Japan Geoscience Union Meeting 2015

Presentation information

Oral

Symbol M (Multidisciplinary and Interdisciplinary) » M-IS Intersection

[M-IS35] Why is this planet to be the Earth? -the role of water

Sun. May 24, 2015 9:00 AM - 10:45 AM 201A (2F)

Convener:*Nobukazu Seama(Department of Planetology, Graduate School of Science, Kobe University), Yoshiyuki Tatsumi(Institute for Research on Earth Evolution, Japan Agency for Marine-Earth Science and Technology), Keiji Ohtsuki(Graduate School of Science, Kobe University), Takashi Nakagawa(JAMSTEC/MAT), Ikuo Katayama(Department of Earth and Planetary Systems Science, Hiroshima University), Gou Fujie(Japan Agency for Marine-Earth Science and Technology), Akiko Nakamura(Graduate School of Science, Kobe University), Chair:Keiji Ohtsuki(Graduate School of Science, Kobe University), Nobukazu Seama(Department of Planetology, Graduate School of Science, Kobe University)

9:30 AM - 9:45 AM

[MIS35-03] Exploring the origin of Earth's water by the Hayabusa-2 near-infrared spectrometer

*Kohei KITAZATO1, Takahiro IWATA2, Masanao ABE2, Makiko OHTAKE2, Takahiro HIROI3, Tomoki NAKAMURA4, Mutsumi KOMATSU5, Tomoko ARAI6, Aiko NAKATO2, Takahito OHSAWA7, Yusuke NAKAUCHI5, Sei-ichiro WATANABE8 (1.University of Aizu, 2.JAXA/ISAS, 3.Brown University, 4.Tohoku University, 5.Graduate University for Advanced Studies, 6.Chiba Institute of Technology, 7.JAEA, 8.Nagoya University)

Keywords:Hayabusa-2, asteroids, water, near-infrared spectroscopy

NIRS3, the near-infrared spectrometer onboard the Hayabusa-2 spacecraft, is a remote-sensing instrument to obtain the reflectance spectra including 3-μm absorption features due to structural OH ions and H2O molecules. In 2018-2019, we are planning to perform proximity observations of a near-Earth C-type asteroid 1999JU3 using NIRS3 and to reveal the distribution of hydrated minerals on the asteroid surface. Recently, the results indicating the presence of internal water ice for C-type asteroids were reported from ground-based observations. Hence, there is a possibility that the contribution of C-type asteroids to formation of Earth's ocean becomes larger than that predicted so far. It is required to understand the behavior of water in the aqueous alteration to verify the internal water ice. Thus, NIRS3 aims at obtaining information about the aqueous alteration discerning the secondary alteration effects such as thermal dehydration and space weathering from observations of the crater formed by the artificial impact experiment. In this presentation, we introduce the expected outcome of NIRS3 based on the current knowledge of C-type asteroids.