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Table B.1

Properties of the detected lines – Comparison with those of ASAI.

Survey Species Transition RMS [mK] 10kms15kms1TBdv$\int_{-10\, \rm{km\, s}^{-1}}^{5\,\rm{km\, s}^{-1}} T_{\rm B}\, dv$ [K km s−1] N [cm−2]
CH2OHCHO 80,8 – 71,7 0.9 0.04 ± 0.03 (1.4 ± 1.3) × 1013
CH2OHCHO 81,8 – 70,7 0.6 < 0.04 < 1.4 × 1013
ASAI CH2OHCHO 101,10 – 90,9 1.1 0.05 ± 0.04 (1.1 ± 0.9) × 1013
C2H5 OH 70,7 — 61,6, anti 1.1 0.11 ± 0.04 (6.5 ± 2.6) × 1013
ch2OHCHO 80,8 – 71,7 0.6 0.06 ± 0.01 (2.3 ± 1.3) × 1013
CH2OHCHO 81,8 – 70,7/p> 0.6 < 0.02 < 1 × 1013
NOEMA CH2OHCHO 101,10 – 90,9 1.0 0.11 ± 0.02 (2.4 ± 1.2) × 1013
C2H5OH 70,7 – 61,6, anti 1.1 0.11 ± 0.02 (5.5 ± 3.6) × 1013

Notes. The velocity integrated intensities computed using the NOEMA data and reported in the 5th column were averaged over the IRAM-30m half-power beam, used in ASAI. The column densities in column six were computed using the ASAI (upper part) and NOEMA (bottom part) data, and considering a beam dilution factor for a source of 20″. We derived those quantities assuming LTE and an excitation temperature of 30 K. The uncertainties associated include the 1σ noise RMS and a 10% error on the flux calibration. Please note that because the flux was integrated over a larger area, the RMS given in this table differs from the value reported in Tab. 2.

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