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Planet ¤Î¥Ð¥Ã¥¯¥¢¥Ã¥×(No.75)


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Schedule & History

2020ǯÅÙ 2019ǯÅÙ 2018ǯÅÙ 2017ǯÅÙ 2016ǯÅÙ 2015ǯÅÙ 2014ǯÅÙ

ÆüÄøÈ¯É½¥¿¥¤¥È¥ëRemarksôÅö
Á°´ü Âè1²ó 4/15 15:00-All membersSelf-introduction¸Å²È
Á°´ü Âè2²ó 4/22 15:00-All membersSelf-introduction¸Å²È
Á°´ü Âè3²ó 5/13 14:00-Teruyuki Hirano (ABC)Near Infrared Spectroscopy as a Powerful Tool to Probe Exoplanetary Systems14:00¸Å²È
Á°´ü Âè4²ó 5/20 15:00-Ryuki Hyodo (ISAS/JAXA)Planetesimal formation -- Around the snow line and the "no-drift" mechanism¹ÓÀî
Á°´ü Âè5²ó 6/17 15:00-Riouhei Nakatani (RIKEN)Photoevaporation of Protoplanetary Disks: Revisiting the Underlying Physics and the Gravitational Radius¹â¶¶
Á°´ü ÂèXX²ó 6/24 15:00-Hiroaki Kaneko (titech)À±Ìî
5/20 Ryuki Hyodo (ISAS/JAXA), Planetesimal formation -- Around the snow line and the "no-drift" mechanism
Forming planetesimals in protoplanetary disks is a major challenge in our current understanding of planet formation. Icy pebbles mixed with silicate dust formed at the outer disk drift inward due to the gas drag. We performed 1D diffusion-advection simulations that include the back-reaction (the inertia) to radial drift and diffusion of icy pebbles and silicate dust, ice sublimation, the release of silicate dust, and their recycling through the recondensation and sticking onto pebbles outside the snow line. In this talk, I will present how icy pebbles and silicate dust pile up around the snow line. I also report a new mechanism, the ¡Èno-drift¡É runaway pile-up, that leads to a runaway accumulation of pebbles in disks, thus favoring the formation of planetesimals by streaming and/or gravitational instabilities. References: Hyodo et al. 2021 A&A, 646, A14; Ida et al. 2021 A&A, 646, A13; Hyodo et al. 2021 A&A, 645, L9
6/17 Riouhei Nakatani (RIKEN), Photoevaporation of Protoplanetary Disks: Revisiting the Underlying Physics and the Gravitational Radius
In a variety of astrophysical problems, we find a situation where a clump of gas is irradiated by ultraviolet and X-ray from radiation sources. An important outcome of this process is that excessive photon energy goes into the heat for the gas, which results in driving winds. This wind-driving process, termed photoevaporation, is essential to determine the fate of the irradiated objects. Protoplanetary disks are one of such objects. The stellar UV and X-ray can yield sufficiently high mass-loss rates that can disperse the disks within 10 Myr. The gravitational radius is often used as a criterial radius above which the photoheated gas is possible to escape from the gravitational binding of the host star. However, the gravitational radius is derived from dimensional analysis and thus does not provide a definite criterion regarding the escape capability. We have recently developed an analytic model for photoevaporation in a first-principles approach. It is of use to understand the basic physics operating in the vicinity of the wind-launching points. Our model naturally sets a gravitational-radius-like criterion, which is fundamentally different from the gravitational radius in origin. In this talk, I first present the analytic model. Then, the model aside, I introduce our recent numerical works regarding photoevaporation of protoplanetary disks hosted by intermediate-mass stars.