Elucidating isotope exchange between atmospheric trace molecular species is important for environment monitoring, climate control studies, and a fundamental understanding of atmospheric chemistry. Here, we provide direct experimental evidence of oxygen-isotopic exchange between carbon dioxide (CO) and nitrogen dioxide (NO), which are simultaneously emitted into the atmosphere from common sources. A combined near-infrared and UV-vis optical cavity-enhanced experimental investigation along with quantum-chemical calculations followed by a reaction modeling study revealed that CO and NO can communicate isotopically by near-ultraviolet-driven NO photolysis. Our results found evidence for a near-barrierless (1.67 kcal/mol) nitrate-containing complex having a very short lifetime (∼13 ns) which facilitates the transfer of O-isotopes from OCO to NOO, leading to isotopic depletion of O in OCO, thus opening a new gas-phase isotope-selective chemical transformation mechanism in the lower atmosphere. This isotope exchange study may serve as a new window into the fundamental understanding of isotopic photochemistry, oxygen isotopic fractionations, and climate modeling.
Download full-text PDF |
Source |
---|---|
http://dx.doi.org/10.1021/acs.jpclett.4c00485 | DOI Listing |
Enter search terms and have AI summaries delivered each week - change queries or unsubscribe any time!