Water vapor line parameters from 6450 to 9400 cm-1 / L. Régalia [et al.]
Уровень набора: Journal of Quantitative Spectroscopy and Radiative Transfer = 1961-Язык: английский.Страна: .Резюме или реферат: The spectra of natural water vapor were recorded in the spectral range 6450–9400 cm-1 with a step-by-step Fourier transform spectrometer at room temperature with absorption path lengths up to 1200 m. Positions, intensities and self-broadening coefficients of about 11,000 lines were determined. This paper focuses on the intensity parameters: the lines of four isotopologues H216O, H218O, H217O and HD16O were observed and assigned; it presents a new experimental dataset in the 6450–9400 cm-1 spectral range. Obtained results were compared to the literature data. Fifty-nine new and corrected energy levels of H216O and H217O were determined from the vibration–rotation analysis of the observed lines. A brief discussion is added for self-broadening coefficients at the end of this paper..Примечания о наличии в документе библиографии/указателя: [References: p. 135-136 (83 tit.)].Аудитория: .Тематика: электронный ресурс | труды учёных ТПУ | водяные пары | инфракрасная спектроскопия Ресурсы он-лайн:Щелкните здесь для доступа в онлайнTitle screen
[References: p. 135-136 (83 tit.)]
The spectra of natural water vapor were recorded in the spectral range 6450–9400 cm-1 with a step-by-step Fourier transform spectrometer at room temperature with absorption path lengths up to 1200 m. Positions, intensities and self-broadening coefficients of about 11,000 lines were determined. This paper focuses on the intensity parameters: the lines of four isotopologues H216O, H218O, H217O and HD16O were observed and assigned; it presents a new experimental dataset in the 6450–9400 cm-1 spectral range. Obtained results were compared to the literature data. Fifty-nine new and corrected energy levels of H216O and H217O were determined from the vibration–rotation analysis of the observed lines. A brief discussion is added for self-broadening coefficients at the end of this paper.
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