XUE. JWST spectroscopy of externally irradiated disks around young intermediate-mass stars

TL;DR

This study uses JWST spectroscopy to analyze the physical and chemical properties of disks around young intermediate-mass stars in irradiated environments, revealing their potential for rocky planet formation despite external UV influence.

Contribution

First detailed characterization of inner disks around young intermediate-mass stars exposed to external irradiation using JWST, showing their chemical richness and potential for rocky planet formation.

Findings

Disks show molecular richness comparable to isolated T Tauri systems.

Most disks exhibit water emission indicating potential for rocky planet formation.

External UV irradiation appears to truncate disks without significantly affecting inner disk chemistry.

Abstract

Most young stars and therefore planetary systems form in high-mass star forming regions and are exposed to ultraviolet radiation, affecting the protoplanetary disk. These regions are located at large distances and only now with JWST become accessible to study the inner disks surrounding young stars. We present the eXtreme UV Environments (XUE) program, which provides the first detailed characterization of the physical and chemical properties of the inner disks around young intermediate-mass stars exposed to external irradiation from nearby massive stars. We present high signal to noise MIRI-MRS spectroscopy of 12 disks located in three sub-clusters of the high-mass star-forming region NGC 6357. Based on their mid-infrared spectral energy distribution, we classify the XUE sources into Group I and II based on the Meeus scheme. We analyze their molecular emission features, and compare their spectral indices and 10 $\mu$m silicate emission profiles to those of nearby Herbig and intermediate T Tauri disks. Despite being more massive, the XUE stars host disks with molecular richness comparable to isolated T Tauri systems. The 10 $\mu$m silicate features show lower F$_{11.3}$/F$_{9.8}$ ratios at a given F$_{\mathrm{peak}}$, but current uncertainties prevent conclusions about their inner disk properties. Most disks display water emission from the inner disk, suggesting that even in these extreme environments rocky planets can form in the presence of water. The absence of strong line fluxes and other irradiation signatures suggests that the XUE disks have been truncated by external UV photons. However, this truncation does not appear to significantly impact the chemical richness of their inner regions. These findings indicate that even in extreme environments, IMTT disks can retain the ingredients necessary for rocky planet formation.