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.

The kinetics of the reaction of OH With COS

Identifieur interne : 001538 ( Istex/Corpus ); précédent : 001537; suivant : 001539

The kinetics of the reaction of OH With COS

Auteurs : Andreas Wahner ; A. R. Ravishankara

Source :

RBID : ISTEX:52174110CB10DF095DF5BB8309038A0A07ACFF89

Abstract

The laser/flash‐photolysis laser‐induced fluorescence technique was employed to study the reaction of OH with carbonyl sulfide (COS) in various buffer gases (He, N2, and SF6). In order to determine the relevance of this reaction to tropospheric chemistry the influence of O2 on the rate constant was investigated. To avoid secondary reactions, especially the photolysis of COS, different photolytic OH precursors (H2O2, HNO3, and HONO) with different photolysis light sources (Xe flash lamp, ArF laser, fourth‐harmonic Nd: YAG laser, XeF laser, and third‐harmonic Nd: YAG laser) were used. The rate constant (1.92±0.25)×10−15 cm3 s−1 for the reaction of OH with COS at room temperature was found (after correcting for H2S impurity) to be independent of the pressure and the buffer gas. Addition of O2 was found to have no influence on the measured rate constant. Certain experiments were carried out at 298 K and 245 K to ascertain the mechanism for this reaction. Our results suggest that the degradation pathway involving homogeneous gas phase reaction of COS with OH is of minor importance in the troposphere.

Url:
DOI: 10.1029/JD092iD02p02189

Links to Exploration step

ISTEX:52174110CB10DF095DF5BB8309038A0A07ACFF89

Le document en format XML

<record>
<TEI wicri:istexFullTextTei="biblStruct">
<teiHeader>
<fileDesc>
<titleStmt>
<title xml:lang="en">The kinetics of the reaction of OH With COS</title>
<author wicri:is="90%">
<name sortKey="Wahner, Andreas" sort="Wahner, Andreas" uniqKey="Wahner A" first="Andreas" last="Wahner">Andreas Wahner</name>
</author>
<author wicri:is="90%">
<name sortKey="Ravishankara, A R" sort="Ravishankara, A R" uniqKey="Ravishankara A" first="A. R." last="Ravishankara">A. R. Ravishankara</name>
</author>
</titleStmt>
<publicationStmt>
<idno type="wicri:source">ISTEX</idno>
<idno type="RBID">ISTEX:52174110CB10DF095DF5BB8309038A0A07ACFF89</idno>
<date when="1987" year="1987">1987</date>
<idno type="doi">10.1029/JD092iD02p02189</idno>
<idno type="url">https://api.istex.fr/document/52174110CB10DF095DF5BB8309038A0A07ACFF89/fulltext/pdf</idno>
<idno type="wicri:Area/Istex/Corpus">001538</idno>
</publicationStmt>
<sourceDesc>
<biblStruct>
<analytic>
<title level="a" type="main" xml:lang="en">The kinetics of the reaction of OH With COS</title>
<author wicri:is="90%">
<name sortKey="Wahner, Andreas" sort="Wahner, Andreas" uniqKey="Wahner A" first="Andreas" last="Wahner">Andreas Wahner</name>
</author>
<author wicri:is="90%">
<name sortKey="Ravishankara, A R" sort="Ravishankara, A R" uniqKey="Ravishankara A" first="A. R." last="Ravishankara">A. R. Ravishankara</name>
</author>
</analytic>
<monogr></monogr>
<series>
<title level="j">Journal of Geophysical Research: Atmospheres</title>
<title level="j" type="abbrev">J. Geophys. Res.</title>
<idno type="ISSN">0148-0227</idno>
<idno type="eISSN">2156-2202</idno>
<imprint>
<publisher>Blackwell Publishing Ltd</publisher>
<date type="published" when="1987-02-20">1987-02-20</date>
<biblScope unit="volume">92</biblScope>
<biblScope unit="issue">D2</biblScope>
<biblScope unit="page" from="2189">2189</biblScope>
<biblScope unit="page" to="2194">2194</biblScope>
</imprint>
<idno type="ISSN">0148-0227</idno>
</series>
<idno type="istex">52174110CB10DF095DF5BB8309038A0A07ACFF89</idno>
<idno type="DOI">10.1029/JD092iD02p02189</idno>
<idno type="ArticleID">6D0632</idno>
</biblStruct>
</sourceDesc>
<seriesStmt>
<idno type="ISSN">0148-0227</idno>
</seriesStmt>
</fileDesc>
<profileDesc>
<textClass></textClass>
<langUsage>
<language ident="en">en</language>
</langUsage>
</profileDesc>
</teiHeader>
<front>
<div type="abstract">The laser/flash‐photolysis laser‐induced fluorescence technique was employed to study the reaction of OH with carbonyl sulfide (COS) in various buffer gases (He, N2, and SF6). In order to determine the relevance of this reaction to tropospheric chemistry the influence of O2 on the rate constant was investigated. To avoid secondary reactions, especially the photolysis of COS, different photolytic OH precursors (H2O2, HNO3, and HONO) with different photolysis light sources (Xe flash lamp, ArF laser, fourth‐harmonic Nd: YAG laser, XeF laser, and third‐harmonic Nd: YAG laser) were used. The rate constant (1.92±0.25)×10−15 cm3 s−1 for the reaction of OH with COS at room temperature was found (after correcting for H2S impurity) to be independent of the pressure and the buffer gas. Addition of O2 was found to have no influence on the measured rate constant. Certain experiments were carried out at 298 K and 245 K to ascertain the mechanism for this reaction. Our results suggest that the degradation pathway involving homogeneous gas phase reaction of COS with OH is of minor importance in the troposphere.</div>
</front>
</TEI>
<istex>
<corpusName>wiley</corpusName>
<author>
<json:item>
<name>Andreas Wahner</name>
</json:item>
<json:item>
<name>A. R. Ravishankara</name>
</json:item>
</author>
<articleId>
<json:string>6D0632</json:string>
</articleId>
<language>
<json:string>eng</json:string>
</language>
<abstract>The laser/flash‐photolysis laser‐induced fluorescence technique was employed to study the reaction of OH with carbonyl sulfide (COS) in various buffer gases (He, N2, and SF6). In order to determine the relevance of this reaction to tropospheric chemistry the influence of O2 on the rate constant was investigated. To avoid secondary reactions, especially the photolysis of COS, different photolytic OH precursors (H2O2, HNO3, and HONO) with different photolysis light sources (Xe flash lamp, ArF laser, fourth‐harmonic Nd: YAG laser, XeF laser, and third‐harmonic Nd: YAG laser) were used. The rate constant (1.92±0.25)×10−15 cm3 s−1 for the reaction of OH with COS at room temperature was found (after correcting for H2S impurity) to be independent of the pressure and the buffer gas. Addition of O2 was found to have no influence on the measured rate constant. Certain experiments were carried out at 298 K and 245 K to ascertain the mechanism for this reaction. Our results suggest that the degradation pathway involving homogeneous gas phase reaction of COS with OH is of minor importance in the troposphere.</abstract>
<qualityIndicators>
<score>6.606</score>
<pdfVersion>1.2</pdfVersion>
<pdfPageSize>597 x 811 pts</pdfPageSize>
<refBibsNative>true</refBibsNative>
<keywordCount>0</keywordCount>
<abstractCharCount>1112</abstractCharCount>
<pdfWordCount>4506</pdfWordCount>
<pdfCharCount>27033</pdfCharCount>
<pdfPageCount>6</pdfPageCount>
<abstractWordCount>175</abstractWordCount>
</qualityIndicators>
<title>The kinetics of the reaction of OH With COS</title>
<genre.original>
<json:string>article</json:string>
</genre.original>
<genre>
<json:string>article</json:string>
</genre>
<host>
<volume>92</volume>
<publisherId>
<json:string>JGRD</json:string>
</publisherId>
<pages>
<total>6</total>
<last>2194</last>
<first>2189</first>
</pages>
<issn>
<json:string>0148-0227</json:string>
</issn>
<issue>D2</issue>
<subject>
<json:item>
<value>ATMOSPHERIC COMPOSITION AND STRUCTURE</value>
</json:item>
<json:item>
<value>Troposphere: composition and chemistry</value>
</json:item>
<json:item>
<value>Regular Issue</value>
</json:item>
</subject>
<genre>
<json:string>journal</json:string>
</genre>
<language>
<json:string>unknown</json:string>
</language>
<eissn>
<json:string>2156-2202</json:string>
</eissn>
<title>Journal of Geophysical Research: Atmospheres</title>
<doi>
<json:string>10.1002/(ISSN)2156-2202d</json:string>
</doi>
</host>
<publicationDate>1987</publicationDate>
<copyrightDate>1987</copyrightDate>
<doi>
<json:string>10.1029/JD092iD02p02189</json:string>
</doi>
<id>52174110CB10DF095DF5BB8309038A0A07ACFF89</id>
<fulltext>
<json:item>
<original>true</original>
<mimetype>application/pdf</mimetype>
<extension>pdf</extension>
<uri>https://api.istex.fr/document/52174110CB10DF095DF5BB8309038A0A07ACFF89/fulltext/pdf</uri>
</json:item>
<json:item>
<original>false</original>
<mimetype>application/zip</mimetype>
<extension>zip</extension>
<uri>https://api.istex.fr/document/52174110CB10DF095DF5BB8309038A0A07ACFF89/fulltext/zip</uri>
</json:item>
<istex:fulltextTEI uri="https://api.istex.fr/document/52174110CB10DF095DF5BB8309038A0A07ACFF89/fulltext/tei">
<teiHeader>
<fileDesc>
<titleStmt>
<title level="a" type="main" xml:lang="en">The kinetics of the reaction of OH With COS</title>
</titleStmt>
<publicationStmt>
<authority>ISTEX</authority>
<publisher>Blackwell Publishing Ltd</publisher>
<availability>
<p>WILEY</p>
</availability>
<date>1987</date>
</publicationStmt>
<sourceDesc>
<biblStruct type="inbook">
<analytic>
<title level="a" type="main" xml:lang="en">The kinetics of the reaction of OH With COS</title>
<author>
<persName>
<forename type="first">Andreas</forename>
<surname>Wahner</surname>
</persName>
</author>
<author>
<persName>
<forename type="first">A. R.</forename>
<surname>Ravishankara</surname>
</persName>
</author>
</analytic>
<monogr>
<title level="j">Journal of Geophysical Research: Atmospheres</title>
<title level="j" type="abbrev">J. Geophys. Res.</title>
<idno type="pISSN">0148-0227</idno>
<idno type="eISSN">2156-2202</idno>
<idno type="DOI">10.1002/(ISSN)2156-2202d</idno>
<imprint>
<publisher>Blackwell Publishing Ltd</publisher>
<date type="published" when="1987-02-20"></date>
<biblScope unit="volume">92</biblScope>
<biblScope unit="issue">D2</biblScope>
<biblScope unit="page" from="2189">2189</biblScope>
<biblScope unit="page" to="2194">2194</biblScope>
</imprint>
</monogr>
<idno type="istex">52174110CB10DF095DF5BB8309038A0A07ACFF89</idno>
<idno type="DOI">10.1029/JD092iD02p02189</idno>
<idno type="ArticleID">6D0632</idno>
</biblStruct>
</sourceDesc>
</fileDesc>
<profileDesc>
<creation>
<date>1987</date>
</creation>
<langUsage>
<language ident="en">en</language>
</langUsage>
<abstract>
<p>The laser/flash‐photolysis laser‐induced fluorescence technique was employed to study the reaction of OH with carbonyl sulfide (COS) in various buffer gases (He, N2, and SF6). In order to determine the relevance of this reaction to tropospheric chemistry the influence of O2 on the rate constant was investigated. To avoid secondary reactions, especially the photolysis of COS, different photolytic OH precursors (H2O2, HNO3, and HONO) with different photolysis light sources (Xe flash lamp, ArF laser, fourth‐harmonic Nd: YAG laser, XeF laser, and third‐harmonic Nd: YAG laser) were used. The rate constant (1.92±0.25)×10−15 cm3 s−1 for the reaction of OH with COS at room temperature was found (after correcting for H2S impurity) to be independent of the pressure and the buffer gas. Addition of O2 was found to have no influence on the measured rate constant. Certain experiments were carried out at 298 K and 245 K to ascertain the mechanism for this reaction. Our results suggest that the degradation pathway involving homogeneous gas phase reaction of COS with OH is of minor importance in the troposphere.</p>
</abstract>
<textClass>
<keywords scheme="Journal Subject">
<list>
<head>index-terms</head>
<item>
<term>ATMOSPHERIC COMPOSITION AND STRUCTURE</term>
</item>
<item>
<term>Troposphere: composition and chemistry</term>
</item>
</list>
</keywords>
</textClass>
<textClass>
<keywords scheme="Journal Subject">
<list>
<head>article-category</head>
<item>
<term>Regular Issue</term>
</item>
</list>
</keywords>
</textClass>
</profileDesc>
<revisionDesc>
<change when="1986-08-01">Received</change>
<change when="1986-10-24">Registration</change>
<change when="1987-02-20">Published</change>
</revisionDesc>
</teiHeader>
</istex:fulltextTEI>
<json:item>
<original>false</original>
<mimetype>text/plain</mimetype>
<extension>txt</extension>
<uri>https://api.istex.fr/document/52174110CB10DF095DF5BB8309038A0A07ACFF89/fulltext/txt</uri>
</json:item>
</fulltext>
<metadata>
<istex:metadataXml wicri:clean="Wiley, elements deleted: body">
<istex:xmlDeclaration>version="1.0" encoding="UTF-8" standalone="yes"</istex:xmlDeclaration>
<istex:document>
<component type="serialArticle" version="2.0" xml:lang="en" xml:id="jgrd669">
<header>
<publicationMeta level="product">
<doi>10.1002/(ISSN)2156-2202d</doi>
<issn type="print">0148-0227</issn>
<issn type="electronic">2156-2202</issn>
<idGroup>
<id type="product" value="JGRD"></id>
<id type="coden" value="JGREA2"></id>
</idGroup>
<titleGroup>
<title type="main" xml:lang="en" sort="JOURNAL OF GEOPHYSICAL RESEARCH: ATMOSPHERES">Journal of Geophysical Research: Atmospheres</title>
<title type="short">J. Geophys. Res.</title>
</titleGroup>
</publicationMeta>
<publicationMeta level="part" position="20">
<doi>10.1002/jgrd.v92.D2</doi>
<idGroup>
<id type="focusSection" value="4"></id>
</idGroup>
<titleGroup>
<title type="focusSection" xml:lang="en">Journal of Geophysical Research: Atmospheres</title>
</titleGroup>
<numberingGroup>
<numbering type="journalVolume" number="92">92</numbering>
<numbering type="journalIssue">D2</numbering>
</numberingGroup>
<coverDate startDate="1987-02-20">20 February 1987</coverDate>
</publicationMeta>
<publicationMeta level="unit" type="article" position="210" status="forIssue">
<doi>10.1029/JD092iD02p02189</doi>
<idGroup>
<id type="editorialOffice" value="6D0632"></id>
<id type="unit" value="JGRD669"></id>
</idGroup>
<countGroup>
<count type="pageTotal" number="6"></count>
</countGroup>
<titleGroup>
<title type="articleCategory">Regular Issue</title>
<title type="tocHeading1">Regular Issue</title>
</titleGroup>
<copyright ownership="thirdParty">Copyright 1987 by the American Geophysical Union.</copyright>
<eventGroup>
<event type="manuscriptReceived" date="1986-08-01"></event>
<event type="manuscriptAccepted" date="1986-10-24"></event>
<event type="publishedPrint" date="1987-02-20"></event>
<event type="firstOnline" date="2012-09-21"></event>
<event type="publishedOnlineFinalForm" date="2012-09-21"></event>
<event type="xmlConverted" agent="SPi Global Converter:AGUv1.0_TO_WileyML3Gv1.0.3 version:1.2; WileyML 3G Packaging Tool v1.0" date="2012-12-01"></event>
<event type="xmlConverted" agent="Converter:WILEY_ML3G_TO_WILEY_ML3GV2 version:3.8.8" date="2014-01-30"></event>
<event type="xmlConverted" agent="Converter:WML3G_To_WML3G version:4.1.7 mode:FullText,remove_FC" date="2014-10-30"></event>
</eventGroup>
<numberingGroup>
<numbering type="pageFirst">2189</numbering>
<numbering type="pageLast">2194</numbering>
</numberingGroup>
<subjectInfo>
<subject href="http://psi.agu.org/taxonomy5/0300">ATMOSPHERIC COMPOSITION AND STRUCTURE</subject>
<subjectInfo>
<subject href="http://psi.agu.org/taxonomy5/0365">Troposphere: composition and chemistry</subject>
</subjectInfo>
</subjectInfo>
<selfCitationGroup>
<citation xml:id="jgrd669-cit-0000" type="self">
<author>
<familyName>Wahner</familyName>
,
<givenNames>A.</givenNames>
</author>
, and
<author>
<givenNames>A. R.</givenNames>
<familyName>Ravishankara</familyName>
</author>
(
<pubYear year="1987">1987</pubYear>
),
<articleTitle>The kinetics of the reaction of OH With COS</articleTitle>
,
<journalTitle>J. Geophys. Res.</journalTitle>
,
<vol>92</vol>
(
<issue>D2</issue>
),
<pageFirst>2189</pageFirst>
<pageLast>2194</pageLast>
, doi:
<accessionId ref="info:doi/10.1029/JD092iD02p02189">10.1029/JD092iD02p02189</accessionId>
.</citation>
</selfCitationGroup>
<linkGroup>
<link type="toTypesetVersion" href="file:JGRD.JGRD669.pdf"></link>
</linkGroup>
</publicationMeta>
<contentMeta>
<titleGroup>
<title type="main">The kinetics of the reaction of OH With COS</title>
<title type="shortAuthors">Wahner and Ravishankara</title>
</titleGroup>
<creators>
<creator xml:id="jgrd669-cr-0001">
<personName>
<givenNames>Andreas</givenNames>
<familyName>Wahner</familyName>
</personName>
</creator>
<creator xml:id="jgrd669-cr-0002">
<personName>
<givenNames>A. R.</givenNames>
<familyName>Ravishankara</familyName>
</personName>
</creator>
</creators>
<abstractGroup>
<abstract type="main">
<p xml:id="jgrd669-para-0001">The laser/flash‐photolysis laser‐induced fluorescence technique was employed to study the reaction of OH with carbonyl sulfide (COS) in various buffer gases (He, N
<sub>2</sub>
, and SF
<sub>6</sub>
). In order to determine the relevance of this reaction to tropospheric chemistry the influence of O
<sub>2</sub>
on the rate constant was investigated. To avoid secondary reactions, especially the photolysis of COS, different photolytic OH precursors (H
<sub>2</sub>
O
<sub>2</sub>
, HNO
<sub>3</sub>
, and HONO) with different photolysis light sources (Xe flash lamp, ArF laser, fourth‐harmonic Nd: YAG laser, XeF laser, and third‐harmonic Nd: YAG laser) were used. The rate constant (1.92±0.25)×10
<sup>−15</sup>
cm
<sup>3</sup>
s
<sup>−1</sup>
for the reaction of OH with COS at room temperature was found (after correcting for H
<sub>2</sub>
S impurity) to be independent of the pressure and the buffer gas. Addition of O
<sub>2</sub>
was found to have no influence on the measured rate constant. Certain experiments were carried out at 298 K and 245 K to ascertain the mechanism for this reaction. Our results suggest that the degradation pathway involving homogeneous gas phase reaction of COS with OH is of minor importance in the troposphere.</p>
</abstract>
</abstractGroup>
</contentMeta>
</header>
</component>
</istex:document>
</istex:metadataXml>
<mods version="3.6">
<titleInfo lang="en">
<title>The kinetics of the reaction of OH With COS</title>
</titleInfo>
<titleInfo type="alternative" contentType="CDATA" lang="en">
<title>The kinetics of the reaction of OH With COS</title>
</titleInfo>
<name type="personal">
<namePart type="given">Andreas</namePart>
<namePart type="family">Wahner</namePart>
</name>
<name type="personal">
<namePart type="given">A. R.</namePart>
<namePart type="family">Ravishankara</namePart>
</name>
<typeOfResource>text</typeOfResource>
<genre type="article" displayLabel="article"></genre>
<originInfo>
<publisher>Blackwell Publishing Ltd</publisher>
<dateIssued encoding="w3cdtf">1987-02-20</dateIssued>
<dateCaptured encoding="w3cdtf">1986-08-01</dateCaptured>
<dateValid encoding="w3cdtf">1986-10-24</dateValid>
<edition>Wahner, A., and A. R. Ravishankara (1987), The kinetics of the reaction of OH With COS, J. Geophys. Res., 92(D2), 2189–2194, doi:10.1029/JD092iD02p02189.</edition>
<copyrightDate encoding="w3cdtf">1987</copyrightDate>
</originInfo>
<language>
<languageTerm type="code" authority="rfc3066">en</languageTerm>
<languageTerm type="code" authority="iso639-2b">eng</languageTerm>
</language>
<physicalDescription>
<internetMediaType>text/html</internetMediaType>
</physicalDescription>
<abstract>The laser/flash‐photolysis laser‐induced fluorescence technique was employed to study the reaction of OH with carbonyl sulfide (COS) in various buffer gases (He, N2, and SF6). In order to determine the relevance of this reaction to tropospheric chemistry the influence of O2 on the rate constant was investigated. To avoid secondary reactions, especially the photolysis of COS, different photolytic OH precursors (H2O2, HNO3, and HONO) with different photolysis light sources (Xe flash lamp, ArF laser, fourth‐harmonic Nd: YAG laser, XeF laser, and third‐harmonic Nd: YAG laser) were used. The rate constant (1.92±0.25)×10−15 cm3 s−1 for the reaction of OH with COS at room temperature was found (after correcting for H2S impurity) to be independent of the pressure and the buffer gas. Addition of O2 was found to have no influence on the measured rate constant. Certain experiments were carried out at 298 K and 245 K to ascertain the mechanism for this reaction. Our results suggest that the degradation pathway involving homogeneous gas phase reaction of COS with OH is of minor importance in the troposphere.</abstract>
<relatedItem type="host">
<titleInfo>
<title>Journal of Geophysical Research: Atmospheres</title>
</titleInfo>
<titleInfo type="abbreviated">
<title>J. Geophys. Res.</title>
</titleInfo>
<genre type="journal">journal</genre>
<subject>
<genre>index-terms</genre>
<topic authorityURI="http://psi.agu.org/taxonomy5/0300">ATMOSPHERIC COMPOSITION AND STRUCTURE</topic>
<topic authorityURI="http://psi.agu.org/taxonomy5/0365">Troposphere: composition and chemistry</topic>
</subject>
<subject>
<genre>article-category</genre>
<topic>Regular Issue</topic>
</subject>
<identifier type="ISSN">0148-0227</identifier>
<identifier type="eISSN">2156-2202</identifier>
<identifier type="DOI">10.1002/(ISSN)2156-2202d</identifier>
<identifier type="CODEN">JGREA2</identifier>
<identifier type="PublisherID">JGRD</identifier>
<part>
<date>1987</date>
<detail type="volume">
<caption>vol.</caption>
<number>92</number>
</detail>
<detail type="issue">
<caption>no.</caption>
<number>D2</number>
</detail>
<extent unit="pages">
<start>2189</start>
<end>2194</end>
<total>6</total>
</extent>
</part>
</relatedItem>
<identifier type="istex">52174110CB10DF095DF5BB8309038A0A07ACFF89</identifier>
<identifier type="DOI">10.1029/JD092iD02p02189</identifier>
<identifier type="ArticleID">6D0632</identifier>
<accessCondition type="use and reproduction" contentType="copyright">Copyright 1987 by the American Geophysical Union.</accessCondition>
<recordInfo>
<recordContentSource>WILEY</recordContentSource>
</recordInfo>
</mods>
</metadata>
<serie></serie>
</istex>
</record>

Pour manipuler ce document sous Unix (Dilib)

EXPLOR_STEP=$WICRI_ROOT/Ticri/CIDE/explor/OcrV1/Data/Istex/Corpus
HfdSelect -h $EXPLOR_STEP/biblio.hfd -nk 001538 | SxmlIndent | more

Ou

HfdSelect -h $EXPLOR_AREA/Data/Istex/Corpus/biblio.hfd -nk 001538 | SxmlIndent | more

Pour mettre un lien sur cette page dans le réseau Wicri

{{Explor lien
   |wiki=    Ticri/CIDE
   |area=    OcrV1
   |flux=    Istex
   |étape=   Corpus
   |type=    RBID
   |clé=     ISTEX:52174110CB10DF095DF5BB8309038A0A07ACFF89
   |texte=   The kinetics of the reaction of OH With COS
}}

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