An investigation into the reactions between Cl atoms and acrolein (1), meth
acrolein (2) and methyl vinyl ketone (3)
CH2CHCHO+Cl --> products (1)
CH2C(CH3)CHO + Cl --> products (2)
CH2CHC(O)CH3 + Cl --> products (3)
is presented. Values of the rate constants for the reactions have been dete
rmined by an absolute technique for the first time. At a pressure of 1.6 To
rr, the rate constants obtained were: and k(1) = 1.1 +/- 0.2, k(2) = 3.3 +/
- 0.6 k(3) = 0.99 +/- 0.20 in units of 10(-10) cm(3) molecule(-1) s(-1). k(
1) was also determined at atmospheric pressure using a relative-rate techni
que. The rate constant obtained was (2.2 +/- 0.3) x 10(-10) cm(3) molecule(
-1) s(-1); the larger value compared with that for 1.6 Torr is thought to r
eflect a true dependence of the reaction rate on pressure. The final produc
ts of the reactions performed under an atmosphere of synthetic air were inv
estigated using FTIR spectroscopy. The only chlorinated organic species ide
ntified as products of the reactions were chloroacetaldehyde in the case of
reaction of Cl atoms with acrolein; chloroacetone with methacrolein; and c
hloroacetaldehyde with methyl vinyl ketone. Branching ratios for abstractio
n (the fraction of reactions occurring by abstraction relative to the sum o
f addition and abstraction processes) were found to be 0.22 +/- 0.13 for ac
rolein, 0.18 +/- 0.02 for methacrolein and <0.03 for methyl vinyl ketone. T
he reaction of Cl atoms with methacrolein proceeds via a mechanism that inv
olves the decomposition of the methyl vinyl radical. The decomposition of t
his radical in synthetic air, and in the absence of NO, appears to lead to
the formation of significantly more CO than previously thought. This observ
ation is in agreement with the work of J. J. Orlando, S. E. Paulson and G.
S. Tyndall, Geophys. Res. Lett., 1999, 26, 2191 (ref. 1), who studied the d
ecomposition of the radical under different conditions.