The planetary system of HD 69830 is uniquely constrained by observations of (i)
an infrared excess indicative of a debris disk with warm dust and (ii) radial
velocity variations indicative of three planets. This presents a valuable
opportunity to test planet formation models by integrating dynamical models of
planetary formation and migration with those for the sculpting of a
dust-producing planetesimal disk. We perform n-body
simulations and investigate the excitation of both planet and planetesimal
eccentricities, the accretion of planetesimals onto the planets, and the
clearing of a planetesimal disk by the planets as they grow in mass and migrate
through the disk. In simulations tuned to closely follow previous semi-analytic
models for the growth and migration of the planets, we find that the inner
planet accretes significantly more planetesimals than previously estimated. We
find that eccentricity excitation due to mutual planetary perturbations during
and after the migration do not naturally produce the observed eccentricities.
Our simulations suggest that this discrepancy may be reduced or possibly
reconciled if the planets are significantly more massive
than expected (possible if the planetary system's angular
momentum were nearly parallel to our line of sight). Even if the planets are
significantly more massive than previously assumed, we find that the migrating
planets are inefficient at clearing the outer planetesimal disk and that a
significant fraction of the planetesimal population beyond 1 AU remains bound on
moderately eccentric and inclined orbits. While much of the remaining
planetesimal belt would have eroded via a collisional cascade and radiation
pressure, we explore whether some of the highly excited planetesimals may be
able to persist over the age of the central star,
producing the dust observed in the HD 69830 system.