In the case of high mass star formation, it has become clear that hot
cores represent one of the earliest phases
(Walmsley 1992). Chemically, hot cores are characterized by high
abundances of fully hydrogenated molecules such as water (H2O), ammonia
(NH3) and hydrogen sulfide (H2S), along with a rich variety of complex organic
molecules ranging from methanol (CH3OH) and ethanol (CH3CH2OH)
to methyl cyanide (CH3CN), dimethyl ether (CH3OCH3),
methyl formate (HCOOCH3) and ethyl cyanide (C2H5CN)
(Walmsley & Schilke 1993; Kuan & Snyder 1996; Hatchell et al. 1998; Schilke 2000).
The chemical richness is explained
by evaporation of the ice mantles above 90 K, followed by rapid
gas-phase ion-molecule reactions leading to more complex species for a
period of
104 yrs (Charnley et al. 1995; Millar et al. 1997;
Rodgers & Charnley 2001,
see van Dishoeck & Blake 1998 and Langer et al. 2000 for overviews). Low mass protostars are less
luminous and less massive, but a similar physical structure is
expected except for a scale factor (Ceccarelli et al. 1996; Ivezic & Elitzur 1997). On
the other hand, shocks due to the interaction of the outflows with the
envelope can also liberate ice mantles and drive a high-temperature
chemistry; such shocks may be relatively more important for
low-luminosity objects than for high-mass protostars (e.g., van
Dishoeck et al. 1995). It is of considerable interest to establish
if low mass protostars also have hot and dense regions, and if so,
whether a similarly complex organic chemistry to that found in the
case of high-mass protostars has ensued and whether passive heating by the
accretion luminosity or active shocks dominate the liberation of grain
mantles. Since it is the material in the warm inner envelope that
will be incorporated into circumstellar disks, it is important to know
the level of chemical complexity as it relates to forming planetary
systems.
IRAS 16293-2422 is by far the best candidate for investigating a
low mass hot core (e.g., Blake et al. 1994;
van Dishoeck et al. 1995;
Ceccarelli et al. 2000a,b).
IRAS 16293-2422 is a deeply embedded low mass protostellar
object located within the
Ophiuchus molecular cloud
complex. Due to the relative proximity of this source
(160 pc; Whittet 1974) a wealth of molecular lines has been
detected, in spite of its relatively low luminosity
(27
;
Mundy et al. 1986), and this has made IRAS 16293-2422 one of the best studied young stellar objects.
Interferometer observations of radio and millimetre continuum emission
reveal two compact sources in the center of its circumstellar envelope
(Wootten 1989; Mundy et al. 1990; Mundy et al. 1992; Looney et al. 2000), likely to be accretion
disks through which matter is fed onto the central stars.
The separation of the two protostars
is approximately 800 AU (Looney et al. 2000).
IRAS 16293-2422 is thought to be in one of the earliest
stages of formation; the observed spectral energy distribution (SED)
can be fitted by a modified blackbody of
40 K
(e.g., Walker et al. 1986; André et al. 2000) and has a high ratio of
submillimetre to bolometric luminosity, suggesting a large amount of
envelope mass. This places IRAS 16293-2422 among a family of
deeply embedded and recently formed hydrostatic stellar objects known
as, in the traditional evolutionary sequence of low mass protostellar
objects (e.g., André et al. 1993), "class 0''
protostars.
The circumstellar surroundings of this protobinary star were extensively studied in a large molecular line survey presented in Blake et al. (1994) and van Dishoeck et al. (1995). It was found that molecular line emission is potentially a very powerful tool to probe both the physics and chemistry of the circumstellar environment; however, a full radiative transfer analysis was not performed and the derived abundances have significant uncertainties. Due to the complexity of molecular excitation and its sensitivity to the environment, various species - and even different lines of the same species - probe different parts of the circumstellar material. At least three physically and chemically distinct parts were identified including a circumbinary envelope, circumstellar disk(s), and outflow components. The latter component was thought to be a small and warm region of a few arcsec in size where the bipolar outflow(s) interact with the inner part of the circumbinary envelope. Recently, Ceccarelli et al. (2000a,b) used deep JCMT observations of H2CO combined with a physical-chemical collapse model to argue that IRAS 16293-2422 does in fact have a hot-core-like region in which the liberation of ices is consistent with heating by the accretion luminosity.
We present here spherically-symmetric radiative transfer modelling of the dust and gas components constituting the material in the circumstellar envelope of IRAS 16293-2422. The dust parameters are constrained by the observed continuum emission in the form of submillimetre brightness maps and the SED over a large wavelength region. The resulting temperature and density structures are a prerequisite to chemical studies of the molecular gas present in the envelope. The approach taken here is different from that adopted by Ceccarelli et al. (2000a,b) in that the physical parameters of the envelope are derived empirically from the analysis of the dust emission. Once the physical structure of the envelope is known, a detailed excitation analysis of molecular millimetre line emission is performed aimed at obtaining accurate abundances. This provides valuable insight into the complex chemistry occurring in this proto-stellar envelope. In particular, the derived abundances allow for direct comparison with other sources and comets (e.g., Bockelée-Morvan et al. 2000). Moreover, searches for evidence of abundance changes, e.g., due to evaporation of ices ("jump models'') is of considerable interest. In addition to providing constraints on the chemistry, the molecular line observations give further information on the physical structure, e.g., kinematic information. Similar strategies have been adopted by van der Tak et al. (1999,2000b) and Hogerheijde & Sandell (2000) and have proven to be powerful tools when determining the physics and chemistry of star-forming regions.
Copyright ESO 2002