posted on 2024-01-31, 12:03authored byZeyi Moo, Peizhi Hao, Kate E. DeMarsh, Xuan Zhang
The reactive chemistry of isoprene, the most emitted
biogenic hydrocarbon
worldwide, has a controlling influence on the composition and cleansing
capacity of the atmosphere. Although isoprene emission by plant biosynthesis
is negligible at night, heat-stressed vegetation in close proximity
to the fire front releases a substantial amount of isoprene, which
subsequently reacts with NO3 radicals, the major oxidant
in the dark. In this study, we performed chamber experiments to investigate
the efficacy of HOx recycling through
the nighttime chemistry of isoprene. By operating the experiments
at the continuous-flow steady-state mode, we created a chemical regime
that features sub-ppbv levels of NO, a regime that is highly relevant
to the nighttime atmosphere disturbed by fire plumes but was rarely
studied in previous chamber experiments. Using measurements of trace
levels of cyclohexane at steady state, we derived the total OH radicals
produced from isoprene + NO3 reactions in the range of
(4.4–8.0) × 105 molecules cm–3, accounting for 9.9–17.7% of the total reacted isoprene mass.
To explain this high level of observed OH, a simplified mechanism
that efficiently generates and converts HO2 to OH was proposed.
By incorporating this mechanism into an observationally constrained
box model, we predicted that the mixing ratio of OH radicals can exceed
∼105 molecules cm–3 when isoprene
and NO were present at parts per trillion by volume, a level frequently
encountered in environments impacted by biomass burning emissions.
Such an efficient production of OH radicals has an important impact
on the oxidizing power of the nocturnal atmosphere in regions with
intertwined biogenic and anthropogenic activities.