High sensitivity Cavity Ring Down spectroscopy of 18O enriched carbon dioxide between 5850 and 7000 cm-1: Part II-Analysis and theoretical modeling of the 12C18O2, 13C18O2 and 16O13C18O spectra

被引:27
|
作者
Karlovets, E. V. [1 ,2 ]
Campargue, A. [1 ]
Mondelain, D. [1 ]
Kassi, S. [1 ]
Tashkun, S. A. [2 ]
Perevalov, V. I. [2 ]
机构
[1] Univ Grenoble 1, CNRS, LIPhy UMR5588, F-38041 Grenoble, France
[2] Russian Acad Sci, Lab Theoret Spect, VE Zuev Inst Atmospher Opt, SB, Tomsk 634021, Russia
关键词
Carbon dioxide; CO2; Isotopologue; Global modeling; Cavity Ring Down Spectroscopy; HITRAN; GEISA; CDSD; ABSOLUTE LINE-INTENSITIES; CW-CRDS; INFRARED-SPECTROSCOPY; ABSORPTION-SPECTRUM; MOLECULAR-CONSTANTS; SHIFT COEFFICIENTS; EMISSION-SPECTRA; BANDS; CO2; POSITIONS;
D O I
10.1016/j.jqsrt.2013.11.005
中图分类号
O43 [光学];
学科分类号
070207 ; 0803 ;
摘要
More than 19000 transitions belonging to 11 isotopologues of carbon dioxide have been assigned in the room temperature absorption spectrum of highly O-18 enriched carbon dioxide recorded by very high sensitivity CW-Cavity Ring Down spectroscopy between 5851 and 6990 cm(-1) (1.71-1.43 mu m). The line positions were determined with accuracy better than 1 x 10(-3) cm(-1) while the absolute line intensities are reported with an uncertainty better than 10%. This second report is devoted to the analysis of the bands of three multiply substituted isotopologues: (CO2)-C-12-O-18, (CO2)-C-13-O-18 and (OCO)-O-16-C-13-O-18 (828, 838 and 638 in short hand notation). On the basis of the predictions of effective Hamiltonian models, a total of 2870, 538 and 1375 transitions belonging to 59, 11 and 15 bands were rovibrationnally assigned for 828, 838 and 638, respectively. For comparison, only 11 bands were previously measured by Fourier Transform spectroscopy in the region, for the 828 species. All the identified bands correspond to a Delta P=9 variation of the polyad number (P=2V(1)+V-2+3V(3), where V-i are vibrational quantum numbers). The band-by-band analysis has allowed deriving accurate spectroscopic parameters of 81 bands from a fit of the measured line positions. A few resonance perturbations were identified. In particular, the 31113 and 51106 states of 638 belonging to different polyads (P=10 and P=11, respectively) are anharmonically coupled. Using the large set of newly measured line positions and those collected from the literature, the global modeling of the line positions within the effective Hamiltonian approach was performed and a new set of Hamiltonian parameters was obtained for each of the three considered isopotologues. Using a similar approach, the global fits of the obtained intensity values of the Delta P=9 series of transitions were used to derive the corresponding Delta P=9 effective dipole moment parameters of the three considered isotopologues. The obtained results will help to improve the quality of the spectral line parameters of the three considered minor isopotologues in the most currently used spectroscopic databases of carbon dioxide. (C) 2013 Elsevier Ltd. All rights reserved.
引用
收藏
页码:71 / 88
页数:18
相关论文
共 50 条
  • [41] Simultaneous measurement of δ13C, δ18O and δ17O of atmospheric CO2 - performance assessment of a dual-laser absorption spectrometer
    Steur, Pharahilda M.
    Scheeren, Hubertus A.
    Nelson, Dave D.
    McManus, J. Barry
    Meijer, Harro A. J.
    ATMOSPHERIC MEASUREMENT TECHNIQUES, 2021, 14 (06) : 4279 - 4304
  • [42] High-accuracy 12C16O2 line intensities in the 2 μm wavelength region measured by frequency-stabilized cavity ring-down spectroscopy
    Yi, Hongming
    Liu, Qingnan
    Gameson, Lyn
    Fleisher, Adam J.
    Hodges, Joseph T.
    JOURNAL OF QUANTITATIVE SPECTROSCOPY & RADIATIVE TRANSFER, 2018, 206 : 367 - 377
  • [43] Use of the isotope flux ratio approach to investigate the C18O16O and 13CO2 exchange near the floor of a temperate deciduous forest
    Santos, E.
    Wagner-Riddle, C.
    Lee, X.
    Warland, J.
    Brown, S.
    Staebler, R.
    Bartlett, P.
    Kim, K.
    BIOGEOSCIENCES, 2012, 9 (07) : 2385 - 2399
  • [44] An optimized sampling system for highly reproducible isotope ratio measurements (δ13C and δ18O) of pure CO2 gas by infrared spectroscopy
    Viallon, Joele
    Flores, Edgar
    Moussay, Philippe
    Chubchenko, Ian
    Rolle, Francesca
    Zhang, Tiqiang
    Mussell Webber, Eric B.
    Wielgosz, Robert, I
    METROLOGIA, 2020, 57 (05)
  • [45] In situ δ13C and δ18O microanalysis by SIMS: A method for characterizing the carbonate components of natural and engineered CO2-reservoirs
    Sliwinski, Maciej G.
    Kitajima, Kouki
    Kozdon, Reinhard
    Spicuzza, Michael J.
    Denny, Adam
    Valley, John W.
    INTERNATIONAL JOURNAL OF GREENHOUSE GAS CONTROL, 2017, 57 : 116 - 133
  • [46] Cavity Ring-Down Spectroscopy Performance and Procedures for High-Throughput δ18O and δ2H Measurement in Water Using "Express" Mode
    Galili, Nir
    Blattmann, Thomas M.
    Somlyay, Anna
    Gallarotti, Nora
    Eglinton, Timothy I.
    Hemingway, Jordon D.
    APPLIED SPECTROSCOPY, 2025,
  • [47] A Kinetic Difference Between 12C- and 13C-Bound Oxygen Exchange Rates Results in Decoupled δ18O and Δ47 Values of Equilibrating DIC Solutions
    Staudigel, Philip T.
    Swart, Peter K.
    GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS, 2018, 19 (08): : 2371 - 2383
  • [48] Maintaining consistent traceability in high-precision isotope measurements of CO2: a way to verify atmospheric trends of δ13C and δ18O
    Huang, L.
    Chivulescu, A.
    Ernst, D.
    Zhang, W.
    Norman, A. -L.
    Lee, Y. -S.
    ATMOSPHERIC MEASUREMENT TECHNIQUES, 2013, 6 (07) : 1685 - 1705
  • [49] High-resolution Fourier-transform spectroscopy and deperturbation analysis of the A1Π(ν=1) level in 12C18O
    Malicka, M., I
    Ryzner, S.
    Heays, A. N.
    de Oliveira, N.
    Field, R. W.
    Ubachs, W.
    Hakalla, R.
    JOURNAL OF QUANTITATIVE SPECTROSCOPY & RADIATIVE TRANSFER, 2020, 255
  • [50] CO2 degassing at La Solfatara volcano (Phlegrean Fields): Processes affecting δ13C and δ18O of soil CO2
    Federico, Cinzia
    Corso, Pietro Paolo
    Fiordilino, Emilio
    Cardellini, Carlo
    Chiodini, G.
    Parello, F.
    Pisciotta, A.
    GEOCHIMICA ET COSMOCHIMICA ACTA, 2010, 74 (12) : 3521 - 3538