摘要: Recent ALMA observations have identified a variety of dust gaps in
protoplanetary disks, which are commonly interpreted to be generated by
unobserved planets. Predicting mass of such embedded planets is of fundamental
importance in comparing those disk architectures with the observed diversity of
exoplanets. The prediction, however, depends on the assumption that whether the
same gap structure exists in the dust component alone or in the gas component
as well. We assume a planet can only open a gap in the gas component when its
mass exceeds the pebble isolation mass by considering the core accretion
scenario. We then propose two criteria to distinguish if a gap is opened in the
dust disk alone or the gas gap as well when observation data on the gas profile
is not available. We apply the criteria to 35 disk systems with a total of 55
gaps compiled from previous studies, and classify each gap into four different
groups. The classification of the observed gaps allows us to predict the mass
of embedded planets in a consistent manner with the pebble isolation mass. We
find that outer gaps are mostly dust alone, while inner gaps are more likely to
be associated with a gas gap as well. The distribution of such embedded planets
is very different from the architecture of the observed planetary systems,
suggesting that the significant inward migration is required in their
evolution.