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Schedule & History

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ÆüÄøȯɽ¥¿¥¤¥È¥ëRemarks
Á°´ü Âè1²ó 4/11 14:30-Shinsuke Takasao3D MHD simulations of Inner Protoplanetary Disks14:30
Á°´ü Âè2²ó 4/18 14:00-Carina Heinreichsberger (Universität Wien)Terrestrial or Gaseous? A classification of exoplanets according to density, mass and radius
Á°´ü Âè3²ó 4/25 14:00-Kazunari IwasakiChemistry in Debris Disks
Á°´ü Âè4²ó 5/16 14:30-Yuhito Shibaike (Tokyo Tech)A new formation scenario for the Galilean satellites14:30
Á°´ü Âè5²ó 5/23 14:00-Yuji Matsumoto (ASIAA)The orbital stability of planets in resonances considering the evolution of mass ratio
4/18 Carina Heinreichsberger, Terrestrial or Gaseous? A classification of exoplanets according to density, mass and radius
When looking at Exoplanet Archives the class of a planet is not given. Therefore I tried to find an easy and fast way to classify exoplanets using only density, mass and radius. In this talk I will discuss the formation theory of Planets to explain the boundaries between the different classes (gas, terrestrial) and show the results of my empirical study.
5/16 Yuhito Shibaike, A new formation scenario for the Galilean satellites
It is generally accepted that the four major (Galilean) satellites formed out of the gas disk that accompanied Jupiter¡Çs formation. I will discuss a new formation scenario for the Galilean satellites, based on the capture of several planetesimal seeds and subsequent slow accretion of pebbles. Our slow-pebble-accretion scenario can reproduce the following characteristics: (1) the mass of all the Galilean satellites; (2) the orbits of Io, Europa, and Ganymede captured in mutual 2:1 mean motion resonances; (3) the ice mass fractions of all the Galilean satellites; (4) the unique ice-rock partially differentiated Callisto and the complete differentiation of the other satellites.