Please use this identifier to cite or link to this item: http://hdl.handle.net/10397/89877
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dc.contributorDepartment of Applied Biology and Chemical Technologyen_US
dc.creatorChow, Ren_US
dc.creatorMok, DKWen_US
dc.date.accessioned2021-05-13T08:31:57Z-
dc.date.available2021-05-13T08:31:57Z-
dc.identifier.issn1463-9076en_US
dc.identifier.urihttp://hdl.handle.net/10397/89877-
dc.language.isoenen_US
dc.publisherRoyal Society of Chemistryen_US
dc.rightsThis journal is © the Owner Societies 2020en_US
dc.rightsThe following publication Chow, R., & Mok, D. K. W. (2020). A theoretical study of the addition of CH2OO to hydroxymethyl hydroperoxide and its implications on SO3 formation in the atmosphere. Physical Chemistry Chemical Physics, 22(25), 14130-14141 is available at https://dx.doi.org/10.1039/D0CP00961J.en_US
dc.titleA theoretical study of the addition of CH2OO to hydroxymethyl hydroperoxide and its implications on SO3 formation in the atmosphereen_US
dc.typeJournal/Magazine Articleen_US
dc.identifier.spage14130en_US
dc.identifier.epage14141en_US
dc.identifier.volume22en_US
dc.identifier.issue25en_US
dc.identifier.doi10.1039/d0cp00961jen_US
dcterms.abstractThe reaction of hydroxymethyl hydroperoxide (HMHP, HOCH2OOH) with the simplest Criegee intermediate, CH2OO, has been examined using quantum chemical methods with transition state theory. Geometry optimization and IRC calculations were performed using the M06-2X, MN15-L, and B2PLYP-D3 functionals in conjunction with the aug-cc-pVTZ basis set. Single point energy calculations using QCISD(T) and BD(T) with the same basis set have been performed to determine the energy of reactants, reactive complexes, transition states, and products. Rate coefficients have been obtained using variational transition state theory. The addition of CH2OO on the three different oxygen atoms in HMHP has been considered and the ether oxide forming channel, CH2OO + HOCH2OOH → HOCH2O(O)CH2OOH (channel 2), is the most favorable. The best computed standard enthalpy of reaction (ΔHRX298K) and zero-point corrected barrier height are -20.02 and -6.33 kcal mol-1, respectively. The reaction barrier is negative and our results suggest that both the inner and outer transition states contribute to the corresponding overall reactive flux in the tropospheric temperature range (220 K to 320 K). A two-transition state model has been used to obtain reliable rate coefficients at the high-pressure limit. The pressure-dependent rate coefficient calculations using the SS-QRRK theory have shown that this channel is pressure-dependent. Moreover, our investigation has shown that the ether oxide formed may rapidly react with SO2 at 298 K to form SO3, which can, in turn, react with water to form atmospheric H2SO4. A similar calculation has been conducted for the reaction of HMHP with OH, suggesting that the titled reaction may be a significant sink of HMHP. Therefore, the reaction between CH2OO and HOCH2OOH could be an indirect source for generating atmospheric H2SO4, which is crucial to the formation of clouds, and it might relieve global warming.en_US
dcterms.accessRightsopen accessen_US
dcterms.bibliographicCitationPhysical chemistry chemical physics, 7 July 2020, v. 22, no. 25, p. 14130-14141en_US
dcterms.isPartOfPhysical chemistry chemical physicsen_US
dcterms.issued2020-07-07-
dc.identifier.scopus2-s2.0-85087532801-
dc.identifier.pmid32542295-
dc.identifier.eissn1463-9084en_US
dc.description.validate202105 bchyen_US
dc.description.oaAccepted Manuscripten_US
dc.identifier.FolderNumbera0743-n03-
dc.identifier.SubFormID1419-
dc.description.fundingSourceRGCen_US
dc.description.fundingText15301315en_US
dc.description.pubStatusPublisheden_US
dc.description.oaCategoryGreen (AAM)en_US
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