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Table F.2

Disk properties derived from the fit to the emission using a 2D Gaussian fit.

source λ (mm) Fν (mJy) Deconv. major FWHM (au) Deconv. minor FWHM (au) R95 (au) R68 (au)
RCrA IRS7B b 1.3 35.64 ± 0.68 27.54 ± 0.55 11.7 ± 0.30 28.65 ± 0.57 17.66 ± 0.35
3 6.32 ± 0.16 25.37 ± 0.67 10.4 ± 0.34 26.40 ± 0.70 16.27 ± 0.43
RCrA IRS7A 1.3 12.32 ± 0.24 7.02 ± 0.30 3.9 ± 0.21 7.30 ± 0.31 4.50 ± 0.19
3a 6.54 ± 0.25 10.07 ± 0.49 6.1 ± 0.48 10.48 ± 0.51 6.46 ± 0.32
CrA24 3 1.82 ± 0.09 16.21 ± 0.92 4.8 ± 0.54 16.87 ± 0.96 10.40 ± 0.59
CXO 34 1.3 16.27 ± 0.2 18.53 ± 0.27 7.7 ± 0.11 19.28 ± 0.28 11.88 ± 0.17
3 3.62 ± 0.04 17.60 ± 0.23 7.6 ± 0.14 18.31 ± 0.24 11.28 ± 0.15
Elias 29 1.3 13.93 ± 0.04 2.07 ± 0.04 1.8 ± 0.04 2.15 ± 0.04 1.33 ± 0.02
3 4.25 ± 0.02 2.23 ± 0.08 2.0 ± 0.08 2.32 ± 0.08 1.43 ± 0.05
RCrA SMM2 a 3 0.51 ± 0.04 point source point source ≲ 3b ≲ 2b
RCrA SMM2 b 3 0.51 ± 0.046 point source point source ≲ 3 ≲ 2
VLA 1623 Aa 1.3 49.85 ± 0.39 16.42 ± 0.14 9.0 ± 0.09 17.08 ± 0.15 10.53 ± 0.09
3 10.00 ± 0.06 14.32 ± 0.10 7.4 ± 0.09 14.90 ± 0.11 9.18 ± 0.07
VLA 1623 Ab 1.3 45.61 ± 0.38 14.02 ± 0.10 7.2 ± 0.09 14.59 ± 0.10 8.99 ± 0.06
3 9.78 ± 0.06 15.84 ± 0.14 8.6 ± 0.10 16.48 ± 0.15 10.16 ± 0.09
IRAS 16293 A1 1.3 5.90 ± 0.5 ... ... ≲ 6.5c ≲ 4c 0.00
3 4.91 ± 3.6 4.79 ± 2.68 2.8 ± 2.26 4.99 ± 2.79 3.07 ± 1.72
IRAS 16293 A2 1.3 6.00 ± 0.6 ... ... ≲ 12.6c ≲ 7.8c 0.00
3 4.20 ± 0.1 10.58 ± 2.12 6.8 ± 3.53 11.00 ± 2.20 6.78 ± 1.36

Notes.a The 3 mm observations likely contain significant non-thermal emission, and thus the disk size at this wavelength is not reliable.

b The results from the fit is that the source is a point source. Upper limit corresponds to assuming the deconvolved size of the source is a third of the major beam axis. c Imfit could not deconvolve the source from the beam because it was only marginally resolved in just one direction. Values in the table are thus only provided as a reference. They are calculated assuming the deconvolved FWHM of the source is a third of the minor beam axis divided by the cosine of the inclination, the latter derived from the 3 mm observations.

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