Issue |
A&A
Volume 445, Number 2, January II 2006
|
|
---|---|---|
Page(s) | 747 - 758 | |
Section | Planets and planetary systems | |
DOI | https://doi.org/10.1051/0004-6361:20053238 | |
Published online | 16 December 2005 |
3D-radiation hydro simulations of disk-planet interactions
I. Numerical algorithm and test cases
1
Universität Tübingen, Institut für Astronomie und Astrophysik, Abt. Computational Physics, Auf der Morgenstelle 10, 72076 Tübingen, Germany e-mail: wilhelm.kley@uni-tuebingen.de
2
Max-Planck-Institut für Astronomie, Königstuhl 17, 69117 Heidelberg, Germany e-mail: klahr@mpia.de
Received:
13
April
2005
Accepted:
16
August
2005
We study the evolution of an embedded protoplanet in a circumstellar
disk using the 3D-Radiation Hydro code TRAMP, and treat
the thermodynamics of the gas properly in three dimensions.
The primary interest of this work lies in the
demonstration and testing of the numerical method.
We show how far numerical parameters can influence
the simulations of gap opening. We study
a standard reference model under various numerical approximations.
Then we compare the commonly used locally isothermal approximation
to the radiation hydro simulation using an
equation for the internal energy.
Models with different treatments of the mass accretion process
are compared. Often mass accumulates in the Roche lobe of the planet
creating a hydrostatic atmosphere around the planet.
The gravitational torques induced by the spiral pattern of the disk
onto the planet are not strongly affected in the average
magnitude, but the short time scale fluctuations are
stronger in the radiation hydro models.
An interesting result of this work lies in the analysis of the temperature
structure around the planet. The most striking effect of treating the thermodynamics properly
is the formation of a hot pressure-supported bubble around the planet
with a pressure scale height of rather than a thin Keplerian
circumplanetary accretion disk.
Key words: accretion, accretion disks / hydrodynamics / solar system: formation / radiative transfer / planets and satellites: formation
© ESO, 2005
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