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Origins: from the Protosun to the First Steps of Life Proceedings IAU Symposium No. 345, 2019

Bruce G. Elmegreen, L. Viktor T´oth, Manuel G¨udel, eds.

c

2019 International Astronomical Union DOI: 00.0000/X000000000000000X

Global Protoplanetary Disk Simulations:

Dead Zone Formation and FUor Outbursts

Kundan Kadam

1,∗

, E. Vorobyov

2,3

, Zs. Reg´ aly

1

, ´ A. K´ osp´ al

1,4

, P. ´ Abr´ aham

1

1Konkoly Observatory, MTA CSFK, Budapest, Hungary;

email:kundan.kadam@csfk.mta.hu

2The University of Vienna, Vienna, Austria;3Southern Federal University, Rostov-on-Don, Russia;4Max Planck Institute for Astronomy, Heidelberg, Germany.

Abstract. We conducted global hydrodynamic simulations of protoplanetary disk evolution with an adaptive Shakura-Sunyaevαprescription to represent the layered disk structure, and starting with the collapse phase of the molecular cloud. With the canonical values of model parameters, self-consistent dead zones formed at the scale of a few au. The instabilities associated with the dead zone and corresponding outbursts, similar to FUor eruptions, were also observed in the simulations.

Keywords.planetary systems: protoplanetary disks, hydrodynamics, turbulence

1. Introduction

T Tauri-type stars in young stellar clusters show an apparent “luminosity problem”, where their luminosity is observed to be about an order of magnitude lower as compared to that predicted by theoretical models (Kenyon et al. 1990). Variable young stars called FUors (prototype- FU Orionis) indeed show brightening by a factor of ∼ 100, which can last for several decades (Hartmann & Kenyon 1996). Magneto-rotational instabil- ity (MRI) and gravitational instability (GI) are two of the prominent mechanisms for angular momentum transport in a protoplanetary disk. Gammie (1996) suggested that the midplane temperature of a protoplanetary disk at ∼1 au is low enough to suppress the MRI, and the accretion occurs only through a thin surface layer due to cosmic ray ionization. Armitage et al. (2001) demonstrated that the transport of gas due to GI in the outer regions may lead to pile up of material at the magnetically inactive dead zone.

The increased viscous heating in the this zone can eventually trigger MRI if the midplane temperature reaches a critical value (Tcrit) when the alkali metals are ionized, giving rise to the gravo-magneto (GM) instability in the disk.

2. Results

We performed global hydrodynamic simulations of protoplanetary disks in the thin disk limit, including the gravitational collapse phase of the cloud core (for details about the hy- drodynamic code, see Vorobyov & Basu 2015). The kinematic viscosity was parametrized using a variable Shakura & Sunyaev (1973)αparameter-αeff = (Σaαadαd)/(Σad), where the subscript ‘a’ denotes the gas surface density of the MRI active layer, while ‘d’

denotes that of the dead zone. This prescription of the angular momentum transport is consistent with the expectations from a layered disk model.

With the canonical values of layered disk parameters (Tcrit= 1300K,Σa= 100 g/cm2), self-consistent dead zone formed with the variableαprescription; while such zone did not

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2 Kundan Kadam, E. Vorobyov, et al.

Figure 1.Evolution of the surface density and effectiveα-parameter in the inner 10 au box, showing the progression of the dead zone across an outburst.

Figure 2.Total luminosity of the outbursting system, depicting an eruption similar to FUors.

form in (an otherwise identical) fully MRI active disk. The dead zone showed formation of high surface density and low effective viscosity rings between 1−5 au (Figure 1, first two columns).

Since the dead zone can not effectively transport angular momentum, the gas contin- ued to accumulate in its vicinity from the outer regions. The central disk temperature eventually reachedTcritthrough viscous heating triggering MRI, and thus the GM insta- bility. The dead zone disappeared (see Figure 3, last two columns) and the accumulated material was accerted onto the star. An associated eruption was observed, which can be considered as FUor-like outburst. The eruption typically lasted few hundred years, while the total luminosity of the system increased to∼100L (Figure 2).

References

Armitage, P. J., Livio, M., & Pringle, J. E. 2001, MNRAS, 324, 705 Gammie, C. F. 1996, ApJ, 457, 355

Hartmann, L., & Kenyon, S. J. 1996, ARA&A, 34, 207

Kenyon, S. J., Hartmann, L. W., Strom, K. M., & Strom, S. E. 1990, AJ, 99, 869 Shakura, N. I., & Sunyaev, R. A. 1973, A&A, 24, 337

Vorobyov, E. I., & Basu, S. 2015, ApJ, 805, 115

Ábra

Figure 1. Evolution of the surface density and effective α-parameter in the inner 10 au box, showing the progression of the dead zone across an outburst.

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