Experimental and theoretical studies of the C2F4 + O reaction: Nonadiabatic reaction mechanism
dc.contributor.author | Nguyen, T.L. | |
dc.contributor.author | Dils, B. | |
dc.contributor.author | Carl, S.A. | |
dc.contributor.author | Vereecken, L. | |
dc.contributor.author | Peeters, J. | |
dc.date | 2005 | |
dc.date.accessioned | 2016-12-07T10:36:06Z | |
dc.date.available | 2016-12-07T10:36:06Z | |
dc.identifier.uri | https://orfeo.belnet.be/handle/internal/4636 | |
dc.description | In this work, the C2F4(X1Ag) + O(3P) reaction was investigated experimentally using molecular beam-threshold ionization mass spectrometry (MB-TIMS). The major primary products were observed to be CF2O (+ CF2) and CF 3 (+ CFO), with measured approximate yields of 84-11 +7% versus 16-7 +11%, respectively, neglecting minor products. Furthermore, the lowest-lying triplet and singlet potential energy surfaces for this reaction were constructed theoretically using B3LYP, G2M(UCC, MP2), CBS-QB3, and G3 methods in combination with various basis sets such as 6-31G(d), 6-31l+G(3df), and cc-pVDZ. The primary product distribution for the multiwell multichannel reaction was then determined by RRKM statistical rate theory and weak-collision master equation analysis. It was found that the observed production of CF3 (+ CFO) can only occur on the singlet surface, in parallel with formation of ca. 5 times more CF2O(X) + CF2(X1A1). This requires fast intersystem crossing (ISC) from the triplet to the singlet surface at a rate of ca. 4 × 1012 s-1. The theoretical calculations combined with the experimental results thus indicate that the yield of triplet CF 2(ã3B1 + CF2O formed on the triplet surface prior to ISC is ≤35%, whereas singlet CF2(X 1A1) + CF2O is produced with yield ≥60%, after ISC. In addition, the thermal rate coefficients k(O + C2F 4) in the T = 150-1500 K range were computed using multistate transition state theory and can be expressed as k(T) = 1.67 × 10 -16 × T1.48 cm3 molecule-1 s-1; they are in agreement with the available experimental results in the T = 298-500 K range. | |
dc.language | eng | |
dc.title | Experimental and theoretical studies of the C2F4 + O reaction: Nonadiabatic reaction mechanism | |
dc.type | Article | |
dc.subject.frascati | Chemical sciences | |
dc.audience | Scientific | |
dc.subject.free | Carbon inorganic compounds | |
dc.subject.free | Ionization | |
dc.subject.free | Mass spectrometry | |
dc.subject.free | Molecular dynamics | |
dc.subject.free | Oxygen | |
dc.subject.free | Potential energy | |
dc.subject.free | Statistical methods | |
dc.subject.free | Molecular beam-threshold ionization mass spectrometry (MB-TIMS) | |
dc.subject.free | Multiwell multichannel reactions | |
dc.subject.free | Nonadiabatic reaction mechanisms | |
dc.subject.free | Potential energy surfaces | |
dc.subject.free | Reaction kinetics | |
dc.source.title | Journal of Physical Chemistry A | |
dc.source.volume | 109 | |
dc.source.issue | 43 | |
dc.source.page | 9786-9794 | |
Orfeo.peerreviewed | Yes | |
dc.identifier.doi | 10.1021/jp053585y | |
dc.identifier.scopus | 2-s2.0-27744566467 |