The combination of our H2 data with previous observational results, allows us to draw a comprehensive picture of the outflow activity of S140 IRS1 on a wide range of spatial and temporal scales:
The presence of the large scale
outflow
was already well established from radio line observations. In the radio maps,
outflowing gas can be seen at least up to distances of 1' (54000 AU)
from IRS1 (e.g. Minchin et al. 1993).
Our high-resolution speckle observations (Schertl et al. 2000; Weigelt
et al. 2002) revealed the detailed structure of the cavity through which the
material in the
outflow lobe is flowing on scales of 90-1800 AU.
Our molecular hydrogen emission line images show
only two relatively weak H2 knots associated
with this outflow, knots 3 and 9. This suggests that there
are currently not many strong shocks in this outflow, perhaps
because the path of the outflow is already well cleared and
the material is flowing away without producing strong shocks.
However, the detection of H2 shock emission in this outflow is
aggravated due to the inclination of the flow and projection effects:
In the south-eastern part, where the outflow is directed towards us,
H2 emission very close to (
2'' away from) IRS1 would be projected
onto the very bright emission of the cavity.
In the north-western part of this outflow, H2 shock emission might
be present, but
hidden behind the dense circumstellar material around IRS1.
The fact that the high resolution radio continuum observations
presented by Schwartz (1989) and Hoare & Muxlow (1996)
do not show any sign
of the
outflow, supports our assumption
that this outflow is probably currently not very active.
A rough estimate of the kinematic age of this outflow can also be made:
from the projected distance of knot 9, an assumed velocity of
100 kms-1, and assuming an inclination angle of
,
we find a lower limit of
years.
The existence of a
outflow
has not so far been well established.
Radio line observations had shown a relatively weak
low-velocity wing in the CO and HCO+ emission that indicated
outflowing material in the
direction, but no reliable evidence
for an outflow in the
direction.
The high-resolution radio continuum maps of S140 IRS1 presented
by Schwartz (1989) revealed a strongly elongated jet-like appendage extending
from IRS1 in the south-west direction (position angle
), and
a diffuse radio source (VLA 4) south-west of IRS1 (position angle
)
which may be a radio Herbig-Haro object.
These features were interpreted as evidence for ejection
of material from IRS1 in the south-western direction.
The high-resolution radio observations by Hoare & Muxlow (1996) showed
a strongly elongated structure oriented in the
direction.
It was interpreted as a highly collimated jet, probably being driven
by a disk wind. The 8.4 GHz VLA observations of S140 presented by
Tofani et al. (1995) revealed an interesting S-shape for the
emission within 1'' of IRS1. While the core of the emission is
oriented in the
direction, the position angle
of the north-eastern tip of the 8.4 GHz emission is
,
in very good agreement with the position angle of the outflow cavities
we found in the speckle images.
Our high-resolution speckle observations (Weigelt et al. 2002)
revealed three arc-like structures with position angles of
,
,
and
north-east of IRS1.
The shapes of these arcs could be well reproduced by a
semi-analytical model of jet-driven flows,
in which prompt entrainment occurs at the head of the traveling bow shock.
This strongly suggested a flow of material
in this direction, but could not be considered as a clear proof.
The result that the eastern edge of the supposed cavities is actually
associated with strong H2 emission,
confirms our previous interpretation that these cavities have been
created by outflowing material from IRS1
in the
20
direction.
Our H2 line emission image reveals numerous knots along the paths
of the
outflow:
knots 1, 2, 10, 11, and 12 are related
to the
flow,
knots 4 and 5 to the
flow.
These knots span a range of position angles from
to
,
which is consistent with the orientation of the elongated radio emission
immediately around IRS1.
The numerous H2 shocks in these directions indicate that
the outflow currently interacts very strongly with its surroundings.
Perhaps the outflow is currently in the process of clearing its way through
the ambient material.
The rather wide range of position angles of the individual H2 knots
north-east of IRS1 suggest a pulsed nature for the outflow and directional
variability. A wiggling jet in the NE/SW direction
is also suggested by the radio continuum and
maser emission on the scale of
(Tofani et al. 1995), which
extends
in the 45
direction i.e. towards H2 knot 2.
The temporal variability of the outflow direction may be caused
by the precession of the circumstellar disk around the outflow source
which is a member of a non-coplanar binary system (see Weigelt et al. 2002
for details; for the theoretical background of this model
see e.g. Papaloizou & Terquem 1995; Terquem 1998; Bate et al. 2000).
A rough estimate of the kinematic age of this outflow, based on the
distance of knot 10, an assumed inclination angle of
and a velocity
100 kms-1, yields
years for the
outflow. This
is nearly three times younger than the lower limit to the kinematic age of
the
outflow.
Copyright ESO 2002