R. Schermaul, Transition probability and line broadening for the b(1)Sigma(+)(g)(v=0)<- X-3 Sigma(-)(g)(v=0) band of the (OO)-O-16-O-18 isotopomer of oxygen, J QUAN SPEC, 62(2), 1999, pp. 181-191
Citations number
22
Categorie Soggetti
Spectroscopy /Instrumentation/Analytical Sciences
Journal title
JOURNAL OF QUANTITATIVE SPECTROSCOPY & RADIATIVE TRANSFER
Spectral line parameters and the Einstein transition probability of the b(1
)Sigma(g)(+)(nu = 0) <-- X(3)Sigma(g)(-),(nu = 0) band (A band) of the (OO)
-O-16-O-18 isotopomer of molecular oxygen were determined from high-resolut
ion Fourier transform absorption spectra of pure oxygen at pressures betwee
n 80 and 1000hPa. The spectra were recorded at room temperature and 198 K,
and at absorption pathlengths between 64.75 and 144.7 m. The spectrometer r
esolution varied from 0.0069 to 0.029 cm(-1). Line positions, integrated li
ne intensities and pressure-broadening coefficients for broadening by O-16(
2), were retrieved using a least-squares line-fitting procedure. Though the
line positions remained uncalibrated, improved spectroscopic constants for
the upper state were determined ((B) over tilde(0) = 1.314031(14)cm(-1), (
D) over tilde(0), = 4.75(4) x 10(- 6) cm(-1)). The individual intensity dat
a from all spectra were combined and averaged line intensities with an accu
racy of better than 10% and pressure-broadening coefficients with errors of
less than 25% were derived for most of the lines. The broadening coefficie
nts were found to be approximately (76 +/- 4)% of the corresponding self-br
oadening coefficients of the O-16(2), isotopomer. Combining the individual
observed line intensities in an intensity analysis, the Einstein transition
probability for the A band of (OO)-O-16-O-18 was determined to be 0.079 (3
) s(-1) and is (12 +/- 4)% smaller than the corresponding value for the A b
and of the main species. (C) 1999 Elsevier Science Ltd. All rights reserved
.