A&A 470, 733-739 (2007)
DOI: 10.1051/0004-6361:20077354
Collisions between equal-sized ice grain agglomerates
C. Schäfer, R. Speith, and W. KleyInstitute for Astronomy & Astrophysics, University of Tübingen, Auf der Morgenstelle 10, 72076 Tübingen, Germany
e-mail: [schaefer;speith;kley]@tat.physik.uni-tuebingen.de
(Received 26 February 2007 / Accepted 4 May 2007)
Abstract
Context.Following the recent insight in the material structure of comets,
protoplanetesimals are assumed to have low densities and to be highly
porous agglomerates. It is still unclear if planetesimals can be formed
from these objects by collisional growth.
Aims.Therefore, it is important to study numerically the
collisional outcome from low velocity impacts of equal sized
porous agglomerates which are too large to be examined in a laboratory experiment.
Methods.We use the Lagrangian particle method Smooth Particle Hydrodynamics to
solve the equations that describe the dynamics of
elastic and plastic bodies. Additionally, to account for the influence
of porosity, we follow a previous developed equation of state and
certain relations between the material strength and the relative
density.
Results.Collisional growth seems possible for rather low collision velocities
and particular material strengths. The remnants of collisions with
impact parameters that are larger than 50% of the radius of the
colliding objects tend to rotate. For small impact parameters, the
colliding objects are effectively slowed down without a prominent
compaction of the porous structure, which probably increases the
possibility for growth. The protoplanetesimals, however, do not stick
together for the most part of the employed material strengths.
Conclusions.An important issue in subsequent studies has to be the influence of
rotation to collisional growth. Moreover, for realistic
simulations of protoplanetesimals it is crucial to know the
correct material parameters in more detail.
Key words: planetary systems: formation -- planetary systems: protoplanetary disks
© ESO 2007

BibSonomy
CiteUlike
Del.icio.us
Digg
Facebook
Mendeley
Twitter