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There is no disk mass budget problem of planet formation
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The inferred dust masses from Class II protoplanetary disk observations are lower than or equal to the masses of the observed exoplanet systems. This poses the question of how planets form if their natal environments do not contain enough mass. This hypothesis has entered the literature as the "mass budget problem" of planet formation. We utilize numerical simulations of planet formation via pebble and gas accretion, including migration, in a viscously evolving protoplanetary disk, while tracing the time evolution of the dust mass. As expected, we find that the presence of a giant planet in the disk can influence the evolution of the disk itself and prevent rapid dust mass loss by trapping the dust outside its orbit. Early formation is crucial for giant planet formation, as we found in our previous work; therefore, our findings strengthen the hypothesis that planet formation has already occurred or is ongoing in Class II disks. Most importantly, we find that the optically thin dust mass significantly underestimates the total dust mass in the presence of a dust-trapping deep gap. We also show that the beam convolution would smear out the feature from a deep gap, especially if the planet forms in the inner disk. Such hidden dust mass, along with early planet formation, could be the answer to the hypothetical mass budget problem.
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Cited by 2 Pith papers
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On the Mass Budget Problem of Protoplanetary Disks: Streaming Instability and Optically Thick Emission
Overdense dust filaments produced by the streaming instability become optically thick at sub-millimeter wavelengths, biasing disk mass estimates low by factors of about 2 to 7.
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From Streaming Instability to the Onset of Pebble Accretion I. Investigating the Growth Modes in Planetesimal Rings
Growth to pebble-accreting embryos from streaming-instability planetesimal rings is viable mainly in the inner disk and is strongly suppressed around low-mass stars.
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