A&A 462, 211-220 (2007)
DOI: 10.1051/0004-6361:20066255
D. Lommen1 - C. M. Wright2 - S. T. Maddison3 - J. K. Jørgensen4 - T. L. Bourke4 - E. F. van Dishoeck1 - A. Hughes3 - D. J. Wilner4 - M. Burton5 - H. J. van Langevelde6,1
1 - Leiden Observatory, Leiden University, PO Box 9513, 2300 RA Leiden, The Netherlands
2 - School of Physical, Environmental and Mathematical Sciences, UNSW@ADFA, Canberra ACT 2600, Australia
3 - Centre for Astrophysics and Supercomputing, Swinburne University of Technology, PO Box 218, Hawthorn, VIC 3122, Australia
4 - Harvard-Smithsonian Center for Astrophysics, 60 Garden Street, Cambridge, MA 02138, USA
5 - School of Physics, University of New South Wales, Sydney, NSW 2052, Australia
6 - Joint Institute for VLBI in Europe, PO Box 2, 7990 AA Dwingeloo, The Netherlands
Received 17 August 2006 / Accepted 23 October 2006
Abstract
Context. Low-mass stars form with disks in which the coagulation of grains may eventually lead to the formation of planets. It is not known when and where grain growth occurs, as models that explain the observations are often degenerate. A way to break this degeneracy is to resolve the sources under study.
Aims. Our aim is to find evidence for the existence of grains of millimetre sizes in disks around T Tauri stars, implying grain growth.
Methods. The Australia Telescope Compact Array (ATCA) was used to observe 15 southern T Tauri stars, five in the constellation Lupus and ten in Chamaeleon, at 3.3 mm. The five Lupus sources were also observed with the SubMillimeter Array (SMA) at 1.4 mm. Our new data are complemented with data from the literature to determine the slopes of the spectral energy distributions in the millimetre regime.
Results. Ten sources were detected at better than 3
with the ATCA, with
1-2 mJy, and all sources that were observed with the SMA were detected at better than 15
,
with
4 mJy. Six of the sources in our sample are resolved to physical radii of
100 AU. Assuming that the emission from such large disks is predominantly optically thin, the millimetre slope can be related directly to the opacity index. For the other sources, the opacity indices are lower limits. Four out of six resolved sources have opacity indices
1, indicating grain growth to millimetre sizes and larger. The masses of the disks range from <0.01 to 0.08
,
which is comparable to the minimum mass solar nebula. A tentative correlation is found between the millimetre slope and the strength and shape of the 10-
m silicate feature, indicating that grain growth occurs on similar (short) timescales in both the inner and outer disk.
Key words: circumstellar matter - planetary systems: protoplanetary disks - stars: pre-main-sequence
Disks of dust and gas are observed around many young stars. According to the so-called core-accretion model (Safronov & Zvjagina 1969), planetary systems such as our
own Solar System are formed in these circumstellar disks: the solid
particles coagulate to form larger grains, which will grow to eventually form planets. The grains mainly consist of carbon and silicates.
The silicate grains are readily observed through their 10- and 20-m features. Both the change from amorphous to more crystalline grains and the growth of grains
from submicron sizes to sizes of several
m have
been observed by the Infrared Space Observatory
(ISO, van Boekel et al. 2005; Malfait et al. 1998), and more recently by the Spitzer Space Telescope (Kessler-Silacci et al. 2006).
Although the qualitative picture of grain growth has become much clearer over the last few years, several quantitative details are still under discussion. Open questions
include for example the timescale over which grain growth occurs and how this relates to the disk's physical structure (e.g., its temperature and density profile). See
Dominik et al. (2006) for a recent discussion of both laboratory measurements and theoretical modelling of the aggregation of dust in protoplanetary disks.
A large sample of solar-mass T Tauri stars
have recently been observed with the InfraRed Spectrograph (IRS) on board the Spitzer Space
Telescope, in the context of the "Cores to Disks'' (c2d) legacy (Evans et al. 2003) and other programmes.
Most of the sources in the c2d sample show 10- and 20-m amorphous silicate features (Kessler-Silacci et al. 2006), confirming the results of earlier ISO and
ground-based 10-
m observations (e.g., Przygodda et al. 2003; van Boekel et al. 2003), and extending the observed protoplanetary disk sample to lower mass objects.
The data indicate a large variety of silicate profiles, ranging
from strongly peaked silicate bands and steeply rising spectral energy distributions (SEDs) to "boxy'' silicate profiles and flat SEDs. The boxy features with low
feature-to-continuum ratios are interpreted as grain growth to micron size (Bouwman et al. 2001).
One possible explanation for the different spectra and SEDs is that grain growth and the shape of the disk are related. Dullemond & Dominik (2004a) identified a correspondence between the growth of grains in a circumstellar disk and the evolution of the disk from a "flaring'' to a "self-shadowed'' geometry. In their models, the larger, more massive dust grains settle to the midplane of the disks as the grains grow, and the initially flared disks evolve into flatter, self-shadowed disks. To what extent this process is related to the age of the young star is still under debate; there are indications that some young stellar objects evolve more quickly than others.
Numerical models show that the process of settling and coagulation is rapid, being well underway at distances of 1-30 AU from the central star in 104 yr
(e.g., Nomura & Nakagawa 2006). Models predict that the slopes of the SEDs in the millimetre wavelength range will become shallower as the grains in the disk grow to
millimetre (mm) and subsequently centimetre (cm) and larger sizes (Dullemond & Dominik 2004a; D'Alessio et al. 2006).
It is therefore necessary to observe these sources at larger wavelengths than the infrared. Furthermore, millimetre observations probe the entire disk, including the
cold midplane, whereas infrared observations can only probe the hot surface layer of the inner disk.
However, a shallow millimetre slope in itself is not enough evidence for grain growth in the disks, since an excess flux at long wavelengths may also
be caused by a very small, optically thick disk (see, e.g., Beckwith & Sargent 1991). To break this degeneracy it is necessary to resolve the disks to determine their
actual sizes, since if the physical disk size is known, a reasonable estimate of the disk's opacity can be obtained. To resolve the disks around T Tauri stars,
interferometric observations are indispensable.
Considerable progress has been made in this field over the last several years. Wilner et al. (2000) resolved the inner disk of the classical T Tauri star TW Hya in
dust emission at 7 mm using the Very Large Array (VLA). Calvet et al. (2002) did extensive modelling of the SED of this source and showed that the dust grains in the disk must
have grown to sizes
of at least 1 cm. Wilner et al. (2003) used the Australia Telescope Compact Array (ATCA) to study TW Hya at 3.4 mm and found that
a passive two-layer disk (Chiang & Goldreich 1999) provides a reasonable model to explain the observations. Ten T Tauri stars in the Taurus-Auriga star-forming regions were
resolved at 7 mm with the VLA by Rodmann et al. (2006); the majority of these show strong evidence for grain growth to at least millimetre-sized dust.
The more massive counterparts of the T Tauri stars, the Herbig Ae/Be stars, have been studied extensively. Meeus et al. (2001) classified 14 isolated Herbig Ae/Be stars
into two groups based on the shape of the SED.
Disks with a flared outer part of the disk show a rising mid-infrared (20-100 m) excess (Group I in the classification by Meeus et al. 2001), whereas self-shadowed disks have more
modest mid-infrared excesses (Group II). Acke et al. (2004) compared the millimetre slopes for a sample of 26 Herbig Ae/Be stars, based on single-dish data, and found that
Group II sources have in
general a shallower slope, consistent with grain growth to larger sizes than in the Group I sources, and observationally confirming the model predictions from
Dullemond & Dominik (2004a). Natta et al. (2004)
analysed interferometric observations of nine pre-main-sequence stars, mostly Herbig Ae stars, and find that the observations are well explained with dust size distributions
containing boulders of up to metre sizes.
We have used the ATCA to observe 3.3-mm continuum emission from a sample of 15 southern T Tauri stars, five in Lupus and ten in Chamaeleon. Compared with the Taurus star-forming cloud, the T Tauri stars in Lupus and Chamaeleon are generally somewhat older, and the Lupus clouds are much richer in very low mass stars than the other clouds (Hughes et al. 1994). The sources IM Lup and WW Cha were also observed in spectral-line mode to search for HCO+ as a tracer of the molecular gas. The observations of the Lupus sources were followed up with 1.4-mm observations using the SubMillimeter Array (SMA). The sample and the observations are described in Sect. 2. The basic results are presented in Sect. 3 and further discussed in Sect. 4. We will summarize our results and draw some conclusions in Sect. 5.
The ATCA was used to observe 15 southern T Tauri stars (listed in Table 1) at 3.3 mm. The sources were selected to overlap with the sample observed in the c2d programme. We furthermore selected sources with strong 1.3-mm fluxes (Nürnberger et al. 1997; Henning et al. 1993) to improve the chances of detection at 3.3 mm.
The distances used in this work are 150
20 pc to Lupus I (HT Lup, GW Lup) and Lupus II (IM Lup, RU Lup), 200
20 pc to Lupus III (HK Lup) (Comerón 2006),
and 160
15 pc to Chamaeleon I (Whittet et al. 1997). The distances to most of these pre-main-sequence stars are not very well constrained (see, e.g., van Kempen et al. 2007; Comerón 2006, for discussions on the distances to the Lupus clouds).
The distance to the isolated source T Cha, however, is known to be closer at
66+19-12 pc (Hipparcos, van den Ancker et al. 1998).
ATCA observations were carried out in July 2003, October 2004,
and August 2005. All sources were observed at 3.3-mm continuum in double sideband. The
primary beam of the ATCA antennas is
at 3 mm. Each sideband consisted of 32 channels and had an effective total bandwidth of 128 MHz.
Furthermore, the sources WW Cha and IM Lup were observed in a dual mode: the lower sideband was a 512-channel band with an effective total bandwidth of 8 MHz to provide
high-frequency resolution for detection of the HCO+ J = 1-0 line, and the upper sideband was used as a wideband channel with again 32 channels and a total bandwidth
of 128 MHz. These two sources were observed for a complete track to reach a similar rms noise in the continuum as that for the other sources, and to maximize the
possibility of detecting the HCO+ J = 1-0 line.
The resulting velocity resolution of the narrow-band observations was 0.11 km s-1, the velocity coverage was
24 km s-1.
The ATCA was in the EW214 configuration at the time of the observations in 2003 (three antennas equipped with 3-mm receivers, baselines of 31-107 m) and in the H214C configuration in 2004 and
2005 (five antennas, baselines of 82-247 m).
The data were calibrated and reduced with the MIRIAD package (Sault et al. 1995). The quasars PKS 1622-297 and PKS 1057-797 served as gain calibrators
for the Lupus and
Chamaeleon sources, respectively, and the absolute fluxes were calibrated on Mars or Uranus. The calibration is estimated to have an uncertainty of
20%. The
passbands were calibrated on the quasars PKS 0537-441 and PKS 1253-055.
Table 1: Source list of sources observed with the ATCA.
The phase centre was offset from the source position by
to avoid
possible artefacts. There was some overlap in the samples that were observed in the three runs.
The 2004 data suffered badly from unstable weather and were not used in the analysis,
whereas the 2003 and 2005 data were consistent.
In 2003, there were only three ATCA antennas fitted with 3-mm receivers, resulting in a large and elongated beam. Five antennas with 3-mm receivers were available in
2005, greatly
improving the resolution and beam shape of our observations. With the exception of HK Lup, which was only observed in 2003, we decided to use only the 2005 data for our
analysis. For an overview of the ATCA observations, see Table 2.
Table 2: Overview of the observations.
Table 3: Basic results of ATCA observations at 3.3 mm.
The five Lupus sources in our sample were observed in double-sideband continuum (217 and 227 GHz, primary beam
)
with the SMA
(Ho et al. 2004) on 28 April 2006. The data from
both sidebands were combined, giving an effective bandwidth of 3 GHz. The SMA was in the compact configuration and baselines ranged from 5 to 52 m. The low elevation of
the sources as seen from Mauna Kea and the relatively short integration time of
30 min per source resulted in a rather elongated beam of
9
2.5 arcsec
(natural weighting). The raw visibility data were calibrated and flagged with MIR, and
the calibrated visibility data were analysed with MIRIAD. The gains were calibrated on the quasar PKS 1622-297, and the absolute fluxes and correlator passbands were calibrated
on Uranus with an expected uncertainty of
20%.
All eight antennas of the array were available at the time of the observations. For an overview of the SMA observations, see Table 2.
From the 15 sources that were observed with the ATCA in 2003 and 2005, ten were detected at better than 3,
with 3.3-mm fluxes ranging from
6 mJy up to
30 mJy. For those objects, both point sources and circular Gaussians were fitted in the (u, v) plane, the results of which are presented in Table 3.
Those sources that were detected at better than 5
are shown in Fig. 1, overplotted on 2MASS K-band (2.1
m) images. The positions of the
infrared sources and the millimetre peaks agree very well.
Table 4 presents the results of the SMA 1.4-mm observations of the Lupus sources, which were all detected at better than 15,
with fluxes
ranging from
70 mJy up to
210 mJy.
For comparison, the SEST 1.3 mm single-dish fluxes from Nürnberger et al. (1997) are also shown.
A plot of the visibility amplitude as a function of baseline for each of our target sources is presented in Figs. 2 and 3. An amplitude that decreases as a function of baseline indicates a resolved source, suggesting that at least some of our sources are resolved. Note that in principle the resolved structure could be the protoplanetary disk, or the remnant centrally-condensed envelope around it. One can distinguish between the two by looking in more detail at the shape of the amplitude vs. (u, v) distance curves. A disk shows a shallower profile at shorter baselines, levelling off to the flux of the integrated disk emission. A power-law envelope shows a flux that increases steeply towards the shortest baselines, and the total integrated flux can only be obtained with single-dish telescopes, observing with a larger beam. An illustrative example is provided by Fig. 3 in Jørgensen et al. (2005), who need a disk and an envelope to explain the amplitude as a function of baseline for the deeply embedded class 0 source NGC 1333 IRAS 2A.
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Figure 1:
ATCA images of the
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Table 4: Basic results of SMA observations at 1.4 mm. For comparison, the SEST 1.3 mm single-dish fluxes from Nürnberger et al. (1997) are shown.
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Figure 2:
Amplitude vs. (u, v) distance for sources observed with the ATCA. The data points give the vector-averaged amplitude per
bin, where the data are binned in annuli according to (u, v) distance. The error bars show the statistical ![]() |
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Figure 3: Same as Fig. 2 for sources observed with the SMA. |
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The amplitude vs. (u, v) distance plot for KG 49 (Cha IRN) appears to indicate a resolved envelope rather than a disk. This is in line with the results of
Henning et al. (1993) who find that the SED from 1 m to 1 mm cannot be fitted with a disk, but is consistent with a spherically symmetric model with constant
density and
mag. Furthermore, all other sources show silicates in emission around 10
m, which is indicative of a disk without significant foreground
absorption. KG 49 on the other hand does not show silicate emission around 10
m. However, it does show bands of H2O, CO, and CO2 ice
(Pontoppidan et al. 2003; Gürtler et al. 1999), which can be explained by a cold envelope.
It thus appears that KG 49 is not a genuine T Tauri star, but a less evolved object that is still embedded in an envelope. We will therefore disregard KG 49 in the
further analysis in this work.
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Figure 4:
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We consider a source to be resolved if the integrated flux of the fitted Gaussian is at least 2
higher than the flux obtained from a point-source fit (see
Tables 3 and 4). Note that for a point source the peak flux density equals the integrated flux.
According to this definition, five of the detected sources (KG 49, WW Cha, HT Lup, IM Lup, RU Lup) are resolved by the ATCA, and three of the Lupus sources (IM Lup, RU Lup, HK Lup)
are resolved by the SMA. In the case of KG 49 it is the envelope that is resolved, in the other cases the disks.
Table 5: SEST 1.3 mm fluxes from the literature, mm slopes, derived opacity indices, and disk masses.
At low frequencies, i.e., in the Rayleigh-Jeans regime, the flux density, ,
is
related to frequency,
,
by a power law:
.
One can determine the dust opacity index,
,
where
,
from the observed spectral index,
,
through
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(1) |
Due to the frequency dependence of the dust opacity, protoplanetary disks are generally
optically thick at short wavelengths and optically thin at long wavelengths. Optically thick
emission cannot be neglected in the inner disk where column densities get very high, even at
very long wavelengths. The ratio of optically thick
to optically thin emission coming from the disk is given by
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(2) |
The spectral index
and the opacity index
were determined from the ATCA 3.3-mm fluxes and SEST 1.3-mm
fluxes from the literature (Nürnberger et al. 1997; Henning et al. 1993).
The uncertainties in
and
are typically 0.5, due to both the large uncertainties in the absolute fluxes of the data points
and to the relatively short wavelength range over which
was determined. For the Lupus sources,
was also determined with the SMA 1.4-mm fluxes included, giving consistent
results. The robustness of the value for
is illustrated by Fig. 4,
which shows the integrated fluxes from this work and single-dish (sub)millimetre fluxes from the
literature for RU Lup (Nürnberger et al. 1997; Weintraub et al. 1989), along with the fitted
slope:
0.1. We thus find that the formal uncertainties in
and
for the other sources are probably
overestimates. Unfortunately, RU Lup is the only source for which currently observations at such short wavelengths are available.
The low error in the fit to its data points illustrates that more observations,
preferably over a larger wavelength regime, will help to better constrain values for
,
and hence
.
The values for
and
for the sources in our sample are presented in Table 5. Figure 5 shows the cumulative fraction of sources with given dust-opacity indices for our sample and that of Rodmann et al. (2006). Rodmann et al. corrected for the contribution of free-free radiation at 7 mm. We estimate
the contribution of free-free radiation to be
5% at 3.3 mm, and hence it is not necessary to correct for it at this wavelength. Figure 4 illustrates that contamination from free-free emission is not an issue for RU Lup. The Kolmogorov-Smirnov test gives a probability of 58% that Rodmann et al.'s and our groups are drawn from the same distribution.
However, the uncertainties in
are still quite large, and are not taken into account by the standard Kolmogorov-Smirnov test.
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Figure 5:
Cumulative number of sources with an opacity index less than a given value of ![]() |
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For optically thin disks, the disk mass
is directly proportianal to the flux
(see, e.g., Natta et al. 2000; Hildebrand 1983):
Both IM Lup and WW Cha were observed in spectral-line mode to search for HCO+ J = 1-0 emission. In general, CO is a more easily detectable gas tracer in the
millimetre regime, but
since the ATCA does not presently have the capability to observe at frequencies above 106 GHz, HCO+ was used to investigate the gas component of disks. We
tentatively detect HCO+ at 0.05 Jy beam-1 in IM Lup, as presented in Fig. 6.
Van Kempen et al. (2007) detected a double-peaked feature, consistent with a rotating gas disk, using JCMT observations of the 12CO J = 3-2 line. However, they
find the line at
1 km s-1 lower velocity. The cause of this discrepancy is unclear.
A ray-tracing programme (Hogerheijde & van der Tak 2000) was used to compute the line profile of HCO+ J = 1-0, using the model for IM Lup
described in van Kempen et al. (2007). The abundance of HCO+ was set to be 10-8 with respect to H2 in areas with temperatures above 30 K, and 10-12 in
areas with temperatures below 30 K.
An intensity of 0.02 Jy beam-1 was predicted, consistent with the observations within the uncertainties.
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Figure 6:
Spectrum of HCO+ J = 1-0 line emission observed from IM Lup, at the position of the peak continuum emission, binned to 0.44 km s-1 velocity resolution, in the
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No HCO+ line emission is detected to a limit of 97 mJy beam-1 (3)
in the direction of WW Cha. Combining our new results with those of Wilner et al. (2003)
who detected HCO+ in TW Hya, but not in
HD 100546, we have two detections of HCO+ and two non-detections.
Data for more targets are required, in order to determine whether the presence of HCO+ is related to the disk's evolutionary state.
About half the sources that are detected are spatially resolved. The inferred physical sizes (disk radii of 100 AU) indicate that the emission coming from the disks
is predominantly optically thin at millimetre wavelengths. This is illustrated by the work of
Testi et al. (2001), who do detailed modeling of the Herbig Ae stars UX Ori and CQ Tau, and find that disk radii of
100 AU, combined with millimetre
slopes of
3 and 1.3 mm fluxes of
102 mJy, are well explained by an opacity index
.
If we assume that all
sources in our sample are optically thin at millimetre wavelengths, the opacity index
can be determined. Seven out of ten detected sources have
,
which can
be naturally explained by grain growth to millimetre and centimetre sizes (Draine 2006).
Our values for
indicate grain growth to sizes of millimetres and larger in the outer disks. The surface layers of the inner disks can be probed by infrared
observations and, as noted in Sect. 1, the 10-
m feature indicates the growth of grains through changes in its strength and shape.
In Fig. 7 we compare the millimetre slope
as derived in Sect. 3 with the "strength'' or peak 10-
m flux (
)
and to the "shape'' or the ratio of the 11.3 to 9.8
m flux (
)
of the 10-
m silicate feature for those sources in our sample that overlap with the samples of Przygodda et al. (2003) and Kessler-Silacci et al. (2006). Here the normalized 10-
m spectra
are given by
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Figure 7:
Slope in the millimetre regime vs. the peak 10-![]() ![]() ![]() |
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On the other hand, while a significant fraction of the dust has already grown to sizes of millimetres and centimetres, the infrared data indicate that micron-sized
grains are also still present, at least in the surface layers. This
may be explained by assuming that not only grain growth, but also aggregate fragmentation takes place in the disks (Dullemond & Dominik 2005). After about 104 years a semi-stationary state is reached for sizes below cm, which may last for several 106 years.
Note that Fig. 7 shows a trend rather than a bimodal distribution. Dullemond & Dominik (2005) suggest fragmentation of grains to allow for the
semi-stationary state that is observed in the disks around T Tauri stars.
If the correlation between the 10-m feature and the millimetre slope
is confirmed by a more extensive dataset, it would indicate
that when aggregates are fragmented in collisions, the size of the fragments increases as the aggregate sizes increase. Hence, when the
largest particles grow from millimetre to centimetre sizes, the submicron-sized grains are no longer replenished, and the 10-
m feature - tracing the
upper layers of the disk where the stirred-up small particles reside - flattens while the millimetre slope - which traces the midplane where the largest particles are
present - becomes shallower.
We also compared
to the spectral index over the 13 to 35
m range from Kessler-Silacci et al. (2006). However,
could only be determined for five of the sources in
Kessler-Silacci et al., and no obvious correlation is found for this small sample.
It is interesting to note that Acke & van den Ancker (2004) do not find a correlation between the 10-m silicate feature and the (sub)millimetre spectral index for
their sample of 26 Herbig Ae/Be stars. On the other hand, Acke et al. (2004) do find a correlation between the shape of the mid-IR (12-60
m) SED and the
(sub)millimetre slope in their sample. They interpret this finding as a correlation between disk geometry and grain size: as grains grow, the disk structure evolves from
flared to geometrically flat (see, e.g., Dullemond 2002). For the twelve sources in our sample for which it was possible to determine
,
we determined the non-colour-corrected IRAS [12]-[60] colour and compared this to
.
No clear correlation was found, consistent with the above lack of correlation with the 13-35
m spectral index.
This may indicate that grain growth has a less dramatic effect on the geometry
of disks around the low-mass T Tauri stars than on the intermediate-mass Herbig Ae/Be stars, or that IRAS fluxes are contaminated by other (extended) emission
in the large IRAS beams.
Natta et al. (2004) did a study similar to ours for a sample of six isolated Herbig Ae stars and three T Tauri stars. They estimated
in two different ways,
firstly using only interferometric data, and secondly with single-dish data included. Their results are included in Fig. 5, where the values for
with the
single-dish data included were used for comparison.
According to the Kolmogorov-Smirnov test there is a 65% probability that the sample of Natta et al. and our sample are drawn from the same distribution.
It is interesting to note that in general the sources in Natta et al.'s sample are considerably older than those sources in the current work and that of Rodmann et al. (2006).
This may be an extra indication that the size distribution of grains in protoplanetary disks remains stationary for several Myr once sizes of millimetres are reached.
We used the ATCA to make interferometric observations of fifteen southern T Tauri sources at 3.3 mm. Ten of the sources are located in Chamaeleon, the remaining five in Lupus. The Lupus sources were also observed at 1.4 mm with the SMA. The main results are as follows.
The capability to observe the continuum across a 2 GHz bandwidth, as opposed to the current 128 MHz, will provide a marked increase in sensitivity, allowing more disks to be detected. Furthermore, as the new generation of (sub)millimetre interferometers, notably eSMA, CARMA, and ALMA, becomes available to the scientific community, it becomes possible to resolve the circumstellar disks at millimetre and submillimetre wavelengths down to subarcsecond scales. A survey of a large sample of objects, in different clouds, and at higher resolution will greatly enhance our understanding of the timescale for grain growth and the building of planetary systems as a function of disk radius.
Acknowledgements
We would like to thank the ATNF for their hospitality and assistance, and specifically Tony Wong for extensive assistance during the observations and the data reduction. SMA staff, in particular Alison Peck, are thanked for scheduling observations of the Lupus sources as a filler programme and for carrying out the observations. Partial support for this work was provided by a Netherlands Research School For Astronomy network 2 grant, and by a Netherlands Organisation for Scientific Research Spinoza grant. C.M.W. acknowledges financial support from an ARC Australian Research Fellowship. We are grateful to Jackie Kessler-Silacci for providing us with infrared data, and to Tim van Kempen for useful discussions on IM Lup and calculating the HCO+ emission in his model. Finally, we would like to thank our referee, Claire Chandler, for useful comments that significantly improved this paper.