-Quentin-en-Yvelines), E. Palomba(Institute for Space Astrophysics and Planetology), A. Galiano(Institute for Space Astrophysics and Planetology), Kohji Tsumura(Tokyo City University), Takahito Osawa(Japan Atomic Energy Agency), M. Komatsu(The Graduate University for Advanced Studies, SOKENDAI), Aiko Nakato(Japan Aerospace Exploration Agency), T. Arai(Ashikaga University), N. Takato(The Graduate University for Advanced Studies, SOKENDAI), Tsuneo Matsunaga(National Institute for Environmental Studies), Y. Takagi(Aichi Toho University), Koji Matsumoto(The Graduate University for Advanced Studies, SOKENDAI), Toru Kouyama(National Institute of Advanced Industrial Science and Technology), Y. Yokota(Japan Aerospace Exploration Agency), Eri Tatsumi(The University of Tokyo), Naoya Sakatani(Japan Aerospace Exploration Agency), Yukio Yamamoto(The Graduate University for Advanced Studies, SOKENDAI), Tatsuaki Okada(Japan Aerospace Exploration Agency), Seiji Sugita(The University of Tokyo), Rie Honda(Kōchi University), Tomokatsu Morota(Nagoya University), Shingo Kameda(Rikkyo University), Hirotaka Sawada(Japan Aerospace Exploration Agency), Chikatoshi Honda(University of Aizu), Manabu Yamada(Chiba Institute of Technology), Hidehiko Suzuki(Meiji University), Kazuo Yoshioka(The University of Tokyo), Masahiko Hayakawa(Japan Aerospace Exploration Agency), Kazunori Ogawa(Kobe University), Y. Cho(The University of Tokyo), K. Shirai(Japan Aerospace Exploration Agency), Yuri Shimaki(Japan Aerospace Exploration Agency), Naoyuki Hirata(University of Aizu), Akira Yamaguchi(The Graduate University for Advanced Studies, SOKENDAI), Naoko Ogawa(Japan Aerospace Exploration Agency), Fuyuto Terui(Japan Aerospace Exploration Agency), T. Yamaguchi(Mitsubishi Electric (Japan)), Yuto Takei(Japan Aerospace Exploration Agency), Takanao Saiki(Japan Aerospace Exploration Agency), Satoru Nakazawa(Japan Aerospace Exploration Agency), S. Tanaka(The Graduate University for Advanced Studies, SOKENDAI), Makoto Yoshikawa(The Graduate University for Advanced Studies, SOKENDAI), Sei‐ichiro Watanabe(Japan Aerospace Exploration Agency), Yuichi Tsuda(The Graduate University for Advanced Studies, SOKENDAI)
Science
March 19, 2019
Cited by 358Open Access
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Abstract

Hayabusa2 at the asteroid Ryugu Asteroids fall to Earth in the form of meteorites, but these provide little information about their origins. The Japanese mission Hayabusa2 is designed to collect samples directly from the surface of an asteroid and return them to Earth for laboratory analysis. Three papers in this issue describe the Hayabusa2 team's study of the near-Earth carbonaceous asteroid 162173 Ryugu, at which the spacecraft arrived in June 2018 (see the Perspective by Wurm). Watanabe et al. measured the asteroid's mass, shape, and density, showing that it is a “rubble pile” of loose rocks, formed into a spinning-top shape during a prior period of rapid spin. They also identified suitable landing sites for sample collection. Kitazato et al. used near-infrared spectroscopy to find ubiquitous hydrated minerals on the surface and compared Ryugu with known types of carbonaceous meteorite. Sugita et al. describe Ryugu's geological features and surface colors and combined results from all three papers to constrain the asteroid's formation process. Ryugu probably formed by reaccumulation of rubble ejected by impact from a larger asteroid. These results provide necessary context to understand the samples collected by Hayabusa2, which are expected to arrive on Earth in December 2020. Science , this issue p. 268 , p. 272 , p. 252 ; see also p. 230


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