10min:
ANALYSIS OF AN 18O AND D ENHANCED FT-IBBCEAS WATER SPECTRUM: NEW ASSIGNMENTS FOR HD18O, HD16O, D218O AND D216O IN THE NEAR-INFRARED REGION (6000-7000~cm-1)..

MICHAEL J. DOWN, JONATHAN TENNYSON, Department of Physics and Astronomy, University College London, London, WC1E 6BT, UK; JOHANNES ORPHAL, Karlsruher Institut für Technologie, IMK-ASF, Postfach 36 40, 76021 Karlsruhe, Germany; PASCALE CHELIN, Laboratoire Interuniversitaire des Systèmes Atmosphériques (LISA), Université de Paris-Est, CNRS UMR 7583, Créteil, France; AND ALBERT A. RUTH, Physics Department and Environmental Research Institute, University College Cork, Cork, Ireland.

An experimental infrared spectrum recorded using isotopically enriched water in the 6000-7000~cm-1 region with a spectral resolution of 0.02~cm-1 is analysed and assigned. The spectrum employs a combination of Fourier-transform (FT) spectroscopy and incoherent broad-band cavity-enhanced absorption spectroscopy (IBBCEAS) . Application of FT-IBBCEAS to a sample mixture of 8.0 mbar of D2O and 12.4 mbar of pure H218O in the optical cavity resulted in the observation of a large number of new absorption features in the spectrum, notably due to the rare HD18O isotope of water. This was possible due to the superior absorption sensitivity of FT-IBB-CEAS compared to other techniques previously employed in this region

combined with the prescence of D216O in the sample. The assignment procedure is based on the use of known transition frequencies for H216O and H218O, existing variational line lists for HD16O

and D216O

and newly calculated variational line lists for HD18O and D218O, with a uniform intensity threshold applied. The main absorption comes from HD16O and HD18O, for which there are few previous assignments in the region.

The following new spectral features were identified. D216O: 265 (all labelled); D218O: 194 (all lower levels labelled); HD16O: 213 (all labelled); HD18O: 743 (all lower and 612 upper levels labelled). In all 3226 of the 4768 lines observed in the spectrum are assigned, resulting in a significant number of newly determined energy levels. The analysis demonstrates both the usefulness of this experimental approach for spectroscopic investigations of isotopic or dangerous samples, and the validity of the new variational line lists.