The 2nu1 + nu2 + 2nu3 band of ozone, occurring in the 4780 cm-1 region, has been observed for the first time, using a Fourier transform spectrometer, at 0.008 cm-1 resolution and using a large path length pressure product. Assignments of vibration-rotational transitions have been made up to J = 48 a
Analysis of the (ν1 + ν2) and (ν2 + ν3) combination bands of ozone
✍ Scribed by Christopher C Jones; John H Shaw
- Publisher
- Elsevier Science
- Year
- 1977
- Tongue
- English
- Weight
- 471 KB
- Volume
- 68
- Category
- Article
- ISSN
- 0022-2852
No coin nor oath required. For personal study only.
📜 SIMILAR VOLUMES
The 2600 -2900 cm Ϫ1 spectral range is revisited for an accurate determination of line intensities of the 2 1 ϩ 2 , 1 ϩ 2 ϩ 3 , and 2 ϩ 2 3 bands of ozone. The fit on 1702 energy levels of ( 012), (111), and (210) states determined from observed transitions with J max Յ 61 and K a max Յ 17 gives a r
Using a Fourier transform spectrometer, we have recorded the spectra of ozone in the region of 4600 cm 01 , with a resolution of 0.008 cm 01 . The strongest absorption in this region is due to the n 1 / n 2 / 3n 3 band which is in Coriolis interaction with the n 2 / 4n 3 band. We have been able to a