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Astron. Astrophys. 331, 669-696 (1998)
6. Conclusions
The framework of the IRAM key-project has allowed us to build a
unique data set on the environment of quiescent low mass dense cores,
because of the multiplicity of the lines observed simultaneously,
because of the large size of the maps with respect to the resolution,
and because of the good signal-to-noise ratio of the spectra, despite
the moderate strength of the lines. The scientific goals of this
project were manyfold. One of our primary objective was to determine
the dynamical characteristics of the turbulent gas which is the
placental medium of thermally supported dense cores, and more
specifically to study the transition region over which the dissipation
of the non-thermal kinetic energy takes place. Our maps were not
centered on some bright source at large scale but on weakly CO
emitting regions containing low mass condensations of dense gas, with
little amount of non-thermal support. A thorough interpretation of the
data is beyond the scope of this first paper and we have focused here
on the presentation of the salient features of the observational
results and on a straightforward interpretation of these results.
Despite their low average column density at the parsec scale, all
the fields appear highly structured in space and velocity. Maps of
integrated line emission barely exhibit unresolved structures, but
channel maps do so. lines, in particular, reveal
a remarkable filamentary structure with, in some cases, unresolved
transverse sizes ( ), and
aspect ratios . These filaments have a much
larger velocity coverage than the gas bright in
or . Interpreted as velocity gradients, this
velocity coverage corresponds to gradients as large as 10 km
s-1 pc-1 across the structures. Unexpectedly,
the quiescent dense cores are surrounded by a gas component which
exhibits quite large accelerations.
The uniformity of the brightness temperature ratio of the two
lowest CO rotational transitions, in the three fields, from the
brightest to the weakest detected lines, across the entire profiles
and for both and isotopes,
is remarkable. 80% of the data points fall within the range
R(2-1/1-0)=0.65 0.15. Deviations from this
general behaviour are also visible. In the Polaris and L1512 fields,
the line profiles may be decomposed into a line-core and a line-wing
component. The line-wing component is bright in
but barely detected in while in the line-core
component the lines reach temperatures as large
as those of . The spatial structure of the
line-wing component is quite different from that of the line-core
component although both are present along most lines of sight. It is
the gas component which emits in the line-wings of the
emission and has the broadest velocity coverage
which exhibits the highest level of observed small scale structure.
The line-wing emission is characterized by a line ratio R(2-1/1-0)
0.6, constant down to the weakest line
intensities while in the line-core emission the line ratio R(2-1/1-0)
increases from 0.65 to 0.8 with the line temperature. Last, in spite
of the low isotopic line ratio observed in the line-core emission,
line profiles are neither flat topped nor self-reversed, except in the
L134A field.
We interpret these well-defined properties as a signature that the
lines form in macroturbulent conditions, i.e. emission arises in
phase-space cells with little radiative coupling with one another.
Under the simple assumption that the cells in a beam are statistically
independent, we infer an upper limit to their size,
200 AU. A preliminary analysis of the line
properties (isotopic line ratios and rotational line ratios) in the
framework of macroturbulence, suggests cell densities
a few
, for the line-wing emission and up to 100 times
larger in the line-core emission. We find that, in the Polaris field
which has the largest velocity dispersion, the
and line intensities increase as their linewidth
decreases. It may be interpreted as an increase of the radiative
coupling of the cells as the cell to cell velocity gradually drops
along a well-defined filament. In the L1512 field, the
and lines are yet brighter
and narrower, and we speculate that the dissipation process there has
already proceeded further.
© European Southern Observatory (ESO) 1998
Online publication: February 16, 1998
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