Serveur d'exploration sur l'OCR

Attention, ce site est en cours de développement !
Attention, site généré par des moyens informatiques à partir de corpus bruts.
Les informations ne sont donc pas validées.

Role of Organic Carbon in Heterogeneous Reaction of N02 with Soot

Identifieur interne : 000188 ( Main/Exploration ); précédent : 000187; suivant : 000189

Role 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 :

RBID : Pascal:13-0320653

Descripteurs français

English descriptors

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:


Links toward previous steps (curation, corpus...)


Le document en format XML

<record>
<TEI>
<teiHeader>
<fileDesc>
<titleStmt>
<title xml:lang="en" level="a">Role of Organic Carbon in Heterogeneous Reaction of N0
<sub>2</sub>
with Soot</title>
<author>
<name sortKey="Chong Han" sort="Chong Han" uniqKey="Chong Han" last="Chong Han">CHONG HAN</name>
<affiliation wicri:level="1">
<inist:fA14 i1="01">
<s1>Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences</s1>
<s2>Beijing, 100085</s2>
<s3>CHN</s3>
<sZ>1 aut.</sZ>
<sZ>2 aut.</sZ>
<sZ>3 aut.</sZ>
</inist:fA14>
<country>République populaire de Chine</country>
<wicri:noRegion>Beijing, 100085</wicri:noRegion>
</affiliation>
</author>
<author>
<name sortKey="Yongchun Liu" sort="Yongchun Liu" uniqKey="Yongchun Liu" last="Yongchun Liu">YONGCHUN LIU</name>
<affiliation wicri:level="1">
<inist:fA14 i1="01">
<s1>Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences</s1>
<s2>Beijing, 100085</s2>
<s3>CHN</s3>
<sZ>1 aut.</sZ>
<sZ>2 aut.</sZ>
<sZ>3 aut.</sZ>
</inist:fA14>
<country>République populaire de Chine</country>
<wicri:noRegion>Beijing, 100085</wicri:noRegion>
</affiliation>
</author>
<author>
<name sortKey="Hong He" sort="Hong He" uniqKey="Hong He" last="Hong He">HONG HE</name>
<affiliation wicri:level="1">
<inist:fA14 i1="01">
<s1>Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences</s1>
<s2>Beijing, 100085</s2>
<s3>CHN</s3>
<sZ>1 aut.</sZ>
<sZ>2 aut.</sZ>
<sZ>3 aut.</sZ>
</inist:fA14>
<country>République populaire de Chine</country>
<wicri:noRegion>Beijing, 100085</wicri:noRegion>
</affiliation>
</author>
</titleStmt>
<publicationStmt>
<idno type="wicri:source">INIST</idno>
<idno type="inist">13-0320653</idno>
<date when="2013">2013</date>
<idno type="stanalyst">PASCAL 13-0320653 INIST</idno>
<idno type="RBID">Pascal:13-0320653</idno>
<idno type="wicri:Area/PascalFrancis/Corpus">000044</idno>
<idno type="wicri:Area/PascalFrancis/Curation">000724</idno>
<idno type="wicri:Area/PascalFrancis/Checkpoint">000031</idno>
<idno type="wicri:doubleKey">0013-936X:2013:Chong Han:role:of:organic</idno>
<idno type="wicri:Area/Main/Merge">000191</idno>
<idno type="wicri:Area/Main/Curation">000188</idno>
<idno type="wicri:Area/Main/Exploration">000188</idno>
</publicationStmt>
<sourceDesc>
<biblStruct>
<analytic>
<title xml:lang="en" level="a">Role of Organic Carbon in Heterogeneous Reaction of N0
<sub>2</sub>
with Soot</title>
<author>
<name sortKey="Chong Han" sort="Chong Han" uniqKey="Chong Han" last="Chong Han">CHONG HAN</name>
<affiliation wicri:level="1">
<inist:fA14 i1="01">
<s1>Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences</s1>
<s2>Beijing, 100085</s2>
<s3>CHN</s3>
<sZ>1 aut.</sZ>
<sZ>2 aut.</sZ>
<sZ>3 aut.</sZ>
</inist:fA14>
<country>République populaire de Chine</country>
<wicri:noRegion>Beijing, 100085</wicri:noRegion>
</affiliation>
</author>
<author>
<name sortKey="Yongchun Liu" sort="Yongchun Liu" uniqKey="Yongchun Liu" last="Yongchun Liu">YONGCHUN LIU</name>
<affiliation wicri:level="1">
<inist:fA14 i1="01">
<s1>Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences</s1>
<s2>Beijing, 100085</s2>
<s3>CHN</s3>
<sZ>1 aut.</sZ>
<sZ>2 aut.</sZ>
<sZ>3 aut.</sZ>
</inist:fA14>
<country>République populaire de Chine</country>
<wicri:noRegion>Beijing, 100085</wicri:noRegion>
</affiliation>
</author>
<author>
<name sortKey="Hong He" sort="Hong He" uniqKey="Hong He" last="Hong He">HONG HE</name>
<affiliation wicri:level="1">
<inist:fA14 i1="01">
<s1>Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences</s1>
<s2>Beijing, 100085</s2>
<s3>CHN</s3>
<sZ>1 aut.</sZ>
<sZ>2 aut.</sZ>
<sZ>3 aut.</sZ>
</inist:fA14>
<country>République populaire de Chine</country>
<wicri:noRegion>Beijing, 100085</wicri:noRegion>
</affiliation>
</author>
</analytic>
<series>
<title level="j" type="main">Environmental science & technology</title>
<title level="j" type="abbreviated">Environ. sci. technol.</title>
<idno type="ISSN">0013-936X</idno>
<imprint>
<date when="2013">2013</date>
</imprint>
</series>
</biblStruct>
</sourceDesc>
<seriesStmt>
<title level="j" type="main">Environmental science & technology</title>
<title level="j" type="abbreviated">Environ. sci. technol.</title>
<idno type="ISSN">0013-936X</idno>
</seriesStmt>
</fileDesc>
<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>
</keywords>
<keywords scheme="Pascal" xml:lang="fr">
<term>Résidu combustion</term>
<term>Matériau carboné</term>
<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>
</keywords>
</textClass>
</profileDesc>
</teiHeader>
<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>
</TEI>
<affiliations>
<list>
<country>
<li>République populaire de Chine</li>
</country>
</list>
<tree>
<country name="République populaire de Chine">
<noRegion>
<name sortKey="Chong Han" sort="Chong Han" uniqKey="Chong Han" last="Chong Han">CHONG HAN</name>
</noRegion>
<name sortKey="Hong He" sort="Hong He" uniqKey="Hong He" last="Hong He">HONG HE</name>
<name sortKey="Yongchun Liu" sort="Yongchun Liu" uniqKey="Yongchun Liu" last="Yongchun Liu">YONGCHUN LIU</name>
</country>
</tree>
</affiliations>
</record>

Pour manipuler ce document sous Unix (Dilib)

EXPLOR_STEP=$WICRI_ROOT/Ticri/CIDE/explor/OcrV1/Data/Main/Exploration
HfdSelect -h $EXPLOR_STEP/biblio.hfd -nk 000188 | SxmlIndent | more

Ou

HfdSelect -h $EXPLOR_AREA/Data/Main/Exploration/biblio.hfd -nk 000188 | SxmlIndent | more

Pour mettre un lien sur cette page dans le réseau Wicri

{{Explor lien
   |wiki=    Ticri/CIDE
   |area=    OcrV1
   |flux=    Main
   |étape=   Exploration
   |type=    RBID
   |clé=     Pascal:13-0320653
   |texte=   Role of Organic Carbon in Heterogeneous Reaction of N02 with Soot
}}

Wicri

This area was generated with Dilib version V0.6.32.
Data generation: Sat Nov 11 16:53:45 2017. Site generation: Mon Mar 11 23:15:16 2024