Streaming Torque with Turbulent Diffusion

Fast type I migration of (proto)planets poses a challenging problem for the core accretion formation scenario. We found that the dust-induced “Streaming Torque” (ST) may slow down or even reverse the planet migration in Q. Hou & C. Yu. But in realistic protoplanetary disks, dust diffusion induce...

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Main Authors: Qiang Hou, Cong Yu
Format: Article
Language:English
Published: IOP Publishing 2025-01-01
Series:The Astrophysical Journal
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Online Access:https://doi.org/10.3847/1538-4357/ada15a
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author Qiang Hou
Cong Yu
author_facet Qiang Hou
Cong Yu
author_sort Qiang Hou
collection DOAJ
description Fast type I migration of (proto)planets poses a challenging problem for the core accretion formation scenario. We found that the dust-induced “Streaming Torque” (ST) may slow down or even reverse the planet migration in Q. Hou & C. Yu. But in realistic protoplanetary disks, dust diffusion induced by gas turbulence may have important influences on ST. We perform linear analysis to investigate the effects of dust diffusion on ST. The dependence of ST on dust diffusion may provide better constraints on the turbulence strength and the stopping time τ . We derive the dispersion relation for all the wave modes in the two-fluid system. The dust diffusion will smooth the short-wavelength structure of the the quasi-drift mode and split it into two predominant D-drift modes with opposite directions. The outgoing D-drift mode will contribute to a negative torque on planets, particularly when τ  ∼ 0.1, which slightly shifts the zero-torque turning point. We explore how ST depends on the regimes of aerodynamic drag, dust mass fraction, and disk scale height. We compare the radial wavenumbers of D-drift modes under different formulations of dust diffusion and find qualitative agreement. In all cases, τ at the zero-torque turning point, which determines the direction of planetary migration, consistently remains on the order of ∼0.1, corresponding to large pebble-sized dust grains. This suggests that rapid dust coagulation can inhibit the inward migration of planets, implying that weak gas turbulence may enhance the survival of protoplanets.
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spelling doaj-art-d2290d3f90724940bbc9d254d31ce3cb2025-01-27T16:40:30ZengIOP PublishingThe Astrophysical Journal1538-43572025-01-01979218510.3847/1538-4357/ada15aStreaming Torque with Turbulent DiffusionQiang Hou0https://orcid.org/0000-0002-8125-7320Cong Yu1https://orcid.org/0000-0003-0454-7890School of Physics and Astronomy, Sun Yat-sen University , Zhuhai 519082, People’s Republic of China ; yucong@mail.sysu.edu.cn; CSST Science Center for the Guangdong-Hong Kong-Macau Greater Bay Area , Zhuhai 519082, People’s Republic of China; State Key Laboratory of Lunar and Planetary Sciences, Macau University of Science and Technology , Macau 999078, People’s Republic of ChinaSchool of Physics and Astronomy, Sun Yat-sen University , Zhuhai 519082, People’s Republic of China ; yucong@mail.sysu.edu.cn; CSST Science Center for the Guangdong-Hong Kong-Macau Greater Bay Area , Zhuhai 519082, People’s Republic of China; State Key Laboratory of Lunar and Planetary Sciences, Macau University of Science and Technology , Macau 999078, People’s Republic of ChinaFast type I migration of (proto)planets poses a challenging problem for the core accretion formation scenario. We found that the dust-induced “Streaming Torque” (ST) may slow down or even reverse the planet migration in Q. Hou & C. Yu. But in realistic protoplanetary disks, dust diffusion induced by gas turbulence may have important influences on ST. We perform linear analysis to investigate the effects of dust diffusion on ST. The dependence of ST on dust diffusion may provide better constraints on the turbulence strength and the stopping time τ . We derive the dispersion relation for all the wave modes in the two-fluid system. The dust diffusion will smooth the short-wavelength structure of the the quasi-drift mode and split it into two predominant D-drift modes with opposite directions. The outgoing D-drift mode will contribute to a negative torque on planets, particularly when τ  ∼ 0.1, which slightly shifts the zero-torque turning point. We explore how ST depends on the regimes of aerodynamic drag, dust mass fraction, and disk scale height. We compare the radial wavenumbers of D-drift modes under different formulations of dust diffusion and find qualitative agreement. In all cases, τ at the zero-torque turning point, which determines the direction of planetary migration, consistently remains on the order of ∼0.1, corresponding to large pebble-sized dust grains. This suggests that rapid dust coagulation can inhibit the inward migration of planets, implying that weak gas turbulence may enhance the survival of protoplanets.https://doi.org/10.3847/1538-4357/ada15aHydrodynamicsProtoplanetary disksPlanetary-disk interactionsPlanetary system formationPlanetary migration
spellingShingle Qiang Hou
Cong Yu
Streaming Torque with Turbulent Diffusion
The Astrophysical Journal
Hydrodynamics
Protoplanetary disks
Planetary-disk interactions
Planetary system formation
Planetary migration
title Streaming Torque with Turbulent Diffusion
title_full Streaming Torque with Turbulent Diffusion
title_fullStr Streaming Torque with Turbulent Diffusion
title_full_unstemmed Streaming Torque with Turbulent Diffusion
title_short Streaming Torque with Turbulent Diffusion
title_sort streaming torque with turbulent diffusion
topic Hydrodynamics
Protoplanetary disks
Planetary-disk interactions
Planetary system formation
Planetary migration
url https://doi.org/10.3847/1538-4357/ada15a
work_keys_str_mv AT qianghou streamingtorquewithturbulentdiffusion
AT congyu streamingtorquewithturbulentdiffusion