CO+ as a probe of the origin of CO in diffuse interstellar clouds
Maryvonne Gerin, Harvey Liszt

TL;DR
This study used ALMA observations to search for CO+ in diffuse interstellar clouds, finding non-detections that support a chemical pathway where HCO+ forms mainly from reactions involving oxygen and carbon hydrides, not CO+.
Contribution
The paper provides the first sensitive upper limits on CO+ in diffuse clouds, clarifying its role in interstellar chemistry and supporting specific formation pathways for HCO+.
Findings
CO+ was not detected, with upper limits set on its abundance.
HCO+ is mainly produced from reactions involving oxygen and carbon hydrides.
The results support a chemical scheme where CO+ and HOC+ form from reactions of C+ with OH and H2O.
Abstract
The chemistry of the diffuse interstellar medium is driven by the combined influences of cosmic rays, ultraviolet (UV) radiation, and turbulence. Previously detected at the outer edges of photodissociation regions (PDRs) and formed from the reaction of C+ and OH, CO+ is the main chemical precursor of HCO+ and CO in a thermal, cosmic-ray, and UV-driven chemistry. Our aim was to test whether the thermal cosmic-ray and UV-driven chemistry is producing CO in diffuse interstellar molecular gas through the intermediate formation of CO+ We searched for CO+ absorption with the Atacama Large Millimeter Array (ALMA) toward two quasars with known Galactic foreground absorption from diffuse interstellar gas, J1717-3342 and J1744-3116, targeting the two strongest hyperfine components of the J=2-1 transition near 236 GHz. We could not detect CO+ but obtained sensitive upper limits toward both…
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