Abstract. The atmospheric chemistry of 2,2,5,5-tetramethyloxolane
(TMO), a promising “green” solvent replacement for toluene, was
investigated in laboratory-based experiments and computational calculations.
Results from both absolute and relative rate studies demonstrated that the
reaction OH + TMO (Reaction R1) proceeds with a rate coefficient k1(296 K) = (3.1±0.4) ×10-12 cm3 molecule−1 s−1, a
factor of 3 smaller than predicted by recent structure–activity
relationships. Quantum chemical calculations (CBS-QB3 and G4) demonstrated that
the reaction pathway via the lowest-energy transition state was
characterised by a hydrogen-bonded pre-reaction complex, leading to
thermodynamically less favoured products. Steric hindrance from the four
methyl substituents in TMO prevents formation of such H-bonded complexes on
the pathways to thermodynamically favoured products, a likely explanation
for the anomalous slow rate of Reaction (R1). Further evidence for a complex
mechanism was provided by k1(294–502 K), characterised by a local
minimum at around T=340 K. An estimated atmospheric lifetime of τ1≈3 d was calculated for TMO, approximately 50 %
longer than toluene, indicating that any air pollution impacts from TMO
emission would be less localised. An estimated photochemical ozone creation
potential (POCPE) of 18 was calculated for TMO in north-western Europe
conditions, less than half the equivalent value for toluene. Relative rate
experiments were used to determine a rate coefficient of k2(296 K) = (1.2±0.1) ×10-10 cm3 molecule−1 s−1
for Cl + TMO (Reaction R2); together with Reaction (R1), which is slow, this may indicate an
additional contribution to TMO removal in regions impacted by high levels of
atmospheric chlorine. All results from this work indicate that TMO is a less
problematic volatile organic compound (VOC) than toluene.