The kinetics of the reactions of chlorine atoms with acrylates have been studied by the
relative kinetic method. While there are a few studies in the literature of OH radical
reactions with unsaturated esters there are almost no data concerning their Cl-initiated
degradation. In this work, we report rate coefficients and preliminary product results for the
reactions of Cl with CH2=CHC(O)OCH3 (k1), CH2=C(CH3)C(O)OCH3 (k2) and
CH2=C(CH3)C(O)O(CH2)3CH3 (k3).
The experiments were performed over the temperature range 283-313K at atmospheric pressure in a large volume photoreactor using in situ FTIR analysis to monitor the decay of the organics and the reference compounds. The following Arrhenius expressions (in units of cm3 molecule-1 s-1) have been obtained: k1 The experiments were performed over the temperature range 283-313K at atmospheric pressure in a large volume photoreactor using in situ FTIR analysis to monitor the decay of the organics and the reference compounds. The following Arrhenius expressions (in units of cm3 molecule-1 s-1) have been obtained: k1
CH2=C(CH3)C(O)O(CH2)3CH3 (k3).
The experiments were performed over the temperature range 283-313K at atmospheric pressure in a large volume photoreactor using in situ FTIR analysis to monitor the decay of the organics and the reference compounds. The following Arrhenius expressions (in units of cm3 molecule-1 s-1) have been obtained: k1
The experiments were performed over the temperature range 283-313K at atmospheric
pressure in a large volume photoreactor using in situ FTIR analysis to monitor the decay of
the organics and the reference compounds.
The following Arrhenius expressions (in units of cm3 molecule-1 s-1) have been obtained: k1
2=CHC(O)OCH3 (k1), CH2=C(CH3)C(O)OCH3 (k2) andCH2=C(CH3)C(O)O(CH2)3CH3 (k3).
The experiments were performed over the temperature range 283-313K at atmospheric pressure in a large volume photoreactor using in situ FTIR analysis to monitor the decay of the organics and the reference compounds. The following Arrhenius expressions (in units of cm3 molecule-1 s-1) have been obtained: k1
The experiments were performed over the temperature range 283-313K at atmospheric
pressure in a large volume photoreactor using in situ FTIR analysis to monitor the decay of
the organics and the reference compounds.
The following Arrhenius expressions (in units of cm3 molecule-1 s-1) have been obtained: k1
2=C(CH3)C(O)O(CH2)3CH3 (k3).The experiments were performed over the temperature range 283-313K at atmospheric
pressure in a large volume photoreactor using in situ FTIR analysis to monitor the decay of
the organics and the reference compounds.
The following Arrhenius expressions (in units of cm3 molecule-1 s-1) have been obtained: k1
3 molecule-1 s-1) have been obtained: k1= (0.59 ± 0.11) × 10-11 exp[(1.097 ± 0.098) × 103 / RT], k2 = (3.77 ± 1.12) × 10-11 exp[-
(16.68 ± 1.54) × 103 / RT], k3 = (1.34 ± 1.04) × 10-11 exp[-(19.59 ± 3.21) × 103 / RT]. The
negative temperature dependencies of the three reactions supports that addition of Cl to the double bond is the main reaction pathway for each reaction. This is further supported by the currently ongoing product analyses. The observed products are in line with the preferential addition of Cl to the less substituted carbon atom of the double bond followed by decomposition of the 1,2-hydroxyalcoxy radicals formed. Reaction mechanisms will be presented for the Cl initiated oxidation which can be used to construct mechanisms for the analogue more atmospherically important OH radical reactions. negative temperature dependencies of the three reactions supports that addition of Cl to the double bond is the main reaction pathway for each reaction. This is further supported by the currently ongoing product analyses. The observed products are in line with the preferential addition of Cl to the less substituted carbon atom of the double bond followed by decomposition of the 1,2-hydroxyalcoxy radicals formed. Reaction mechanisms will be presented for the Cl initiated oxidation which can be used to construct mechanisms for the analogue more atmospherically important OH radical reactions.
(16.68 ± 1.54) × 103 / RT], k3 = (1.34 ± 1.04) × 10-11 exp[-(19.59 ± 3.21) × 103 / RT]. The
negative temperature dependencies of the three reactions supports that addition of Cl to the double bond is the main reaction pathway for each reaction. This is further supported by the currently ongoing product analyses. The observed products are in line with the preferential addition of Cl to the less substituted carbon atom of the double bond followed by decomposition of the 1,2-hydroxyalcoxy radicals formed. Reaction mechanisms will be presented for the Cl initiated oxidation which can be used to construct mechanisms for the analogue more atmospherically important OH radical reactions.
negative temperature dependencies of the three reactions supports that addition of Cl to the
double bond is the main reaction pathway for each reaction.
This is further supported by the currently ongoing product analyses. The observed products
are in line with the preferential addition of Cl to the less substituted carbon atom of the
double bond followed by decomposition of the 1,2-hydroxyalcoxy radicals formed.
Reaction mechanisms will be presented for the Cl initiated oxidation which can be used to
construct mechanisms for the analogue more atmospherically important OH radical
reactions.
-11 exp[(1.097 ± 0.098) × 103 / RT], k2 = (3.77 ± 1.12) × 10-11 exp[-(16.68 ± 1.54) × 103 / RT], k3 = (1.34 ± 1.04) × 10-11 exp[-(19.59 ± 3.21) × 103 / RT]. The
negative temperature dependencies of the three reactions supports that addition of Cl to the double bond is the main reaction pathway for each reaction. This is further supported by the currently ongoing product analyses. The observed products are in line with the preferential addition of Cl to the less substituted carbon atom of the double bond followed by decomposition of the 1,2-hydroxyalcoxy radicals formed. Reaction mechanisms will be presented for the Cl initiated oxidation which can be used to construct mechanisms for the analogue more atmospherically important OH radical reactions.
negative temperature dependencies of the three reactions supports that addition of Cl to the
double bond is the main reaction pathway for each reaction.
This is further supported by the currently ongoing product analyses. The observed products
are in line with the preferential addition of Cl to the less substituted carbon atom of the
double bond followed by decomposition of the 1,2-hydroxyalcoxy radicals formed.
Reaction mechanisms will be presented for the Cl initiated oxidation which can be used to
construct mechanisms for the analogue more atmospherically important OH radical
reactions.
3 / RT], k3 = (1.34 ± 1.04) × 10-11 exp[-(19.59 ± 3.21) × 103 / RT]. Thenegative temperature dependencies of the three reactions supports that addition of Cl to the
double bond is the main reaction pathway for each reaction.
This is further supported by the currently ongoing product analyses. The observed products
are in line with the preferential addition of Cl to the less substituted carbon atom of the
double bond followed by decomposition of the 1,2-hydroxyalcoxy radicals formed.
Reaction mechanisms will be presented for the Cl initiated oxidation which can be used to
construct mechanisms for the analogue more atmospherically important OH radical
reactions.