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Turbulence destroys thermal lobes around Mars-sized planetary embryos

SpaceEarth & Environment

Key takeaway

Large Mars-sized objects in forming planetary systems can disrupt their own local environment through turbulence, limiting the effectiveness of the thermal forces that shape their orbits.

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Quick Explainer

Thermal forces can drive the migration and growth of low-mass planets in protoplanetary disks, but these effects are disrupted by turbulence. The authors' simulations show that turbulence, caused by the magnetorotational instability, quickly destroys the asymmetric hot or cold gas lobes around planetary embryos that are responsible for generating coherent thermal torques. Instead, planets in the critical mass range experience stochastic, oscillatory migration driven by the turbulent gas flow, rather than the predictable migration driven by thermal effects in laminar disks. This finding highlights the importance of accounting for realistic turbulent conditions in models of early planetary system formation.

Deep Dive

Technical Deep Dive: Turbulence destroys thermal lobes around Mars-sized planetary embryos

Problem & Context

  • Thermal forces can drive the migration and growth of low-mass planets in protoplanetary disks. These include:
    • Heating torques: Caused by asymmetric hot gas lobes around a luminous planet
    • Cold thermal torques: Caused by asymmetric cold gas lobes around a non-luminous planet
  • These thermal torques can dominate over the classical Lindblad and corotation torques, potentially slowing down or even reversing inward migration of growing planets.
  • However, prior studies of thermal torques have assumed a laminar, unmagnetized disk. In reality, many regions of protoplanetary disks are expected to be turbulent, driven by the magnetorotational instability (MRI).

Methodology

  • The authors conducted high-resolution 3D magnetohydrodynamic (MHD) simulations of a planetary embryo embedded in a stratified, thermally diffusive protoplanetary disk with a toroidal magnetic field.
  • They simulated two cases: a cold embryo (L=0, cold thermal torque) and a hot, luminous embryo (L=Lc, heating torque).
  • The strength of the magnetic field was parameterized by the plasma beta (β) parameter, with β=50 and β=1000 cases considered.
  • They analyzed the development of turbulence, the disruption of thermal lobes, and the resulting torques on the planetary embryo.

Results

  • Turbulence develops within 1.5-3 orbital periods, completely disrupting the thermal lobes around the planetary embryo.
  • This is true regardless of the embryo's luminosity (L=0 or L=Lc) or the magnetic field strength (β=50 or β=1000).
  • In the turbulent regime, the total torque on the planetary embryo displays a strongly oscillatory, stochastic behavior, rather than the coherent thermal torques seen in laminar disks.
  • This stochastic torque regime applies to planetary masses in the range 0.03 M⊕ ≲ Mp ≲ 1 M⊕, as well as for Mp ≳ 3 M⊕.
  • The authors found no evidence that magnetic resonances play a significant role in the turbulent disk.

Interpretation

  • Thermal torques become inefficient in turbulent regions of protoplanetary disks, such as outside the dead zone where the MRI operates.
  • Planets in the mass range 0.03 M⊕ ≲ Mp ≲ 1 M⊕ and Mp ≳ 3 M⊕ experience stochastic migration in these turbulent disk regions, rather than the coherent migration driven by thermal torques in laminar disks.

Limitations & Uncertainties

  • The authors used a constant thermal diffusivity in their simulations, whereas in real disks it would vary with local conditions like density, temperature, and dust properties.
  • They only simulated two specific planetary masses (0.33 M₃ and 1 M⊕). The behavior for other masses in the critical range is not directly addressed.

What Comes Next

  • Future work should explore more realistic models with variable thermal diffusivity and an explicit treatment of dust, which can influence the local thermal properties.
  • Simulations covering a broader range of planetary masses in the 0.03-1 M⊕ regime would help better characterize the transition to stochastic migration.

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