000889016 001__ 889016 000889016 005__ 20240712100949.0 000889016 0247_ $$2doi$$a10.5194/acp-20-13541-2020 000889016 0247_ $$2ISSN$$a1680-7316 000889016 0247_ $$2ISSN$$a1680-7324 000889016 0247_ $$2Handle$$a2128/27433 000889016 0247_ $$2altmetric$$aaltmetric:94195564 000889016 0247_ $$2WOS$$aWOS:000589246000001 000889016 037__ $$aFZJ-2020-05390 000889016 041__ $$aEnglish 000889016 082__ $$a550 000889016 1001_ $$0P:(DE-HGF)0$$aBerasategui, Matias$$b0$$eFirst author 000889016 245__ $$aReaction between CH<sub>3</sub>C(O)OOH (peracetic acid) and OH in the gas phase: a combined experimental and theoretical study of the kinetics and mechanism 000889016 260__ $$aKatlenburg-Lindau$$bEGU$$c2020 000889016 3367_ $$2DRIVER$$aarticle 000889016 3367_ $$2DataCite$$aOutput Types/Journal article 000889016 3367_ $$0PUB:(DE-HGF)16$$2PUB:(DE-HGF)$$aJournal Article$$bjournal$$mjournal$$s1615973989_29632 000889016 3367_ $$2BibTeX$$aARTICLE 000889016 3367_ $$2ORCID$$aJOURNAL_ARTICLE 000889016 3367_ $$00$$2EndNote$$aJournal Article 000889016 520__ $$aPeracetic acid (CH3C(O)OOH) is one of the mostabundant organic peroxides in the atmosphere; yet the kinetics of itsreaction with OH, believed to be the major sink, have only been studied onceexperimentally. In this work we combine a pulsed-laser photolysis kineticstudy of the title reaction with theoretical calculations of the ratecoefficient and mechanism. We demonstrate that the rate coefficient isorders of magnitude lower than previously determined, with an experimentallyderived upper limit of 4×10-14 cm3 molec.−1 s−1. The relatively low rate coefficient is in good agreement withthe theoretical result of 3×10-14 cm3 molec.−1 s−1 at 298 K, increasing to ∼6×10-14 cm3 molec.−1 s−1 in the cold uppertroposphere but with associated uncertainty of a factor of 2. The reactionproceeds mainly via abstraction of the peroxidic hydrogen via a relativelyweakly bonded and short-lived prereaction complex, in which H abstractionoccurs only slowly due to a high barrier and low tunnelling probabilities.Our results imply that the lifetime of CH3C(O)OOH with respect toOH-initiated degradation in the atmosphere is of the order of 1 year (notdays as previously believed) and that its major sink in the free and uppertroposphere is likely to be photolysis, with deposition important in theboundary layer. 000889016 536__ $$0G:(DE-HGF)POF3-243$$a243 - Tropospheric trace substances and their transformation processes (POF3-243)$$cPOF3-243$$fPOF III$$x0 000889016 588__ $$aDataset connected to CrossRef 000889016 7001_ $$0P:(DE-HGF)0$$aAmedro, Damien$$b1 000889016 7001_ $$0P:(DE-Juel1)167140$$aVereecken, Luc$$b2 000889016 7001_ $$00000-0001-6307-3846$$aLelieveld, Jos$$b3 000889016 7001_ $$00000-0001-8669-0230$$aCrowley, John N.$$b4$$eCorresponding author 000889016 773__ $$0PERI:(DE-600)2069847-1$$a10.5194/acp-20-13541-2020$$gVol. 20, no. 21, p. 13541 - 13555$$n21$$p13541 - 13555$$tAtmospheric chemistry and physics$$v20$$x1680-7324$$y2020 000889016 8564_ $$uhttps://juser.fz-juelich.de/record/889016/files/Berasategui_ACP_2020_CH3COOOH%2BOH.pdf$$yOpenAccess 000889016 8564_ $$uhttps://juser.fz-juelich.de/record/889016/files/Berasategui_ACP_2020_CH3COOOH%2BOH_SI.pdf$$yRestricted 000889016 909CO $$ooai:juser.fz-juelich.de:889016$$pdnbdelivery$$pVDB$$pVDB:Earth_Environment$$pdriver$$popen_access$$popenaire 000889016 915__ $$0StatID:(DE-HGF)0200$$2StatID$$aDBCoverage$$bSCOPUS$$d2020-09-03 000889016 915__ $$0StatID:(DE-HGF)0160$$2StatID$$aDBCoverage$$bEssential Science Indicators$$d2020-09-03 000889016 915__ $$0LIC:(DE-HGF)CCBY4$$2HGFVOC$$aCreative Commons Attribution CC BY 4.0 000889016 915__ $$0StatID:(DE-HGF)0100$$2StatID$$aJCR$$bATMOS CHEM PHYS : 2018$$d2020-09-03 000889016 915__ $$0StatID:(DE-HGF)9905$$2StatID$$aIF >= 5$$bATMOS CHEM PHYS : 2018$$d2020-09-03 000889016 915__ $$0StatID:(DE-HGF)0501$$2StatID$$aDBCoverage$$bDOAJ Seal$$d2020-09-03 000889016 915__ $$0StatID:(DE-HGF)0500$$2StatID$$aDBCoverage$$bDOAJ$$d2020-09-03 000889016 915__ $$0StatID:(DE-HGF)0113$$2StatID$$aWoS$$bScience Citation Index Expanded$$d2020-09-03 000889016 915__ $$0StatID:(DE-HGF)0700$$2StatID$$aFees$$d2020-09-03 000889016 915__ $$0StatID:(DE-HGF)0150$$2StatID$$aDBCoverage$$bWeb of Science Core Collection$$d2020-09-03 000889016 915__ $$0StatID:(DE-HGF)0510$$2StatID$$aOpenAccess 000889016 915__ $$0StatID:(DE-HGF)0030$$2StatID$$aPeer Review$$bDOAJ : Peer review$$d2020-09-03 000889016 915__ $$0StatID:(DE-HGF)0561$$2StatID$$aArticle Processing Charges$$d2020-09-03 000889016 915__ $$0StatID:(DE-HGF)1150$$2StatID$$aDBCoverage$$bCurrent Contents - Physical, Chemical and Earth Sciences$$d2020-09-03 000889016 915__ $$0StatID:(DE-HGF)0300$$2StatID$$aDBCoverage$$bMedline$$d2020-09-03 000889016 915__ $$0StatID:(DE-HGF)0199$$2StatID$$aDBCoverage$$bClarivate Analytics Master Journal List$$d2020-09-03 000889016 9141_ $$y2020 000889016 9101_ $$0I:(DE-588b)5008462-8$$6P:(DE-Juel1)167140$$aForschungszentrum Jülich$$b2$$kFZJ 000889016 9131_ $$0G:(DE-HGF)POF3-243$$1G:(DE-HGF)POF3-240$$2G:(DE-HGF)POF3-200$$3G:(DE-HGF)POF3$$4G:(DE-HGF)POF$$aDE-HGF$$bErde und Umwelt$$lAtmosphäre und Klima$$vTropospheric trace substances and their transformation processes$$x0 000889016 9132_ $$0G:(DE-HGF)POF4-211$$1G:(DE-HGF)POF4-210$$2G:(DE-HGF)POF4-200$$3G:(DE-HGF)POF4$$4G:(DE-HGF)POF$$9G:(DE-HGF)POF4-2111$$aDE-HGF$$bForschungsbereich Erde und Umwelt$$lErde im Wandel – Unsere Zukunft nachhaltig gestalten$$vDie Atmosphäre im globalen Wandel$$x0 000889016 920__ $$lyes 000889016 9201_ $$0I:(DE-Juel1)IEK-8-20101013$$kIEK-8$$lTroposphäre$$x0 000889016 9801_ $$aFullTexts 000889016 980__ $$ajournal 000889016 980__ $$aVDB 000889016 980__ $$aUNRESTRICTED 000889016 980__ $$aI:(DE-Juel1)IEK-8-20101013 000889016 981__ $$aI:(DE-Juel1)ICE-3-20101013