Repository logo
  • English
  • Deutsch
  • Español
  • Français
  • Log In
    New user? Click here to register.Have you forgotten your password?

  • English
  • Deutsch
  • Español
  • Français
  • Log In
    New user? Click here to register.Have you forgotten your password?
Repository logo
  • Communities & Collections
  • Research Outputs
  • Fundings & Projects
  • Researchers
  • Statistics
  1. Home
  2. Current Research Information System UV
  3. Publicaciones
  4. A 1.48–2.48 μm <i>R</i> = 28 000 spectroscopic atlas of the L7.5 and T0.5 components of the nearest pair of brown dwarfs: Luhman 16AB
 
  • Details
Options

A 1.48–2.48 μm <i>R</i> = 28 000 spectroscopic atlas of the L7.5 and T0.5 components of the nearest pair of brown dwarfs: Luhman 16AB

Journal
Monthly Notices of the Royal Astronomical Society
ISSN
0035-8711
Date Issued
2025-03-26
DOI
10.1093/mnras/staf487
Abstract
<jats:title>ABSTRACT</jats:title>
<jats:p>We present a high signal-to-noise (SNR $\sim$ 450), high-dispersion ($R \equiv \lambda / \Delta \lambda \sim$ 28 000) $H$- and $K$-band spectroscopic atlas of the L7.5 and T0.5 components of the Luhman 16AB binary (WISE J104915.57$-$531906.1AB): the closest pair of brown dwarfs, and one of the best substellar benchmarks. The spectra were combined from a 70-d spectroscopic monitoring campaign of the binary with IGRINS on Gemini South. We fit model photospheres to the combined high-quality spectra to estimate atmospheric parameters. The model is based on the Sonora model atmosphere further incorporating the effects of clouds and disequilibrium. We detect ammonia (NH3) lines in both binary components, making Luhman 16A the warmest object where individual NH3 lines were identified. We discover hydrogen (H2), hydrogen sulfide (H2S), and hydrogen fluoride (HF) lines in both components, following recent reports of these species in either cooler (H2, H2S in a T6 dwarf) or warmer (HF in young late-M or mid-L dwarfs) objects. Methane (CH4) shows a small contribution, with lines sensitive to the slight temperature difference spanning the L/T transition. Against model expectations, we do not detect FeH lines, implying more efficient iron rainout than incorporated in the models. We find various unidentified features in water-dominated regions, likely the result of residual inaccuracies in the water line lists. We searched for planetary-mass companions by periodogram analysis of radial velocities over 70 d but detected no significant signal. The upper limits of projected planetary mass are $M\sin {i}=$ 0.2 $M_{\mathrm{J}}$ and 0.3 $M_{\mathrm{J}}$ at P $\sim$ 1 d, and 0.4 $M_{\mathrm{J}}$ and 0.7 $M_{\mathrm{J}}$ at P $\sim$ 10 d for Luhman 16A and B, respectively.</jats:p>
Author(s)
Hiroyuki Tako Ishikawa
Stanimir Metchev
Megan E Tannock
Gregory N Mace
Callie E Hood
Jonathan J Fortney
Sagnick Mukherjee
Paulo Miles-Páez
Kurtev, Radostin  
Facultad de Ciencias  

  • Cookie settings
  • Privacy policy
  • End User Agreement
  • Send Feedback

Hosting & Support by

Built with DSpace-CRIS software - Extension maintained and optimized by 4Science