ATMOSPHERIC DEGRADATION OF BUTYL ACRYLATE
products formed from the OH-initiated degradation are mainly
carbonyl compounds, which are net sources of HOx (OH, HO2)
radicals that enhance photo-oxidation formation.
Table 2. Comparison of the rate constants of the reactions of
—
—
(CH )R and n-hexane with OH
—
different CH2 CHR, CH
—
2
3
radicals under atmospheric pressure and 298 K
kOH ꢂ 1011
Acknowledgements
VOC
(cm3 moleculeꢃ1 sꢃ1
)
The authors wish to acknowledge SECYT (Argentina), CONICET –
1.3a
1.7a
1.8b
4.2c
4.6c
7.1c
3.0d
3.0d
1.7d
0.7d
´
PIP 2004 (Argentina), ANPCyT (Prestamo BID 1728/OC-AR; PICT
25544, 2004; Prestamo BID 1201/OC-AR; PICT B No 25544);
—
CH2 CHC(O)OCH
—
—
3
CH2 CHC(O)OCH CH
´
—
2
3
—
CH2 CHC(O)O(CH ) CH
´
´
—
SECyT-UNC – Res. 19/06s (Cordoba, Argentina), Fundacion
Antorchas – Reentry Grant 2004 (Argentina), Third World Acad-
emy of Sciences (TWAS) 04-316 RG/CHE/LA (Italy), and The Royal
Society of Chemistry (RSC) RF 2007 (UK) for financial support of
this research.
2 3
3
—
CH2 C(CH )C(O)OCH
—
3
3
—
CH2 C(CH )C(O)OCH CH
3
—
3
2
—
CH2 C(CH )C(O)O(CH ) CH
3
—
3
2 3
—
CH2 CHCH
—
3
—
CH2 CHCH CH
—
2
3
—
CH2 CH(CH ) CH
—
2 3
3
CH3(CH2)4CH3
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c Reference.[7]
d Reference.[15]
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The atmospheric lifetime, tx, of the BUAC was calculated
through the expression: tx ¼ 1/kx[OH]. Unfortunately, no kinetic
data are available for the reactions of BUAC with other
tropospheric oxidants like O3 molecules NO3 radicals or Cl
atoms. A tropospheric lifetime of 8 h is calculated, assuming a
12 h average concentration of OH of 2 ꢂ 106 molecule cmꢃ3 [23]
.
This lifetime indicates that BUAC is likely to be rapidly removed in
the gas phase, the reaction with OH being the major loss process
for the unsaturated ester. Loss by photolysis can be considered
negligible since it is photolytically stable in the actinic region of
the electromagnetic spectrum.
The short lifetime of a few hours indicates that BUAC, like other
acrylates and methacrylates will be oxidized close to the emission
sources. Consequently, this emissions will have mainly a local
impact concerning the photochemical smog production. The
[23] R. Hein, P. J. Crutzen, M. Heimann, Global Biogeochem. Cycles 1997,
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J. Phys. Org. Chem. 2008, 21 397–401
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