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Anna M. M. Scaife, David A. Green, Guy G. Pooley, Matthew L. Davies, Thomas M. O. Franzen, Keith J. B. Grainge, Michael P. Hobson, Natasha Hurley-Walker, Anthony N. Lasenby, Malak Olamaie, John S. Richer, Carmen Rodríguez-Gonzálvez, Richard D. E. Saunders, Paul F. Scott, Timothy W. Shimwell, David J. Titterington, Elizabeth M. Waldram, Jonathan T. L. Zwart, High-resolution AMI Large Array imaging of spinning dust sources: spatially correlated 8 µm emission and evidence of a stellar wind in L675, Monthly Notices of the Royal Astronomical Society: Letters, Volume 403, Issue 1, March 2010, Pages L46–L50, https://doi.org/10.1111/j.1745-3933.2010.00812.x
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Abstract
We present 25 arcsec resolution radio images of five Lynds Dark Nebulae (L675, L944, L1103, L1111 and L1246) at 16 GHz made with the Arcminute Microkelvin Imager (AMI) Large Array. These objects were previously observed with the AMI Small Array to have an excess of emission at microwave frequencies relative to lower frequency radio data. In L675, we find a flat spectrum compact radio counterpart to the 850 μm emission seen with Submillimetre Common-User Bolometer Array (SCUBA) and suggest that it is cm-wave emission from a previously unknown deeply embedded young protostar. In the case of L1246, the cm-wave emission is spatially correlated with 8 μm emission seen with Spitzer. Since the mid-infrared emission is present only in Spitzer band 4 we suggest that it arises from a population of polycyclic aromatic hydrocarbon molecules, which also give rise to the cm-wave emission through spinning dust emission.
1 Introduction
The complete characterization of microwave emission from spinning dust grains is a key question in both astrophysics and cosmology. It probes a region of the electromagnetic spectrum where a number of different astrophysical disciplines overlap. It is important for cosmic microwave background observations in order to correctly characterize the contaminating foreground emission; for star and planetary formation, it is important because it potentially probes a regime of grain sizes that is not otherwise easily observable.
Although a number of objects have now been found to exhibit anomalous microwave emission, attributed to spinning dust, it is still unclear what differentiates those objects from the many other seemingly similar targets that do not show the excess. In the specific case of dark clouds, the recent Arcminute Microkelvin Imager (AMI) sample (AMI Consortium: Scaife et al. 2009, hereinafter Paper I) of 14 Lynds dark nebulae found an excess in only five.
It has been suggested that cm-wave emission from spinning dust is emitted by a population of ultra-small grains (Draine & Lazarian 1998). These ultra-small grains are thought to exist mainly in the form of single polycyclic aromatic hydrocarbon (PAH) molecules. PAH molecules are generally detected through their narrow-line emission features in the mid-infrared (MIR). For these emission features to be observed, the PAH molecules must be exposed to a strong source of UV flux. Since this flux is generally absent in the case of dark clouds, the microwave emission from the rotation of PAH molecules may be the only way to study the very small grain population in these objects.
It is also known that radio continuum emission in dark clouds may arise from ionized gas associated with a stellar outflow. When a luminous star is present, this arises as the result of either a compact H ii region or an ionized stellar wind. In the case of very young low luminosity stars, radio continuum emission may also be detected. In this instance, it is generally attributed to the presence of a partially ionized (0.02 ≤xe≤ 0.35; Bacciotti & Eislöffel 1999) stellar wind (Panagia & Felli 1975; Wright & Barlow 1975) or possibly a neutral wind which has been shock-ionized further from the central source by impacting on a dense obstacle (Curiel et al. 1989).
In this Letter, we present follow-up observations of the five AMI Small Array (SA) spinning dust detections (Paper I) at higher resolution with the AMI Large Array (LA) over the same frequency range. All coordinates in this Letter are J2000.0.
2 Observations
AMI comprises two synthesis arrays, one of 10 3.7-m antennas (SA) and one of eight 13 m antennas (LA), both sited at Lord's Bridge, Cambridge (AMI Consortium: Zwart et al. 2008). The telescope observes in the band 13.5–17.9 GHz from which eight 0.75 GHz bandwidth channels are synthesized. In practice, the two lowest frequency channels (1 and 2) are not generally used due to a lower response in this frequency range and interference from geostationary satellites.
Observations of five Lynds dark nebulae selected from the original AMI SA sample were made in 2009 February–March using the AMI LA. The coordinates of these fields are listed in Table 1 along with the size of the AMI LA synthesized beam towards each object and the rms noise measured outside the primary beam on the cleaned maps. We note that the AMI LA observation of L1246 is towards the northeast of this cloud where anomalous emission was detected by the AMI SA and does not cover the same area as the original Submillimetre Common-User Bolometer Array (SCUBA) observation.
Data reduction was performed using the local software tool reduce (see Paper I for more details). Flux calibration was performed using short observations of 3C 286 near the beginning and end of each run. We assumed I+Q flux densities for this source in the AMI LA channels consistent with the frequency-dependent model of Baars et al. (1977), ≃ 3.3 Jy at 16 GHz. As Baars et al. measure I and AMI LA measures I+Q, these flux densities include corrections for the polarization of the calibrator source derived by interpolating from VLA measurements. A correction is also made for the changing intervening air mass over the observation. The phase was calibrated using interleaved observations of calibrators selected from the Jodrell Bank VLA Survey (JVAS; Patnaik et al. 1992). After calibration, the phase is generally stable to 5° for channels 4–7 and 10° for channels 3 and 8. The full width at half-maximum (FWHM) of the primary beam of the AMI LA is ≈6 arcmin at 16 GHz.
Reduced data were imaged using the AIPS data package. clean deconvolution was performed using the task imagr which applies a differential primary beam correction to the individual frequency channels to produce the combined frequency image. Deconvolved maps were made from both the combined channel set (see Fig. 1) and for individual channels. The broad spectral coverage of AMI allows a representation of the spectrum between 14.3 and 17.9 GHz to be made independently of other telescopes, and in what follows we use the convention S∝ν−α, where S is the flux density, ν is the frequency and α is the spectral index. All errors are quoted to 1σ.
AMI LA combined channel data is shown as grey-scale in units of mJy beam−1, grey contours at −6σ, −3σ, ±2σ, ±1σ and black contours at 3σ, 6σ, 12σ, 24σ etc. SCUBA 850 μm data are shown as red contours with levels as in Visser et al. (2001, 2002) for all the clouds except L1246. The AMI LA observation of L1246 does not cover the region observed by SCUBA. AMI SA data are shown as blue contours with levels as in Paper I. The AMI LA primary beam FWHM is shown as a circle and the synthesized beam as a filled ellipse in the bottom-left corner.
3 Results
L675. The AMI LA observations of L675 show two obvious regions of compact emission (see Fig. 1). The first of these, slightly offset from the pointing centre, is coincident with both the peak of the AMI SA emission and also the compact emission seen at 850 μm by the SCUBA instrument (Visser, Richer & Chandler 2001, 2002). We denote this source ‘A’ (
arcsec). The second, just outside the LA primary beam FWHM to the northeast, is coincident with the probable extragalactic point source identified as ‘B’ (
arcsec) in the original AMI SA observations (Paper I).
Source A is completely unresolved by the AMI LA and shows a flat spectrum across the AMI band, α17.914.3= 0.10 ± 0.36, consistent with free–free emission (see Table 2; Fig. 2). This spectral index differs considerably from that measured by AMI SA. This is because the LA is not sensitive to the large-scale emission seen with the SA. Indeed, it seems likely that the emission seen by the two arrays arises from completely different sources.
Integrated flux densities in mJy for AMI LA observations of L675, L944 and L1246. Errors are calculated as σ =
where σrms is the rms noise in the individual channel map.
L675 source A: data points are flux densities from AMI LA channels 3–8. The best-fitting spectral index of α= 0.10 ± 0.36 is shown as a dashed line.
L944. The original AMI SA observations of L944 revealed a compact region of emission to the north of the cloud, coincident with one side of the protostellar outflow. AMI LA observations (see Fig. 1) reveal that this emission arises not from a point-like object but rather from a diffuse region of emission, the peak of which occurs at
arcsec. We estimate the flux spectrum by integrating the flux density from the primary-beam-corrected channel maps within a 2 arcmin radius of the LA pointing centre. This shows a steeply rising spectrum with α17.914.3=−2.1 ± 0.5. This is consistent with that found from the AMI SA data; however, this correspondence is not meaningful as the low signal-to-noise ratio in the SA data precludes a precise estimate. The flux density found towards this region in the LA map is only marginally lower than that found from the comparatively coarser resolution SA map. This implies that the emission comes not from one smooth extended region that is partially resolved out by the LA baselines, but from a collection of smaller fragments or filaments. These fragments are unresolved by either array, although the granularity becomes more evident in the higher frequency channels of the LA. The amount of flux lost in channels 5–8 relative to channel 4 is significantly smaller than would be expected from a Gaussian source of similar dimensions.
L1103 and L1111. AMI LA observations of L1103 and L1111 do not show any distinct regions of compact cm-wave emission. The diffuse patches of low level emission present within the primary beam towards both sources are indicative of larger scale structures which have been resolved out by the synthesized beam. We can provide an estimate of the flux density seen towards these objects with the LA by fitting and removing a tilted plane base level at the primary beam FWHM. From the combined channel data, this gives S16= 5.1 ± 0.6 mJy and S16= 2.4 ± 0.3 mJy for L1103 and L1111, respectively. These values indicate that the flux loss is considerable: approximately 45 and 96 per cent. The sensitivity of these LA observations is much greater than that of the SA, and it is possible that the patchy emission in these fields corresponds to enhancements in the extended emission which are below the detection threshold in the SA data.
L1246. AMI SA observations towards L1246 did not show any excess emission coincident with the SCUBA identification of the dark cloud, but did reveal a region of emission of ≈2 arcmin to the northeast of the cloud, in a region not covered by the SCUBA map, which had no counterpart in the lower frequency observations. AMI LA observations of this northeast region show an arc of emission (peak:
arcsec; see Fig. 1). We assess the spectral behaviour of this object in two ways. First, we estimate the flux density of the arc itself. We fit and remove a tilted plane base level within an irregular polygon drawn around the object and integrate the remaining flux. Secondly, we fit a tilted plane base level to a circle at the primary beam FWHM and integrate all the flux above this base level within that radius. Both methods give consistent results, as might be expected since the primary beam is relatively empty otherwise. From the first method we find a spectral index α17.915.0=−0.40 ± 0.87, and from the second α17.915.0=−0.47 ± 0.82.
4 Discussion and Conclusions
L675 and L1246 have archival Spitzer Infrared Array Camera (IRAC) data, which show in both cases a significant amount of emission in band 4 (6.4–9.4 μm) and very little in the other three (3.2–3.9, 4.0–5.0 and 4.9–6.4 μm, respectively). In the case of L675, this emission is present on a very large scale (see Fig. 3). The emission seen at 16 GHz with the AMI SA appears on a similar scale; however, the small field of view of the Spitzer data precludes a more detailed comparison. L1246 shows an arc of emission at 16 GHz which is also evident in Spitzer IRAC band 4 (see Fig. 4). This emission is again not present in bands 1–3. In band 4 it is present as an arc, coincident with that seen at 16 GHz in the AMI LA data.
L675: AMI LA combined channel data are shown as white contours at 3σ, 6σ, 12σ etc. Spitzer band 4 data are shown as grey-scale in MJy sr−1 and are saturated at both ends to emphasize the structure present. AMI SA data are shown as blue contours as in Fig. 1.
L1246: AMI LA combined channel data are shown as white contours at 1σ, 2σ, 4σ, 8σ etc. Spitzer band 4 data are shown as grey-scale in MJy sr−1, saturated at both ends of the scale to emphasize the structure present. The AMI LA primary beam is shown as a circle and the synthesized beam as a filled ellipse in the bottom-left corner.
Spitzer band 4 contains two of the PAH emission lines, including the strongest (7.7 μm). Of the three other Spitzer bands, only band 1 contains an emission line (3.3 μm) and for ionized PAHs this line is expected to be significantly weaker. It is probable therefore that the MIR-correlated cm-wave data seen in the AMI maps is a consequence of spinning dust emission from a population of ionized PAH molecules. Neutral PAH molecules do not in general possess a permanent dipole moment and are therefore not expected to have rotational emission (Tielens 2008). This emission, the mechanism of which is described in detail by Draine & Lazarian (1998), arises from the intrinsic dipole moments of small dust grains, most likely to be PAH molecules, which emit power when they rotate. This rotation has a variety of contributing factors, the relative importance of which varies with grain environment. However, in the majority of cases excitation through collision with ions is predominant.
In the case of L675A, we must consider the possibility that we are observing a coincidental extragalactic radio source. Using the extended 9C survey 15 GHz source counts (Waldram et al. 2009), where n(S) = 51(S/Jy)−2.15 Jy−1 sr−1, the probability that a source with flux density greater than 2 mJy lies within the FWHM of the AMI LA primary beam is 0.12 and only 0.01 within the SCUBA field. It is therefore likely that the radio source L675A is associated with the SCUBA core.
A further question is whether the cm-wave emission might be explained by thermal (Planckian) dust emission. A single greybody spectrum with a dust temperature, Td≈ 27 K, might be used to explain the LA flux density; however, it would require a β of 0.6. Such a value would be unusual even for objects known to possess flattened dust tails, such as protoplanetary discs. This simple fit also neglects the flux lost by the AMI LA baseline distribution. SA observations have already shown this source to possess a significant amount of extended emission which would make this scenario even more unlikely.
The presence of a neutral or partially ionized wind from an outflow source that has been shocked through encountering a dense obstacle (Torrelles et al. 1985; Rodríguez et al. 1986) is used to understand the spectral indices seen towards exciting sources in the radio regime (Curiel et al. 1990; Cabrit & Bertout 1992). This model allows a spectral index range from 0.1 (optically thin) to −2 (optically thick), which explains results which deviate from the value of α=−0.6 required by a spherically symmetric ionized wind (Panagia & Felli 1975; Wright & Barlow 1975). Using this model as described in Curiel et al. (1989, 1990) the radio emission is expected to be optically thin (τ= 0.1), consistent with the spectral index seen across the AMI band. Assuming a distance of 300 pc and a stellar wind with a wind speed of 200 km s−1, we can calculate that the AMI flux densities towards L675A are consistent with a mass loss of 3.5 × 10−7 M⊙ yr−1. A mass loss such as this implies a mechanical luminosity from the wind of Lmech≈ 1.1 L⊙, comparable to the values found by Curiel et al. for L1448.
The nature of the emission seen towards L944 with the AMI LA is uncertain. The spectral index of this emission is consistent with spinning dust emission or alternatively the optically thick component of the free–free spectrum. Such a free–free spectrum might be exhibited at 16 GHz by ultra-compact H ii regions. However, a turnover frequency above 16 GHz would have an extremely high mass and should therefore be obvious in sub-mm observations. This needs to be confirmed by either higher radio frequency measurements in order to measure the optically thin region of the spectrum and the turnover or sub-mm measurements to place constraints on the mass of such a region.
In conclusion, we have used the AMI LA to observe a sample of five Lynds dark nebulae selected as candidates for spinning dust emission from the AMI SA sample of Lynds dark nebulae (Paper I). Towards two of these clouds (L1103 and L1111), we detect only patchy diffuse emission characteristic of the presence of a larger structure which has been mostly resolved out.
Towards L675, we have observed flat spectrum compact cm-wave emission coincident with the SCUBA 850 μm emission from the same region. These characteristics suggest that this source is associated with a stellar wind from a deeply embedded young protostar.
We detect extended cm-wave emission to the north of the L944 SMM-1 protostar which displays spectral behaviour consistent with either spinning dust or alternatively a collection of ultracompact H ii regions.
L1246 shows an arc of cm-wave emission which is coincident with emission seen in Spitzer band 4. We suggest that this is an example of emission from a population of PAH molecules, seen in emission lines in the Spitzer data, and emission as a consequence of rapid rotation of the molecules in the cm-wave data.
We request that any reference to this Letter cites ‘AMI Consortium: Scaife et al. 2010’.
Acknowledgments
We thank the staff of the Lord's Bridge Observatory for their invaluable assistance in the commissioning and operation of AMI. AMI is supported by Cambridge University and the STFC. NH-W, CR-G, TWS, TMOF, MO and MLD acknowledge the support of PPARC/STFC studentships. This work is based in part on archival data obtained with the Spitzer Space Telescope, which is operated by the Jet Propulsion Laboratory, California Institute of Technology, under a contract with NASA. Support for this work was provided by an award issued by JPL/Caltech.
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