2024/07/06 by Milou Temmink, Temmink, Milou, E. F. van Dishoeck +31
Earth and Planetary Sciences · Physics and Astronomy · #Astronomy and Astrophysical Research #Earth and Planetary Astrophysics (astro-ph.EP) #FOS: Physical sciences #Geophysics and Gravity Measurements #Pulsars and Gravitational Waves Research
paper · pdf · doi:10.48550/arxiv.2407.05070
openalex publication_date 2024/07/06 · openalex created_date 2024/07/10 · openalex updated_date 2026/07/28
The MRS mode of the JWST-MIRI instrument gives insights into the chemical richness and complexity of the inner regions of planet-forming disks. Here, we analyse the H2O-rich spectrum of the compact disk DR Tau. We probe the excitation conditions of the H2O transitions observed in different wavelength regions across the entire spectrum using LTE slab models, probing both the rovibrational and rotational transitions. These regions suggest a radial temperature gradient, as the excitation temperature (emitting radius) decreases (increases) with increasing wavelength. To explain the derived emitting radii, we require a larger inclination for the inner disk (i~20-23 degrees) compared to the outer disk (i~5 degrees), agreeing with our previous analysis on CO. We also analyse the pure rotational spectrum (<10 micron) using a large, structured disk (CI Tau) as a template, confirming the presence of the radial gradient, and by fitting multiple components to further characterise the radial and vertical temperature gradients present in the spectrum. At least three temperature components (T~180-800 K) are required to reproduce the rotational spectrum of H2O arising from the inner ~0.3-8 au. These components describe a radial temperature gradient that scales roughly as ~R-0.5 in the emitting layers. As the H2O is mainly optically thick, we derive a lower limit on the abundance ratio of H2O/CO~0.17, suggesting a potential depletion of H2O. Similarly to previous work, we detect a cold H2O component (T~180 K) originating from near the snowline. We cannot conclude if an enhancement of the H2O reservoir is observed following radial drift. A consistent analysis of a larger sample of compact disks is necessary to study the importance of drift in enhancing the H2O abundances.