Japan Geoscience Union Meeting 2016

Presentation information

Oral

Symbol M (Multidisciplinary and Interdisciplinary) » M-GI General Geosciences, Information Geosciences & Simulations

[M-GI22] Development of computational sciences on planetary formation, evolution and surface environment

Tue. May 24, 2016 9:00 AM - 10:30 AM A07 (APA HOTEL&RESORT TOKYO BAY MAKUHARI)

Convener:*Junichiro Makino(RIKEN AICS), Yoshi-Yuki Hayashi(Department of Planetology/CPS, Graduate School of Science, Kobe University), Shigeru Ida(Department of Earth and Planetary Science, Graduate School of Science and Technology, Tokyo Institute of Technology), Yuri Aikawa(Center for Computational Sciences, University of Tsukuba), Masaki Ogawa(Division of General Systems Studies, Graduate School of Arts and Sciences, University of Tokyo), Masayuki Umemura(Center for Computational Sciences, University of Tsukuba), Chair:Shigeru Ida(Department of Earth and Planetary Science, Graduate School of Science and Technology, Tokyo Institute of Technology)

9:15 AM - 9:30 AM

[MGI22-02] Complex organic molecules in star- and planet-forming regions

*Yuri Aikawa1 (1.Center for Computational Sciences, University of Tsukuba)

Keywords:astrochemistry, formation of star and planetary systems

Complex organic molecules (COMs) are intensively searched for around solar-mass protostars in recent years. For example, glycolaldehyde (HCOCH2OH), the simplest sugar, was detected around IRAS16293 in the ALMA Science Verification program (Jorgensen et al. 2012). COMs are expected to be more abundant in ice mantles than in the gas phase, because their sublimation temperature is relatively high, and because grain-surface reactions would play significant roles in their formation. COMs in star-forming regions, especially in ice mantle, could be an important reservoir of organic compounds in the planetary-system formation and/or mother molecules of prebiotic molecules. It is, however, very difficult to directly observe COMs in ice mantle. Combination of line observations (of gaseous COMs) and theoretical modeling of gas-grain chemistry is thus needed to understand the formation and destruction of COMs in the gas phase and ice mantle. Computational modeling efforts include (i) radiation hydrodynamics of star formation, (ii) gas-grain chemical network calculations and (iii) physical/chemical calculations to determine the rates and efficiencies of various chemical reactions and micro processes. In this contribution, I will review recent progresses, especially in (ii) and (iii).