Hostname: page-component-78c5997874-4rdpn Total loading time: 0 Render date: 2024-11-12T21:03:02.977Z Has data issue: false hasContentIssue false

Zooming in on the Formation of Protoplanetary Disks

Published online by Cambridge University Press:  06 January 2014

Åke Nordlund
Affiliation:
Centre for Star and Planet Formation, University of Copenhagen, Øster Voldgade 5, DK-2100 Copenhagen, Denmark email: [email protected] Niels Bohr Institute, University of Copenhagen Juliane Maries Vej 30, DK-2100 Copenhagen, Denmark
Troels Haugbølle
Affiliation:
Centre for Star and Planet Formation, University of Copenhagen, Øster Voldgade 5, DK-2100 Copenhagen, Denmark email: [email protected]
Michael Küffmeier
Affiliation:
Centre for Star and Planet Formation, University of Copenhagen, Øster Voldgade 5, DK-2100 Copenhagen, Denmark email: [email protected] Niels Bohr Institute, University of Copenhagen Juliane Maries Vej 30, DK-2100 Copenhagen, Denmark
Paolo Padoan
Affiliation:
ICREA & ICC, University of Barcelona, Marti i Franqus 1, E-08028 Barcelona, Spain
Aris Vasileiades
Affiliation:
Centre for Star and Planet Formation, University of Copenhagen, Øster Voldgade 5, DK-2100 Copenhagen, Denmark email: [email protected] Niels Bohr Institute, University of Copenhagen Juliane Maries Vej 30, DK-2100 Copenhagen, Denmark
Rights & Permissions [Opens in a new window]

Abstract

Core share and HTML view are not available for this content. However, as you have access to this content, a full PDF is available via the ‘Save PDF’ action button.

We use the adaptive mesh refinement code RAMSES to model the formation of protoplanetary disks in realistic star formation environments. The resolution scales over up to 29 powers of two (~ 9 orders of magnitude) covering a range from outer scales of 40 pc to inner scales of 0.015 AU. The accretion rate from a 1.5 solar mass envelope peaks near 10−4 M about 6 kyr after sink particle formation and then decays approximately exponentially, reaching 10−6 M in 100 kyr. The models suggest universal scalings of physical properties with radius during the main accretion phase, with kinetic and / or magnetic energy in approximate balance with gravitational energy. Efficient accretion is made possible by the braking action of the magnetic field, which nevertheless allows a near-Keplerian disk to grow to a 100 AU size. The magnetic field strength ranges from more than 10 G at 0.1 AU to less than 1 mG at 100 AU, and drives a time dependent bipolar outflow, with a collimated jet and a broader disk wind.

Type
Contributed Papers
Copyright
Copyright © International Astronomical Union 2013 

References

Clyne, J. & Rast, M. 2005, in Proceedings of Visualization and Data Analysis, pp. 284–294Google Scholar
Commercon, B., Teyssier, R., Audit, E., Hennebelle, P., & Chabrier, G. 2011, A&A, 539, 35Google Scholar
Crutcher, R. M. 2011, ARAA, 50, 29CrossRefGoogle Scholar
Goldreich, P. & Ward, W. R. 1973, ApJ, 183, 1051CrossRefGoogle Scholar
Larson, R. 1981, MNRAS, 194, 809Google Scholar
Solomon, P. M., Rivolo, A. R., Barrett, J., & Yahil, A. 1987, ApJ, 319, 730CrossRefGoogle Scholar
Teyssier, R. 2002, A&A, 385, 337Google Scholar
Vasileiades, A., Nordlund, A., & Bizzarro, M. 2013, ApJL, 768, 8CrossRefGoogle Scholar