Abstract. Lab-based experimental and computational methods were used to
study the atmospheric degradation of two promising “green” solvents:
pinacolone, (CH3)3CC(O)CH3, and methyl pivalate,
(CH3)3CC(O)OCH3. Pulsed laser photolysis coupled to pulsed
laser-induced fluorescence was used to determine absolute rate coefficients
(in 10−12 cm3 molec.−1 s−1) of k1(297 K) = (1.2 ± 0.2) for OH + (CH3)3CC(O)CH3 (Reaction R1) and
k2(297 K) = (1.3 ± 0.2) for OH + (CH3)3CC(O)OCH3 (Reaction R2), in good agreement with one
previous experimental study. Rate coefficients for both reactions were found
to increase at elevated temperature, with k1(T) adequately described by
k1(297–485 K) = 2.1 × 10−12 exp(-200/T) cm3 molec.−1 s−1. k2(T) exhibited more complex behaviour, with a
local minimum at around 300 K. In the course of this work, k3(295–450 K) was obtained for the well-characterised reaction OH + C2H5OH (ethanol;
Reaction R3), in satisfactory agreement with the evaluated
literature. UV–Vis spectroscopy experiments and computational calculations were used to
explore cross-sections for (CH3)3CC(O)CH3 photolysis
(Reaction R4), while (CH3)3CC(O)OCH3 showed no sign of
absorption over the wavelengths of interest. Absorption cross-sections for
(CH3)3CC(O)CH3, σ4(λ), in the actinic
region were larger, and the maximum was red-shifted compared to estimates
(methyl ethyl ketone (MEK) values) used in current state-of-science models. As a consequence, we
note that photolysis (Reaction R4) is likely the dominant pathway for removal of
(CH3)3CC(O)CH3 from the troposphere. Nonetheless, large
uncertainties remain as quantum yields φ4(λ) remain
unmeasured. Lifetime estimates based upon Reactions (R1) and (R4) span the
range 2–9 d and are consequently associated with a poorly constrained
estimated photochemical ozone creation potential (POCPE). In accord with
previous studies, (CH3)3CC(O)OCH3 did not absorb in
the actinic region, allowing for straightforward calculation of an
atmospheric lifetime of ≈ 9 d and a small POCPE ≈ 11.