The
gas-phase reaction between
trans
-2-hexenal
(T2H) and chlorine atoms (Cl) was studied using three complementary
experimental setups at atmospheric pressure and room temperature.
In this work, we studied the rate constant for the titled oxidation
reaction as well as the formation of the gas-phase products and secondary
organic aerosols (SOAs). The rate constant of the T2H + Cl reaction
was determined using the relative method in a simulation chamber using
proton-transfer reaction time-of-flight mass spectrometry (PTR-ToF-MS)
to monitor the loss of T2H and the reference compound. An average
reaction rate constant of (3.17 ± 0.72) × 10
–10
cm
3
molecule
–1
s
–1
was obtained. From this, the atmospheric lifetime of T2H due to
Cl reaction was estimated to be 9 h for coastal regions. HCl, CO,
and butanal were identified as primary products using Fourier transform
infrared spectroscopy (FTIR). The molar yield of butanal was (6.4
± 0.3)%. Formic acid was identified as a secondary product by
FTIR. In addition, butanal, 2-chlorohexenal, and 2-hexenoic acid were
identified as products by gas chromatography coupled to mass spectrometry
but not quantified. A reaction mechanism is proposed based on the
observed products. SOA formation was observed by using a fast mobility
particle sizer spectrometer. The measured SOA yields reached maximum
values of about 38% at high particle mass concentrations. This work
exhibits for the first time that T2H can be a source of SOA in coastal
atmospheres, where Cl concentrations can be high at dawn, or in industrial
areas, such as ceramic industries, where Cl precursors may be present.