Herschel / HIFI observations of CO, H2O and NH3 in Mon R2

TL;DR

This study uses Herschel and IRAM observations to analyze the distribution and abundance of water and ammonia in the Mon R2 ultracompact HII region, revealing complex kinematics and chemistry influenced by UV irradiation.

Contribution

It provides the first detailed analysis of H2O and NH3 abundances in Mon R2 using combined observational data and modeling, highlighting the role of PDR dynamics.

Findings

H2O abundance is ~10^-8 in the PDR and higher (~10^-7) in high velocity wings.

NH3 is mainly found in the envelope with an abundance of ~2x10^-9.

The PDR model explains water abundance if outflows are considered minor.

Abstract

Context. Mon R2 is the only ultracompact HII region (UCHII) where the associated photon-dominated region (PDR) can be resolved with Herschel. Due to its brightness and proximity, it is the best source to investigate the chemistry and physics of highly UV-irradiated PDRs. Aims. Our goal is to estimate the abundance of H2O and NH3 in this region and investigate their origin. Methods. We present new observations obtained with HIFI and the IRAM-30m telescope. Using a large velocity gradient approach, we model the line intensities and derive an average abundance of H2O and NH3 across the region. Finally, we model the line profiles with a non-local radiative transfer model and compare these results with the abundance predicted by the Meudon PDR code. Results. The variations of the line profiles and intensities indicate complex geometrical and kinematical patterns. The H2O lines present a strong absorption at the ambient velocity and emission in high velocity wings towards the HII region. The spatial distribution of the o-H2^18O line shows that the its emission arises in the PDR surrounding the HII region. By modeling the o-H2^18O emission we derive a mean abundance of o-H2O of ~10^-8 relative to H2. The ortho-H2O abundance is however larger, ~1x10^-7, in the high velocity wings. Possible explanations for this larger abundance include an expanding hot PDR and/or an outflow. Ammonia seems to be present only in the envelope with an average abundance of ~2x10^-9 relative to H2. Conclusions. The Meudon PDR code can account for the measured water abundance in the high velocity gas as long as we assume that it originates from a <1 mag hot expanding layer of the PDR, i.e. that the outflow has only a minor contribution to this emission. To explain the abundances in the rest of the cloud the molecular freeze out and grain surface chemistry would need to be included.