Bibcode
Burningham, Ben; Leggett, S. K.; Homeier, D.; Saumon, D.; Lucas, P. W.; Pinfield, D. J.; Tinney, C. G.; Allard, F.; Marley, M. S.; Jones, H. R. A.; Murray, D. N.; Ishii, M.; Day-Jones, A.; Gomes, J.; Zhang, Z. H.
Bibliographical reference
Monthly Notices of the Royal Astronomical Society, Volume 414, Issue 4, pp. 3590-3598.
Advertised on:
7
2011
Citations
72
Refereed citations
68
Description
We present near-infrared photometry and spectroscopy, and warm-Spitzer
IRAC photometry of the young very cool T dwarf Ross 458C, which we have
typed as T8.5p. By applying the fiducial age constraints (≤1 Gyr)
imposed by the properties of the active M dwarf Ross 458A, we have used
these data to determine that Ross 458C has Teff= 695 ±
60 K, log g= 4.0-4.7 and an inferred mass of 5-20MJ. We have
compared fits of the near-infrared spectrum and IRAC photometry to the
BT Settl and Saumon & Marley model grids, and have found that both
sets provide best fits that are consistent with our derived properties,
whilst the former provide a marginally closer match to the data for all
scenarios explored here. The main difference between the model grids
arises in the 4.5-μm region, where the BT Settl models are able to
better predict the flux through the IRAC filter, suggesting that
non-equilibrium effects on the CO-CO2 ratio are important for
shaping the mid-infrared spectra of very cool T dwarfs. We have also
revisited the issue of the dust opacity in the spectra of Ross 458C that
was raised by Burgasser et al. We have found that the BT Settl models
which also incorporate a condensate cloud model provide a better match
to the near-infrared spectrum of this target than the Saumon &
Marley model with fsed= 2 and we briefly discuss the
influence of condensate clouds on T dwarf spectra.