APEX survey of interstellar HCl: $^{35}$Cl/$^{37}$Cl isotopic ratios in dense cores and outflows

TL;DR

This study systematically measured the $^{35}$Cl/$^{37}$Cl isotopic ratio in dense star-forming regions, revealing its consistency with Galactic chemical evolution models and detecting HCl in outflows, thus expanding understanding of interstellar chlorine chemistry.

Contribution

It provides the first extensive survey of interstellar HCl isotopic ratios across multiple regions, enhancing knowledge of Galactic chemical evolution and chlorine distribution in star-forming environments.

Findings

H$^{35}$Cl detected in all sources

Isotopic ratios between 1.6 and 3.5

H$^{35}$Cl found in outflows, especially explosive ones

Abstract

Despite being only the 19th most abundant element in the interstellar medium, chlorine's reactivity and volatility give rise to a unique interstellar chemistry, favouring the formation of several chlorine-bearing hydrides. Further, the $^{35}\text{Cl}/ ^{37}$Cl ratio probes nucleosynthesis across the Galaxy. Yet, studies of Cl-bearing molecules have remained limited to a few sightlines due to observational challenges. We systematically investigated the Galactic distribution of HCl and the [H$^{35}$Cl]/[H$^{37}$Cl] ratio in high-mass star-forming regions. As a probe of a region's nucleosynthesis history, this ratio may constrain predictions of Galactic chemical evolution models. We observed the ground-state $J=1$$-$0 lines of H$^{35}$Cl and H$^{37}$Cl toward 28 high-mass star-forming regions with SEPIA660 on APEX, more than doubling the number of known HCl detections and revealing with XCLASS models emission from both cores and outflows. H$^{35}$Cl was detected in all sources, H$^{37}$Cl in all but two, with spectral line profiles ranging from those with only emission to complex emission-absorption mixtures. We find column densities of the order of $10^{13}\,\mathrm{cm}^{-2}$ for H$^{35}$Cl and isotopic ratios between $1.6$ and $3.5$ in emission-only sources. The derived [H$^{35}$Cl]/[H$^{37}$Cl] aligns with Galactic chemical evolution models and shows no trend with Galactocentric radius. However, local variations may reflect recent nucleosynthesis. Overall, the results suggest that most Galactic chlorine was synthesized during epochs of lower average metallicity in the Galaxy. Notably, we detect H$^{35}$Cl emission arising from outflows - particularly explosive ones - hinting at its presence in a broader range of environments. The present single-dish observations cannot reveal the origin of HCl in outflows; necessitating interferometric follow-up observations.