THE $v_{3}$ AND $v_{1}$ BANDS OF THE $^{17}O^{16}O^{16}O$ AND $^{16}O^{17}O^{18}O$ IS0TOPIC SPECIES OF OZONE: LINE POSITIONS AND INTENSITIES,

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1992

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Ohio State University

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Room temperature absorption spectra of 17O-enriched ozone have been recorded around 10 μm at 0.005cm−1 resolution with the Fourier transform spectrometer located in the McMath solar telescope on Kitt Peak. Using these data, the first analysis of the v3 (A-type) and v1 (B-type) bands of 16O17O18O together with the hybrid (both A- and B- type) v3 and v1 bands of 17O16O18O isotopic species of ozone was performed, leading to the following band centers v0(v1)=1095.69309cm−1 v0(v3)−1035.35869cm−1 and v0(v1)−1087,82895cm−1, v0(v3)−1024.39553cm−1 respectively for the 16O17O18O and 17O16O16O isotopic species. The experimental rotational energy levels of the [(100) (001)] interacting vibrational states were very satisfactorily reproduced using a Hamilton matrix which takes explicity into account the Coriolis interactions for the 17O18O (C2v -symmetry) and both formi- and coriolis-type interactions for 17O 17O16O16O (C2 - symmetry). For the 16O17O16O isotopic species the line intensities were calculated by transferring the dipole moment function of 16O3 to 16O17O16O. These intensities were then used to determine the amount of 16O17O16O in the cell and, assuming a factor of 2 between the abundances of 17O16O16O and 16O17O16O, the amount of 17O16O16O was evaluated allowing the measurement of 70 line intensities of the v1 and v3 band lines of this last species. From these experimental values, the coefficients appearing in the transformed transition moment operators of these bands were derived. Finally, a complete spectrum of the v1 and v3 bands of 16O17O16O and 17O16O16O has been generated.""

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Author Institution: Laboratoire de Physique Moleculaire et Applications, C. N. R. S., Universit'{e} Pierre et Marie Curie; Atmosphere Science Division, NASA Langley Research Center; Department of Physics, College of William and Mary

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