4.4 Article

Limonene: A scented and versatile tropospheric free radical deactivator

Journal

Publisher

WILEY
DOI: 10.1002/qua.27103

Keywords

activation energy; atmosphere; kinetics; product distribution; reaction mechanism; temperature dependence; troposphere

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In this study, the reactions between limonene and various free radicals were investigated using density functional theory. It was found that the relative reactivity of the studied radicals towards limonene follows the order: (SH)-S-center dot > (OBr)-O-center dot > (OCH3)-O-center dot > (OOH)-O-center dot > (OOCH3)-O-center dot.
The reactions of limonene with various free radicals ((center dot)OCH3 , (OBr)-O-center dot, (SH)-S-center dot, (OOH)-O-center dot, and (center dot)OOCH3) were investigated along the 273.15-312.15 K temperature range. To that purpose the density functional theory was used, at the M06-2X/6-311+g(d,p) level. Two reaction mechanisms, hydrogen atom transfer (HAT) and radical adduct formation (RAF) were considered. It was found that the relative reactivity of the studied radicals toward limonene is: (SH)-S-center dot > (OBr)-O-center dot > (OCH3)-O-center dot > (OOH)-O-center dot > (OOCH3)-O-center dot. HAT was identified as the dominant mechanism for 'OOH and 'OOCH3 , while RAF contributes the most to the reactions involving (center dot)OCH3 , (OBr)-O-center dot, and (SH)-S-center dot. The obtained Arrhenius expressions are: k((OCH3)-O-center dot) = 1.58 x 10(-13) e-1.59/RT , k((OBr)-O-center dot) = 3.55 x 10(-12) e(+1.82/RT) , k ((SH)-S-center dot) = 3.30 x 10(-11) e(+0.79/RT) , k((OOH)-O-center dot) = 1.33 x 10(-15) e(-5.99/RT) , and k ((OOCH3)-O-center dot) = 5.88 x 10(-17) e(-6.26/RT). According to them, the reactions of (OBr)-O-center dot and (SH)-S-center dot become slower as temperature rises from 273.15 to 312.15 K, while for the other radicals the reactions rate increases with temperature. The subsequent tropospheric fate of the most abundant (OBr)-O-center dot adduct was also investigated in the same temperature range, considering O-2 addition to this radical (step 2) and the reaction of the peroxyl radical yielded in this step 2 with NO. The latter is predicted to take place in two steps: the NO addition (3a) and the NO2 elimination (3b). The corresponding Arrhenius expression are k(2) = 3.56 x 10(-15) e(+1.43/RT) and k(3b) = 1.35 x 10(14) e(-31.65/RT). Step 3a was found to be barrierless. To our best knowledge, all the data provided here is reported for the first time. Thus, it would hopefully contribute to enhance the knowledge necessary for the full understanding (and accurate modeling) of the troposphere.

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