A giant solution to the disk mass budget problem of planet formation
TLDR
Giant planet formation and subsequent planetesimal conversion in protoplanetary disks naturally resolve the disk mass budget problem.
Key contributions
- Identifies intermediate initial disk masses (4-7% solar mass) as best matching observed dust distributions.
- Shows giant planets create pressure bumps, trapping "optically thick" dust, explaining observation discrepancies.
- Demonstrates that giant planet-induced pressure bumps are prime sites for planetesimal formation.
- Concludes that planetesimal conversion significantly reduces observable dust, resolving the mass budget problem.
Why it matters
This paper provides a crucial explanation for the long-standing disk mass budget problem in planet formation. By showing how giant planets facilitate planetesimal formation, it explains why evolved disks appear to have less dust than expected. This work refines our understanding of early solar system evolution.
Original Abstract
Understanding how dust evolves in protoplanetary disks is crucial to constraining the initial conditions of planet formation. The apparent "mass budget problem", which stems from the comparison of the observed disk masses to the ones inferred for exoplanets, remains debated, as it is unclear whether the discrepancy arises from limitations in interpreting disk observations, from evolutionary processes that rapidly deplete dust, or from incorrect assumptions about the initial disk mass distribution. This work is build on the analysis presented in Savvidou and Bitsch (2025) by separating the cumulative distribution functions of dust masses at different evolutionary stages into different populations according to the initial disk masses and embryo injection times. The best match to observations comes from disks with intermediate initial disk masses around 4-7% solar mass. The largest discrepancy between the total dust mass in the models and the estimated through an "optically thin" approximation comes from the models that have the most favorable conditions for giant planet formation and thus contain a large fraction of giants and subsequently trapped "optically thick" dust mass because of the pressure bumps they generate. However, the final dust masses remain higher compared to the estimates from the observed evolved disks. Example cases in this work including planetesimal formation show that the pressure bumps that giant planets form can be prime locations for planetesimal formation and the conversion to planetesimals significantly decreases the dust mass, as expected. However, (giant) planet formation is not influenced showing that the mass in evolved protoplanetary disks can be estimated to be quite low but it can be a natural consequence of planetesimal and planet formation along with depletion due to radial drift.
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