1,2-Dihydroxy
isoprene (1,2-DHI), a product of isoprene oxidation
from multiple chemical pathways, is produced in the atmosphere in
large quantities; however, its chemical fate has not been comprehensively
studied. Here, we perform chamber experiments to investigate its gas-phase
reactions. We find that the reactions of 1,2-DHI with OH radicals
and ozone are rapid (k
OH = 8.0 (±1.3)
× 10–11 cm3 molecule–1 s–1; k
O3 = 7.2 (±1.1)
× 10–18 cm3 molecule–1 s–1). Reaction with OH, which dominates 1,2-DHI
loss, leads primarily to fragmentation and radical recycling; major
products under both high- and low-NO conditions include hydroxyacetone,
glycolaldehyde, and 2,3-dihydroxy-2-methyl-propanal (DHMP). Radical-terminating
hydroperoxide formation from the peroxy radical (RO2) reaction
with HO2 and organonitrate formation from RO2 + NO are not observed in the gas phase, possibly due to low volatility;
constraints for their branching ratios are instead derived by mass
balance. We also measure secondary organic aerosol mass yields from
1,2-DHI (0–23%) and show that oxidation in the presence of
aqueous particles leads to formic and acetic acid production. Finally,
we incorporate results into GEOS-Chem, a global chemical transport
model, to compute the global production (25.3 Tg a–1) and gas-phase loss (20.2 Tg a–1) of 1,2-DHI and
show that its oxidation provides non-negligible contributions to the
atmospheric budgets of hydroxyacetone, glycolaldehyde, hydroxymethyl
hydroperoxide, formic acid, and DHMP.