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CW-Cavity Ring Down Spectroscopy of O3. Part 3: Analysis of the 6490–6900 cm region and overview comparison with the O3 main isotopologue
Authors:E. Starikova   A. Barbe   Vl.G. Tyuterev   M.-R. De Backer-Barilly   S. Kassi  A. Campargue
Affiliation:aGroupe de Spectrométrie Moléculaire et Atmosphérique, UMR CNRS 6089, UFR Sciences Exactes et Naturelles, BP 1039-51687 Reims Cedex 2, France;bLaboratory of Theoretical Spectroscopy, Institute of Atmospheric Optics, Russian Academy of Sciences, 1, Av. Akademicheskii, Tomsk 634055, Russia;cLaboratoire de Spectrométrie Physique, UMR CNRS 5588, Université Joseph Fourier, BP 87-38402 Saint Martin d’Hères Cedex, France
Abstract:This paper is devoted to the third part of the analysis of the very weak absorption spectrum of the 18O3 isotopologue of ozone recorded by CW-Cavity Ring Down Spectroscopy between 5930 and 6900 cm−1. In the two first parts [A. Campargue, A. Liu, S. Kassi, D. Romanini, M.-R. De Backer-Barilly, A. Barbe, E. Starikova, S.A. Tashkun, Vl.G. Tyuterev, J. Mol. Spectrosc. (2009), doi: 10.1016/j.jms.2009.02.012 and E. Starikova, M.-R. De Backer-Barilly, A. Barbe, Vl.G. Tyuterev, A. Campargue, A.W.Liu, S. Kassi, J. Mol. Spectrosc. (2009) doi: 10.1016/j.jms.2009.03.013], the effective operators approach was used to model the spectrum in the 6200–6400 and 5930–6080 cm−1 regions, respectively. The analysis of the whole investigated region is completed by the present investigation of the 6490–6900 cm−1 upper range. Three sets of interacting states have been treated separately. The first one falls in the 6490–6700 cm−1 region, where 1555 rovibrational transitions were assigned to three A-type bands: 3ν2 + 5ν3, 5ν1 + ν2 + ν3 and 2ν1 + 3ν2 + 3ν3 and one B-type band: ν1 + 3ν2 + 4ν3. The corresponding line positions were reproduced with an rms deviation of 18.4 × 10−3 cm−1 by using an effective Hamiltonian (EH) model involving eight vibrational states coupled by resonance interactions. In the highest spectral region – 6700–6900 cm−1 – 389 and 183 transitions have been assigned to the ν1 + 2ν2 + 5ν3 and 4ν1 + 3ν2 + ν3 A-type bands, respectively. These very weak bands correspond to the most excited upper vibrational states observed so far in ozone. The line positions of the ν1 + 2ν2 + 5ν3 band were reproduced with an rms deviation of 7.3 × 10−3 cm−1 by using an EH involving the {(054), (026), (125)} interacting states. The coupling of the (431) upper state with the (502) dark state was needed to account for the observed line positions of the 4ν1 + 3ν2 + ν3 band (rms = 5.7 × 10−3 cm−1).The dipole transition moment parameters were determined for the different observed bands. The obtained set of parameters and the experimentally determined energy levels were used to generate a complete line list provided as Supplementary Materials.The results of the analyses of the whole 5930–6900 cm−1 spectral region were gathered and used for a comparison of the band centres to their calculated values. The agreement achieved for both 18O3 and 16O3 (average difference on the order of 1 cm−1) indicates that the used potential energy surface provides accurate predictions up to a vibrational excitation approaching 80% of the dissociation energy. The comparison of the 18O3 and 16O3 band intensities is also discussed, opening a field of questions concerning the variation of the dipole moments and resonance intensity borrowing by isotopic substitution.
Keywords:Ozone   18O3   16O3   Cavity Ring Down Spectroscopy   Effective Hamiltonian model   Potential function
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