Revisiting Jovian-resonance Induced Chondrule Formation

1M. Nagasawa, 2K. K. Tanaka, 2H. Tanaka, 3T. Nakamoto, 4H. Miura, 5T. Yamamoto
1Interactive Research Center of Science, Tokyo Institute of Technology, 2-12-1 Ookayama, Meguro-ku, Tokyo 152-8551, Japan
2Institute of Low Temperature Science, Hokkaido University, Kita-19, Nishi-8, Kita-ku, Sapporo 060-0819, Japan
3Department of Earth and Planetary Sciences, Tokyo Institute of Technology, 2-12-1 Ookayama, Meguro-ku, Tokyo 152-8551, Japan
4Graduate School of Natural Sciences, Nagoya City University, 1 Yamanohata, Mizuho-cho, Mizuho-ku, Nagoya 467-8501, Japan
5Center for Planetary Science, Kobe University, 7-1-48 Minamimachi, Minatojima, Chuo-ku, Kobe 650-0047, Japan

It is proposed that planetesimals perturbed by Jovian mean-motion resonances are the source of shock waves that form chondrules. It is considered that this shock-induced chondrule formation requires the velocity of the planetesimal relative to the gas disk to be on the order of gsim 7 km s–1 at 1 AU. In previous studies on planetesimal excitation, the effects of Jovian mean-motion resonance together with the gas drag were investigated, but the velocities obtained were at most 8 km s–1 in the asteroid belt, which is insufficient to account for the ubiquitous existence of chondrules. In this paper, we reexamine the effect of Jovian resonances and take into account the secular resonance in the asteroid belt caused by the gravity of the gas disk. We find that the velocities relative to the gas disk of planetesimals a few hundred kilometers in size exceed 12 km s–1, and that this is achieved around the 3:1 mean-motion resonance. The heating region is restricted to a relatively narrowband between 1.5 AU and 3.5 AU. Our results suggest that chondrules were produced effectively in the asteroid region after Jovian formation. We also find that many planetesimals are scattered far beyond Neptune. Our findings can explain the presence of crystalline silicate in comets if the scattered planetesimals include silicate dust processed by shock heating.

Reference
Nagasawa M, Tanaka KK, Tanaka H, Nakamoto T, Miura H, Yamamoto T (2014) Revisiting Jovian-resonance Induced Chondrule Formation. The Astrophysical Journal Letters 794, 1, L7
Link to Article [doi:10.1088/2041-8205/794/1/L7]

Trajectory, orbit, and spectroscopic analysis of a bright fireball observed over Spain on April 13, 2013

1,2José M. Madiedo et al. (>10 Authors)*
1Departamento de Física Atómica, Molecular y Nuclear, Facultad de Física, Universidad de Sevilla, 41012 Sevilla, Spain
2Facultad de Ciencias Experimentales, Universidad de Huelva, 21071 Huelva, Spain
*Find the extensive, full author and affiliation list on the publishers website

We currently do not have a copyright agreement with this publisher and cannot display the abstract here

Reference
José M. Madiedo et al. (2014) Trajectory, orbit, and spectroscopic analysis of a bright fireball observed over Spain on April 13, 2013. Astronomy&Astrophysics 569 (in Press)
Link to Article [http://www.aanda.org/articles/aa/abs/2014/09/aa22120-13/aa22120-13.html]