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Published November 10, 2020 | Published + Accepted Version
Journal Article Open

The Evolution of Disk Winds from a Combined Study of Optical and Infrared Forbidden Lines

Abstract

We analyze high-resolution (Δv ≤ 10 km s⁻¹) optical and infrared spectra covering the [O I] λ6300 and [Ne II] 12.81 μm lines from a sample of 31 disks in different evolutionary stages. Following work at optical wavelengths, we use Gaussian profiles to fit the [Ne II] lines and classify them into high-velocity component (HVC) or low-velocity component (LVC) if the line centroid is more or less blueshifted than 30 km s⁻¹ with respect to the stellar radial velocity, respectively. Unlike for the [O I], where an HVC is often accompanied by an LVC, all 17 sources with an [Ne II] detection have either an HVC or an LVC. [Ne II] HVCs are preferentially detected toward high accretors (M_(acc) > 10⁻⁸M_⊙ yr⁻¹), while LVCs are found in sources with low M_(acc), low [O I] luminosity, and large infrared spectral index (n₁₃₋₃₁). Interestingly, the [Ne II] and [O I] LVC luminosities display an opposite behavior with n₁₃₋₃₁: as the inner dust disk depletes (higher n₁₃₋₃₁), the [Ne II] luminosity increases while the [O I] weakens. The [Ne II] and [O I] HVC profiles are generally similar, with centroids and FWHMs showing the expected behavior from shocked gas in microjets. In contrast, the [Ne II] LVC profiles are typically more blueshifted and narrower than the [O I] profiles. The FWHM and centroid versus disk inclination suggest that the [Ne II] LVC predominantly traces unbound gas from a slow, wide-angle wind that has not lost completely the Keplerian signature from its launching region. We sketch an evolutionary scenario that could explain the combined [O I] and [Ne II] results and includes screening of hard (~1 keV) X-rays in inner, mostly molecular, MHD winds.

Additional Information

© 2020 The American Astronomical Society. Received 2020 June 9; revised 2020 August 26; accepted 2020 September 16; published 2020 November 4. This work is based on observations collected at the European Southern Observatory under ESO program 198.C-0104. I.P., U.G., and S.E. acknowledge support from a Collaborative NSF Astronomy & Astrophysics Research grant (ID: 1715022, ID:1713780, and ID:1714229). This material is based on work supported by the National Aeronautics and Space Administration under agreement No. NNX15AD94G for the program Earths in Other Solar Systems. The results reported herein benefited from collaborations and/or information exchange within NASA's Nexus for Exoplanet System Science (NExSS) research coordination network sponsored by NASA's Science Mission Directorate. R.D.A., G.B., and C.H. acknowledge funding from the European Research Council (ERC) under the European Union's Horizon 2020 research and innovation program (grant agreement No. 681601). G.B. acknowledges support from the University of Leicester through a College of Science and Engineering PhD studentship. C.H. is a Winton Fellow, and this research has been supported by Winton Philanthropies/The David and Claudia Harding Foundation. This project has been carried out as part of the European Union's Horizon 2020 research and innovation program under the Marie Skłodowska-Curie grant agreement No. 823823 (dustbusters). Facility: ESO(VISIR). - Software: astropy (The Astropy Collaboration et al. 2013, 2018), mpfitfun (MINPACK-1 in Jorge Moré & Stephen Wright 1987), cenken (Helsel 2005 and Akritas et al. 1995).

Attached Files

Published - Pascucci_2020_ApJ_903_78.pdf

Accepted Version - 2009.09114.pdf

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Additional details

Created:
September 15, 2023
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October 23, 2023