2014
DOI: 10.1016/j.cplett.2014.04.020
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Reactions of OH and Cl with isopropyl formate, isobutyl formate, n-propyl isobutyrate and isopropyl isobutyrate

Abstract: a b s t r a c tThe rate coefficients for the reactions of OH with isopropyl formate, isobutyl formate, n-propyl isobutyrate and isopropyl isobutyrate have been determined using both absolute and relative methods. The relative rate method has been also used to measure the room temperature rate coefficient for the reaction of Cl with the same esters. In addition, a series of runs conducted on the OH-initiated oxidation of isopropyl formate, isobutyl formate and n-propyl isobutyrate showed the formation of aceton… Show more

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Cited by 3 publications
(14 citation statements)
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References 15 publications
(21 reference statements)
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“…In the case of reaction R1 , the experimentally measured and computationally calculated rate coefficients at 298 K are k R1–298K Exp = (1.56 ± 0.57) × 10 –11 cm 3 molecule –1 s –1 and k R1–298K Theory = 1.87× 10 –11 cm 3 molecule –1 s –1 respectively which are in excellent agreement with each other within the experimental uncertainties. Both experimentally measured and computationally calculated rate coefficients are in good agreement with previously reported rate coefficients by Pimentel et al [(1.75 ± 0.35) × 10 –11 cm 3 molecule –1 s –1 ] and Zhang et al [(1.40 ± 0.20) × 10 –11 cm 3 molecule –1 s –1 ] within the reported experimental uncertainties (maximum deviation between experimentally measured and reported rate coefficients by Pimentel et al and Zhang et al are found out to be 12% and 11% respectively). Both experimentally measured and computationally calculated temperature dependent rate coefficients have shown a negative temperature dependence due to the formation of stabilized prereactive complexes.…”
Section: Results and Discussionsupporting
confidence: 90%
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“…In the case of reaction R1 , the experimentally measured and computationally calculated rate coefficients at 298 K are k R1–298K Exp = (1.56 ± 0.57) × 10 –11 cm 3 molecule –1 s –1 and k R1–298K Theory = 1.87× 10 –11 cm 3 molecule –1 s –1 respectively which are in excellent agreement with each other within the experimental uncertainties. Both experimentally measured and computationally calculated rate coefficients are in good agreement with previously reported rate coefficients by Pimentel et al [(1.75 ± 0.35) × 10 –11 cm 3 molecule –1 s –1 ] and Zhang et al [(1.40 ± 0.20) × 10 –11 cm 3 molecule –1 s –1 ] within the reported experimental uncertainties (maximum deviation between experimentally measured and reported rate coefficients by Pimentel et al and Zhang et al are found out to be 12% and 11% respectively). Both experimentally measured and computationally calculated temperature dependent rate coefficients have shown a negative temperature dependence due to the formation of stabilized prereactive complexes.…”
Section: Results and Discussionsupporting
confidence: 90%
“…The typical concentration of Cl atoms in the marine boundary layer (MBL) and in ambient conditions used for the calculation of cumulative lifetime of the test molecules are 1.3 × 10 5 and 1.0 × 10 3 atom cm –3 . , The typical OH radical concentration used in the calculation is 1.0 × 10 6 radical cm –3 . The rate coefficients for the reactions of IPF and IBF with OH radicals at 298 K are (1.87 ± 0.11) × 10 –12 and (3.17 ± 0.20) × 10 –12 cm 3 molecule –1 s –1 respectively . The rate coefficients for the reactions of IPF and IBF with Cl atoms at 298 K and at 1 atm pressure are (1.56 ± 0.47) × 10 –11 and (7.23 ± 1.80) × 10 –12 cm 3 molecule –1 s –1 respectively.…”
Section: Atmospheric Implicationmentioning
confidence: 96%
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