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 (CO2) and nitrogen dioxide (NO2), 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 CO2 and NO2 can communicate isotopically by near-ultraviolet-driven
NO2 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 18O-isotopes
from 18O12C16O to N16O16O, leading to isotopic depletion of 18O in 18O12C16O, 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.