Planets form in protoplanetary disks and inherit their chemical compositions.
It is thus crucial to map the distribution and investigate the formation of
simple organics, such as formaldehyde and methanol, in protoplanetary disks. We
analyze ALMA observations of the nearby disk-jet system around the T Tauri star
DG Tau in the o-H2CO 31,2−21,1 and CH3OH 3−2,2−4−1,4 E,
50,5−40,4 A transitions at an unprecedented resolution of ∼0.15",
i.e., ∼18 au at a distance of 121 pc. The H2CO emission originates from
a rotating ring extending from ∼40 au with a peak at ∼62 au, i.e., at
the edge of the 1.3mm dust continuum. CH3OH emission is not detected down to
an r.m.s. of 3 mJy/beam in the 0.162 km/s channel. Assuming an ortho-to-para
ratio of 1.8-2.8 the ring- and disk-height-averaged H2CO column density is
∼0.3−4×1014 cm−2, while that of CH3OH is
<0.04−0.7×1014 cm−2. In the inner 40 au no o-H2CO emission
is detected with an upper limit on its beam-averaged column density of
∼0.5−6×1013 cm−2. The H2CO ring in the disk of DG Tau is
located beyond the CO iceline (RCO∼30 au). This suggests that the
H2CO abundance is enhanced in the outer disk due to formation on grain
surfaces by the hydrogenation of CO ice. The emission peak at the edge of the
mm dust continuum may be due to enhanced desorption of H2CO in the gas phase
caused by increased UV penetration and/or temperature inversion. The
CH3OH/H2CO abundance ratio is <1, in agreement with disk chemistry
models. The inner edge of the H2CO ring coincides with the radius where the
polarization of the dust continuum changes orientation, hinting at a tight link
between the H2CO chemistry and the dust properties in the outer disk and at
the possible presence of substructures in the dust distribution.Comment: 8 pages, 6 figures, accepted for publication on A&A Letter