MINDS. JWST-MIRI reveals a peculiar CO2-rich chemistry in the drift-dominated disk CX Tau
Abstract
Radial drift of icy pebbles can have a large impact on the chemistry of the inner regions of protoplanetary disks. Compact dust disks (50 au) are suggested to have a higher (cold) H2O flux than more extended disks, likely due to efficient radial drift bringing H2O-rich material to the inner disk, where it can be observed with JWST. We present JWST MIRI/MRS observations of the disk CX Tau taken as a part of the Mid-INfrared Disk Survey (MINDS) GTO program, a prime example of a drift-dominated disk. This compact disk seems peculiar: the source possesses a bright CO2 feature instead of the bright H2O expected based on its efficient radial drift. We aim to provide an explanation for this finding. We detect molecular emission from H2O, 12CO2, 13CO2, C2H2, HCN, and OH in this disk, and even demonstrate a potential detection of CO18O. Analysis of the 12CO2 and 13CO2 emission shows the former to be tracing a temperature of 450 K, whereas the 13CO2 traces a significantly colder temperature (200 K). H2O is also securely detected both at shorter and longer wavelengths, tracing a similar temperature of 500-600 K as the CO2 emission. We also find evidence for a colder, 200 K H2O component at longer wavelengths, which is in line with this disk having strong radial drift. The cold 13CO2 and H2O emission indicate that radial drift of ices likely plays an important role in setting the chemistry of the inner disk of CX Tau. Potentially, the H2O-rich gas has already advected onto the central star, which is now followed by an enhancement of comparatively CO2-rich gas reaching the inner disk, explaining the enhancement of CO2 emission in CX Tau. The comparatively weaker H2O emission can be explained by the source's low accretion luminosity. (abridged)
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