DOAS for flue gas monitoring—I. Temperature effects in the U.V./visible absorption spectra of NO, NO2, SO2 and NH3

The temperature dependence of the absolute and the differential absorption cross-sections for NO, SO2, NO2 and NH3 were studied by recordings of spectra in a heat-pipe cell and by simulations of theoretical spectra for NO. A review and comparison of the present results with other relevant works were also made. The experimental results showed that the differential absorption features for some of the studied species change dramatically with temperature. For SO2 and NO2 the quantitative change in differential structure was very large with a relative change in magnitude of 70% between 300 and 700 K. For the two other species studied, NO and NH3, the change in magnitude of the differential structure was only 15–20%, over the same temperature range. Simulations for NO showed that the temperature effect was strongly dependent on the spectral resolution of the instrument and that it became smaller at lower resolution. The qualitative change in the spectral features was a continuous lowering of absorbance peaks and an increase in valleys which made the band integral of the absorbance quite insensitive to the temperature. Hot bands also appeared for SO2 and NH3 around 220 nm. The temperature affected the spectral features more in a quantitative than in a qualitative manner.

[1]  A. Ladstätter-Weißenmayer,et al.  Simultaneous determination of NH3, SO2, NO and NO2 by direct UV-absorption in ambient air , 1991 .

[2]  G. Herzberg,et al.  Molecular spectra and molecular structure. Vol.3: Electronic spectra and electronic structure of polyatomic molecules , 1966 .

[3]  G. Herzberg,et al.  Constants of diatomic molecules , 1979 .

[4]  H Edner,et al.  Differential optical absorption spectroscopy system used for atmospheric mercury monitoring. , 1986, Applied optics.

[5]  Florence Goutail,et al.  O3 and NO2 ground‐based measurements by visible spectrometry during Arctic winter and spring 1988 , 1988 .

[6]  S. Madronich,et al.  Visible‐ultraviolet absorption cross sections for NO2 as a function of temperature , 1988 .

[7]  J. Kerr,et al.  Nitrogen Dioxide Concentrations in the Atmosphere , 1973, Nature.

[8]  E. David Hinkley,et al.  Laser monitoring of the atmosphere , 1976 .

[9]  T. Klüpfel,et al.  Ground‐based UV‐VIS spectroscopy: Diurnal OCIO‐profiles during January 1990 above Søndre Strømfjord, Greenland , 1991 .

[10]  W. Harshbarger Franck–Condon Factors for the Ã←X̃ Transition of Ammonia with Anharmonic Potential Functions for the Ground and Excited States , 1970 .

[11]  V. Vaida,et al.  The direct ultraviolet absorption spectrum of the A'~A2" .rarw. ~X'A1 transition of jet-cooled ammonia , 1984 .

[12]  Stanley C. Solomon,et al.  Visible spectroscopy at McMurdo Station, Antarctica: 2. Observations of OClO , 1987 .

[13]  U. Platt,et al.  Simultaneous measurement of atmospheric CH2O, O3, and NO2 by differential optical absorption , 1979 .

[14]  L. Ziegler Rovibronic absorption analysis of the à ← X̃ transition of ammonia , 1985 .

[15]  P. R. Bevington,et al.  Data Reduction and Error Analysis for the Physical Sciences , 1969 .

[16]  F. Goutail,et al.  Identification of polar stratospheric clouds from the ground by visible spectrometry , 1991 .

[17]  R. Kullmer,et al.  Vibronic coupling in SO2, and its influence on the rotational structure of the bands in the 300—330 nm region , 1985 .

[18]  K. Yoshino,et al.  HIGH RESOLUTION ABSORPTION CROSS SECTION MEASUREMENTS OF $SO_{2}$ AT 213 K IN THE WAVELENGTH REGION 172-240 nm , 1984 .

[19]  J. Joens,et al.  SO2 absorption cross‐section measurements from 197 nm to 240 nm , 1992 .

[20]  H. Okabe Fluorescence and predissociation of sulfur dioxide , 1971 .