We show that the very young brown dwarf candidate ISO217 (M6.25) is driving
an intrinsically asymmetric bipolar outflow with a stronger and slightly faster
red-shifted component based on spectro-astrometry of forbidden [SII] emission
lines observed in UVES/VLT spectra taken in 2009. ISO217 is only one of a
handful of brown dwarfs and VLMS (M5-M8) for which an outflow has been detected
and that show that the T Tauri phase continues at the substellar limit. We
measure a spatial extension of the outflow of +/-190mas (+/-30AU) and
velocities of +/-40-50kms/s. We show that the velocity asymmetry between both
lobes is variable on timescales of a few years and that the strong asymmetry of
a factor of 2 found in 2007 might be smaller than originally anticipated when
using a more realistic stellar rest-velocity. We also detect forbidden
[FeII]7155 emission, for which we propose as potential origin the hot inner
regions of the outflow. To understand the ISO217 system, we determine the disk
properties based on radiative transfer modeling of the SED. This disk model
agrees very well with Herschel/PACS data at 70mu. We find that the disk is
flared and intermediately inclined (~45deg). The total disk mass (4e-6 Msun) is
small compared to the accretion and outflow rate of ISO217 (~1e-10 Msun/yr). We
propose that this discrepancy can be explained by either a higher disk mass
than inferred from the model (strong undetected grain growth) and/or by an on
average lower accretion and outflow rate than the determined values. We show
that a disk inclination significantly exceeding 45deg, as suggested from Halpha
modeling and from both lobes of the outflow being visible, is inconsistent with
the SED data. Thus, despite its intermediate inclination angle, the disk of
this brown dwarf does not appear to obscure the red outflow component, which is
very rarely seen for T Tauri objects (only one other case).Comment: Accepted for publication at A&A; minor changes (language editing