Dust settling instability in protoplanetary discs

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Dust settling instability in protoplanetary discs. / Krapp, Leonardo; Youdin, Andrew N.; Kratter, Kaidin M.; Benitez-Llambay, Pablo.

In: Monthly Notices of the Royal Astronomical Society, Vol. 497, No. 3, 09.2020, p. 2715-2729.

Research output: Contribution to journalJournal articleResearchpeer-review

Harvard

Krapp, L, Youdin, AN, Kratter, KM & Benitez-Llambay, P 2020, 'Dust settling instability in protoplanetary discs', Monthly Notices of the Royal Astronomical Society, vol. 497, no. 3, pp. 2715-2729. https://doi.org/10.1093/mnras/staa1854

APA

Krapp, L., Youdin, A. N., Kratter, K. M., & Benitez-Llambay, P. (2020). Dust settling instability in protoplanetary discs. Monthly Notices of the Royal Astronomical Society, 497(3), 2715-2729. https://doi.org/10.1093/mnras/staa1854

Vancouver

Krapp L, Youdin AN, Kratter KM, Benitez-Llambay P. Dust settling instability in protoplanetary discs. Monthly Notices of the Royal Astronomical Society. 2020 Sep;497(3):2715-2729. https://doi.org/10.1093/mnras/staa1854

Author

Krapp, Leonardo ; Youdin, Andrew N. ; Kratter, Kaidin M. ; Benitez-Llambay, Pablo. / Dust settling instability in protoplanetary discs. In: Monthly Notices of the Royal Astronomical Society. 2020 ; Vol. 497, No. 3. pp. 2715-2729.

Bibtex

@article{874986fe083d48698c07e0094ae6a826,
title = "Dust settling instability in protoplanetary discs",
abstract = "The streaming instability (SI) has been extensively studied in the linear and non-linear regimes as a mechanism to concentrate solids and trigger planetesimal formation in the mid-plane of protoplanetary discs. A related dust settling instability (DSI) applies to particles while settling towards the mid-plane. The DSI has previously been studied in the linear regime, with predictions that it could trigger particle clumping away from the mid-plane. This work presents a range of linear calculations and non-linear simulations, performed with FARGO3D, to assess conditions for DSI growth. We expand on previous linear analyses by including particle size distributions and performing a detailed study of the amount of background turbulence needed to stabilize the DSI. When including binned size distributions, the DSI often produces converged growth rates with fewer bins than the standard SI. With background turbulence, we find that the most favourable conditions for DSI growth are weak turbulence, characterized by alpha less than or similar to 10(-6) with intermediate-sized grains that settle from one gas scale height. These conditions could arise during a sudden decrease in disc turbulence following an accretion outburst. Ignoring background turbulence, we performed a parameter survey of local 2D DSI simulations. Particle clumping was either weak or occurred slower than particles settle. Clumping was reduced by a factor of 2 in a comparison 3D simulation. Overall, our results strongly disfavour the hypothesis that the DSI significantly promotes planetesimal formation. Non-linear simulations of the DSI with different numerical methods could support or challenge these findings.",
keywords = "hydrodynamics, methods: numerical, planets and satellites: formation, protoplanetary discs, circumstellar matter, PLANETESIMAL FORMATION, STREAMING INSTABILITY, NONLINEAR EVOLUTION, TURBULENCE DRIVEN, SOLAR, GAS, DISKS, ACCRETION, DYNAMICS, GROWTH",
author = "Leonardo Krapp and Youdin, {Andrew N.} and Kratter, {Kaidin M.} and Pablo Benitez-Llambay",
year = "2020",
month = sep,
doi = "10.1093/mnras/staa1854",
language = "English",
volume = "497",
pages = "2715--2729",
journal = "Royal Astronomical Society. Monthly Notices",
issn = "0035-8711",
publisher = "Oxford University Press",
number = "3",

}

RIS

TY - JOUR

T1 - Dust settling instability in protoplanetary discs

AU - Krapp, Leonardo

AU - Youdin, Andrew N.

AU - Kratter, Kaidin M.

AU - Benitez-Llambay, Pablo

PY - 2020/9

Y1 - 2020/9

N2 - The streaming instability (SI) has been extensively studied in the linear and non-linear regimes as a mechanism to concentrate solids and trigger planetesimal formation in the mid-plane of protoplanetary discs. A related dust settling instability (DSI) applies to particles while settling towards the mid-plane. The DSI has previously been studied in the linear regime, with predictions that it could trigger particle clumping away from the mid-plane. This work presents a range of linear calculations and non-linear simulations, performed with FARGO3D, to assess conditions for DSI growth. We expand on previous linear analyses by including particle size distributions and performing a detailed study of the amount of background turbulence needed to stabilize the DSI. When including binned size distributions, the DSI often produces converged growth rates with fewer bins than the standard SI. With background turbulence, we find that the most favourable conditions for DSI growth are weak turbulence, characterized by alpha less than or similar to 10(-6) with intermediate-sized grains that settle from one gas scale height. These conditions could arise during a sudden decrease in disc turbulence following an accretion outburst. Ignoring background turbulence, we performed a parameter survey of local 2D DSI simulations. Particle clumping was either weak or occurred slower than particles settle. Clumping was reduced by a factor of 2 in a comparison 3D simulation. Overall, our results strongly disfavour the hypothesis that the DSI significantly promotes planetesimal formation. Non-linear simulations of the DSI with different numerical methods could support or challenge these findings.

AB - The streaming instability (SI) has been extensively studied in the linear and non-linear regimes as a mechanism to concentrate solids and trigger planetesimal formation in the mid-plane of protoplanetary discs. A related dust settling instability (DSI) applies to particles while settling towards the mid-plane. The DSI has previously been studied in the linear regime, with predictions that it could trigger particle clumping away from the mid-plane. This work presents a range of linear calculations and non-linear simulations, performed with FARGO3D, to assess conditions for DSI growth. We expand on previous linear analyses by including particle size distributions and performing a detailed study of the amount of background turbulence needed to stabilize the DSI. When including binned size distributions, the DSI often produces converged growth rates with fewer bins than the standard SI. With background turbulence, we find that the most favourable conditions for DSI growth are weak turbulence, characterized by alpha less than or similar to 10(-6) with intermediate-sized grains that settle from one gas scale height. These conditions could arise during a sudden decrease in disc turbulence following an accretion outburst. Ignoring background turbulence, we performed a parameter survey of local 2D DSI simulations. Particle clumping was either weak or occurred slower than particles settle. Clumping was reduced by a factor of 2 in a comparison 3D simulation. Overall, our results strongly disfavour the hypothesis that the DSI significantly promotes planetesimal formation. Non-linear simulations of the DSI with different numerical methods could support or challenge these findings.

KW - hydrodynamics

KW - methods: numerical

KW - planets and satellites: formation

KW - protoplanetary discs

KW - circumstellar matter

KW - PLANETESIMAL FORMATION

KW - STREAMING INSTABILITY

KW - NONLINEAR EVOLUTION

KW - TURBULENCE DRIVEN

KW - SOLAR

KW - GAS

KW - DISKS

KW - ACCRETION

KW - DYNAMICS

KW - GROWTH

U2 - 10.1093/mnras/staa1854

DO - 10.1093/mnras/staa1854

M3 - Journal article

VL - 497

SP - 2715

EP - 2729

JO - Royal Astronomical Society. Monthly Notices

JF - Royal Astronomical Society. Monthly Notices

SN - 0035-8711

IS - 3

ER -

ID: 250544204