Abstract
The spectra of ozone, enriched by 17O oxygen, were recorded and reinvestigated in the 5 μm and 10 μm regions using the Reims Fourier Transform Spectrometer. Here we focus on the analysis of the ν1, ν3 and ν1+ν3 bands of the 16O17O16O isotopologue, which were modeled simultaneously to improve the parameters of the ground state energy level. The analysis of the ν1+ν3 bands of 16O16O17O is also extended. We report here the new system of effective Hamiltonian parameters, give some examples of comparison between observed and simulated spectra, and of the improvement for the ro-vibrational transition data available in spectroscopic databases.
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