The atmospheric oxidation of isoprene by OH radicals
under low
NO
x
conditions primarily leads to hydroxy
hydroperoxides (ISOPOOH), and further, to isoprene epoxy diols (IEPOX),
which have been identified as important SOA precursors. Recent studies
indicate that an additional class of highly oxidized ISOPOOH oxidation
products might contribute equally to SOA. Nonetheless, kinetic investigations
of the phase transfer of ISOPOOH and of its oxidation products are
largely missing, resulting in large uncertainties in understanding
the respective atmospheric chemistry and its implications. In the
present work, the partitioning behavior of synthetic 1,2-ISOPOOH and
its OH oxidation products was investigated in chamber experiments
with a (NO3
–)-CI-APi-ToFMS under low
NO
x
conditions for sulfate seed particles
under variation of relative humidity and particle acidity conditions.
For acidic sulfate particles, a reactive uptake coefficient of γ(1,2‑ISOPOOH)(pH=0) = (9 ± 4) × 10–3 was determined. For monomeric oxidation products, a parametrization
of measured uptake coefficients based on estimated vapor pressures
was obtained with γ(C5 product) =
−1.302 × 10–2 × ln(vap.press.·atm–1) – 0.1662, n = 15, R
2 = 0.727. Dimeric RO2 accretion
products were observed in the gas phase for the first time. In a model
study, an unexpectedly large proportion of these products was used
to constrain the rate constant of intramolecular hydrogen shift reactions
of C5O6H11 radicals to an upper limit
of k = 0.002 s–1. To evaluate the
atmospheric relevance, the results of this study were implemented
in a remote-case model study performed with F0AM, which resulted in
an increased SOA mass formation of 31% by way of the investigated
ISOPOOH oxidation and phase transfer pathways.