Role of Organic Carbon in Heterogeneous Reaction of N02 with Soot
Identifieur interne : 000188 ( Main/Exploration ); précédent : 000187; suivant : 000189Role of Organic Carbon in Heterogeneous Reaction of N02 with Soot
Auteurs : CHONG HAN [République populaire de Chine] ; YONGCHUN LIU [République populaire de Chine] ; HONG HE [République populaire de Chine]Source :
- Environmental science & technology [ 0013-936X ] ; 2013.
Descripteurs français
- Pascal (Inist)
English descriptors
- KwdEn :
Abstract
A large uncertainty among the reported uptake coefficients of NO2 on soot highlights the importance of the composition of soot in this reaction. Soot samples with different fractions of organic carbon (OC) were prepared by combusting n-hexane under controlled conditions. The heterogeneous reaction of NO2 on soot was investigated using a flow tube reactor at ambient pressure. The soot with the highest fuel/oxygen ratio showed the largest uptake coefficient (γinitial) of NO2 and yield of HONO (yHONO). Compared to fresh soot samples, preheated samples exhibited a great decrease in uptake coefficient of NO2 and HONO yield due to the removal of OC from soot. Ozonized soot also showed a lower reactivity toward NO2 than fresh soot, which can be ascribed to the consumption of OC with a reduced state (OCR). A linear dependence of the NO2 uptake coefficient and yields of HONO and NO on the OCR content of the soot was established, with γinitial(NO2) = (1.54 ± 1.39) X 10-6 + (1.96 ± 0.35) × 10-7 × OCR, yHONO = (11.6 ± 16.1) + (1.3 ± 0.40) × OCR, and yNO = (13.1 ± 1.9) - (0.2 ± 0.05) × OCR, respectively.
Affiliations:
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Le document en format XML
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<profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Air pollution</term>
<term>Air quality</term>
<term>Atmospheric chemistry</term>
<term>Carbonaceous materials</term>
<term>Chemical composition</term>
<term>Combustion residue</term>
<term>Heterogeneous reaction</term>
<term>Nitrogen compounds</term>
<term>Nitrogen dioxide</term>
<term>Photochemical oxidants</term>
<term>Property composition relationship</term>
<term>Soot</term>
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<keywords scheme="Pascal" xml:lang="fr"><term>Résidu combustion</term>
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<term>Suie</term>
<term>Pollution air</term>
<term>Composition chimique</term>
<term>Chimie atmosphérique</term>
<term>Réaction hétérogène</term>
<term>Dioxyde d'azote</term>
<term>Qualité air</term>
<term>Relation composition propriété</term>
<term>Oxydant photochimique</term>
<term>Composé de l'azote</term>
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<front><div type="abstract" xml:lang="en">A large uncertainty among the reported uptake coefficients of NO<sub>2</sub>
on soot highlights the importance of the composition of soot in this reaction. Soot samples with different fractions of organic carbon (OC) were prepared by combusting n-hexane under controlled conditions. The heterogeneous reaction of NO<sub>2</sub>
on soot was investigated using a flow tube reactor at ambient pressure. The soot with the highest fuel/oxygen ratio showed the largest uptake coefficient (γ<sub>initial</sub>
) of NO<sub>2</sub>
and yield of HONO (y<sub>HONO</sub>
). Compared to fresh soot samples, preheated samples exhibited a great decrease in uptake coefficient of NO<sub>2</sub>
and HONO yield due to the removal of OC from soot. Ozonized soot also showed a lower reactivity toward NO<sub>2</sub>
than fresh soot, which can be ascribed to the consumption of OC with a reduced state (OC<sub>R</sub>
). A linear dependence of the NO<sub>2</sub>
uptake coefficient and yields of HONO and NO on the OC<sub>R</sub>
content of the soot was established, with γ<sub>initial</sub>
(NO<sub>2</sub>
) = (1.54 ± 1.39) X 10<sup>-6</sup>
+ (1.96 ± 0.35) × 10<sup>-7</sup>
× OC<sub>R</sub>
, y<sub>HONO</sub>
= (11.6 ± 16.1) + (1.3 ± 0.40) × OC<sub>R</sub>
, and y<sub>NO</sub>
= (13.1 ± 1.9) - (0.2 ± 0.05) × OC<sub>R</sub>
, respectively.</div>
</front>
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<name sortKey="Yongchun Liu" sort="Yongchun Liu" uniqKey="Yongchun Liu" last="Yongchun Liu">YONGCHUN LIU</name>
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