000890998 001__ 890998
000890998 005__ 20240712101006.0
000890998 0247_ $$2doi$$a10.5194/acp-20-10459-2020
000890998 0247_ $$2ISSN$$a1680-7316
000890998 0247_ $$2ISSN$$a1680-7324
000890998 0247_ $$2Handle$$a2128/27384
000890998 0247_ $$2altmetric$$aaltmetric:90051972
000890998 0247_ $$2WOS$$aWOS:000569419500001
000890998 037__ $$aFZJ-2021-01305
000890998 082__ $$a550
000890998 1001_ $$0P:(DE-HGF)0$$aDewald, Patrick$$b0
000890998 245__ $$aEvolution of NO<sub>3</sub> reactivity during the oxidation of isoprene
000890998 260__ $$aKatlenburg-Lindau$$bEGU$$c2020
000890998 3367_ $$2DRIVER$$aarticle
000890998 3367_ $$2DataCite$$aOutput Types/Journal article
000890998 3367_ $$0PUB:(DE-HGF)16$$2PUB:(DE-HGF)$$aJournal Article$$bjournal$$mjournal$$s1615559259_28207
000890998 3367_ $$2BibTeX$$aARTICLE
000890998 3367_ $$2ORCID$$aJOURNAL_ARTICLE
000890998 3367_ $$00$$2EndNote$$aJournal Article
000890998 520__ $$aIn a series of experiments in an atmospheric simulation chamber (SAPHIR,1 Forschungszentrum Jülich, Germany), NO3 reactivity (kNO3) resulting from the reaction of NO3 with isoprene and stable trace gases formed as products was measured directly using a flow tube reactor coupled to a cavity ring-down spectrometer (FT-CRDS). The experiments were carried out in both dry and humid air with variation of the initial mixing ratios of ozone (50–100 ppbv), isoprene (3–22 ppbv) and NO2 (5–30 ppbv). kNO3 was in excellent agreement with values calculated from the isoprene mixing ratio and the rate coefficient for the reaction of NO3 with isoprene. This result serves to confirm that the FT-CRDS returns accurate values of kNO3 even at elevated NO2 concentrations and to show that reactions of NO3 with stable reaction products like non-radical organic nitrates do not contribute significantly to NO3 reactivity during the oxidation of isoprene. A comparison of kNO3 with NO3 reactivities calculated from NO3 mixing ratios and NO3 production rates suggests that organic peroxy radicals and HO2 account for ∼50 % of NO3 losses. This contradicts predictions based on numerical simulations using the Master Chemical Mechanism (MCM version 3.3.1) unless the rate coefficient for reaction between NO3 and isoprene-derived RO2 is roughly doubled to ∼5×10−12 cm3 molecule−1 s−1.
000890998 536__ $$0G:(DE-HGF)POF3-243$$a243 - Tropospheric trace substances and their transformation processes (POF3-243)$$cPOF3-243$$fPOF III$$x0
000890998 588__ $$aDataset connected to CrossRef
000890998 7001_ $$0P:(DE-HGF)0$$aLiebmann, Jonathan M.$$b1
000890998 7001_ $$00000-0002-3143-8705$$aFriedrich, Nils$$b2
000890998 7001_ $$0P:(DE-HGF)0$$aShenolikar, Justin$$b3
000890998 7001_ $$0P:(DE-HGF)0$$aSchuladen, Jan$$b4
000890998 7001_ $$0P:(DE-Juel1)16347$$aRohrer, Franz$$b5$$ufzj
000890998 7001_ $$0P:(DE-Juel1)171432$$aReimer, David$$b6$$ufzj
000890998 7001_ $$0P:(DE-Juel1)5344$$aTillmann, Ralf$$b7$$ufzj
000890998 7001_ $$0P:(DE-Juel1)166537$$aNovelli, Anna$$b8
000890998 7001_ $$0P:(DE-Juel1)174162$$aCho, Changmin$$b9
000890998 7001_ $$0P:(DE-HGF)0$$aXu, Kangming$$b10
000890998 7001_ $$0P:(DE-HGF)0$$aHolzinger, Rupert$$b11
000890998 7001_ $$0P:(DE-HGF)0$$aBernard, François$$b12
000890998 7001_ $$0P:(DE-HGF)0$$aZhou, Li$$b13
000890998 7001_ $$0P:(DE-HGF)0$$aMellouki, Wahid$$b14
000890998 7001_ $$0P:(DE-HGF)0$$aBrown, Steven S.$$b15
000890998 7001_ $$0P:(DE-Juel1)7363$$aFuchs, Hendrik$$b16
000890998 7001_ $$00000-0001-6307-3846$$aLelieveld, Jos$$b17
000890998 7001_ $$00000-0001-8669-0230$$aCrowley, John N.$$b18$$eCorresponding author
000890998 773__ $$0PERI:(DE-600)2069847-1$$a10.5194/acp-20-10459-2020$$gVol. 20, no. 17, p. 10459 - 10475$$n17$$p10459 - 10475$$tAtmospheric chemistry and physics$$v20$$x1680-7324$$y2020
000890998 8564_ $$uhttps://juser.fz-juelich.de/record/890998/files/acp-20-10459-2020.pdf$$yOpenAccess
000890998 909CO $$ooai:juser.fz-juelich.de:890998$$pdnbdelivery$$pVDB$$pVDB:Earth_Environment$$pdriver$$popen_access$$popenaire
000890998 915__ $$0StatID:(DE-HGF)0200$$2StatID$$aDBCoverage$$bSCOPUS$$d2021-02-02
000890998 915__ $$0StatID:(DE-HGF)0160$$2StatID$$aDBCoverage$$bEssential Science Indicators$$d2021-02-02
000890998 915__ $$0LIC:(DE-HGF)CCBY4$$2HGFVOC$$aCreative Commons Attribution CC BY 4.0
000890998 915__ $$0StatID:(DE-HGF)1150$$2StatID$$aDBCoverage$$bCurrent Contents - Physical, Chemical and Earth Sciences$$d2021-02-02
000890998 915__ $$0StatID:(DE-HGF)9905$$2StatID$$aIF >= 5$$bATMOS CHEM PHYS : 2019$$d2021-02-02
000890998 915__ $$0StatID:(DE-HGF)0501$$2StatID$$aDBCoverage$$bDOAJ Seal$$d2021-02-02
000890998 915__ $$0StatID:(DE-HGF)0500$$2StatID$$aDBCoverage$$bDOAJ$$d2021-02-02
000890998 915__ $$0StatID:(DE-HGF)0113$$2StatID$$aWoS$$bScience Citation Index Expanded$$d2021-02-02
000890998 915__ $$0StatID:(DE-HGF)0700$$2StatID$$aFees$$d2021-02-02
000890998 915__ $$0StatID:(DE-HGF)0150$$2StatID$$aDBCoverage$$bWeb of Science Core Collection$$d2021-02-02
000890998 915__ $$0StatID:(DE-HGF)0510$$2StatID$$aOpenAccess
000890998 915__ $$0StatID:(DE-HGF)0030$$2StatID$$aPeer Review$$bDOAJ : Peer review$$d2021-02-02
000890998 915__ $$0StatID:(DE-HGF)0561$$2StatID$$aArticle Processing Charges$$d2021-02-02
000890998 915__ $$0StatID:(DE-HGF)0100$$2StatID$$aJCR$$bATMOS CHEM PHYS : 2019$$d2021-02-02
000890998 915__ $$0StatID:(DE-HGF)0300$$2StatID$$aDBCoverage$$bMedline$$d2021-02-02
000890998 915__ $$0StatID:(DE-HGF)0199$$2StatID$$aDBCoverage$$bClarivate Analytics Master Journal List$$d2021-02-02
000890998 9141_ $$y2020
000890998 9101_ $$0I:(DE-588b)5008462-8$$6P:(DE-Juel1)16347$$aForschungszentrum Jülich$$b5$$kFZJ
000890998 9101_ $$0I:(DE-588b)5008462-8$$6P:(DE-Juel1)171432$$aForschungszentrum Jülich$$b6$$kFZJ
000890998 9101_ $$0I:(DE-588b)5008462-8$$6P:(DE-Juel1)5344$$aForschungszentrum Jülich$$b7$$kFZJ
000890998 9101_ $$0I:(DE-588b)5008462-8$$6P:(DE-Juel1)166537$$aForschungszentrum Jülich$$b8$$kFZJ
000890998 9101_ $$0I:(DE-588b)5008462-8$$6P:(DE-Juel1)174162$$aForschungszentrum Jülich$$b9$$kFZJ
000890998 9101_ $$0I:(DE-588b)5008462-8$$6P:(DE-Juel1)7363$$aForschungszentrum Jülich$$b16$$kFZJ
000890998 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
000890998 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$$x0
000890998 9201_ $$0I:(DE-Juel1)IEK-8-20101013$$kIEK-8$$lTroposphäre$$x0
000890998 9801_ $$aFullTexts
000890998 980__ $$ajournal
000890998 980__ $$aVDB
000890998 980__ $$aUNRESTRICTED
000890998 980__ $$aI:(DE-Juel1)IEK-8-20101013
000890998 981__ $$aI:(DE-Juel1)ICE-3-20101013