1998
DOI: 10.1016/s1386-1425(97)00214-x
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The ozone molecule: infrared and microwave spectroscopy

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Cited by 116 publications
(81 citation statements)
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“…The progress in the spectroscopic characterization of the molecule, and the impact of these studies on the understanding of its photochemistry, were reviewed by Steinfeld et al (1), Flaud et al (2,3), and Bacis et al (4). There have been many determinations of the ground state potential energy function of ozone from experimental data (5)(6)(7)(8).…”
Section: Introductionmentioning
confidence: 99%
“…The progress in the spectroscopic characterization of the molecule, and the impact of these studies on the understanding of its photochemistry, were reviewed by Steinfeld et al (1), Flaud et al (2,3), and Bacis et al (4). There have been many determinations of the ground state potential energy function of ozone from experimental data (5)(6)(7)(8).…”
Section: Introductionmentioning
confidence: 99%
“…In this region appear the ν 3 and ν 4 bands of various nitric acid isotopes. We made a rough estimation of a pressure for HNO 3 , leading to a value lower than 10 −3 Torr. The assignments of HNO 3 lines have been made using a set of other spectra, not given in Table 1, recorded for the analysis of the other different mixtures of isotopic O 3 : the two different spectra shown in Fig.…”
Section: (A) (020) Statementioning
confidence: 99%
“…With respect to these studies, 18 O 3 is spectroscopically of interest: new experimental data can serve to study isotopic effects in spectroscopy properties and in the dynamics of nuclear motion of the ozone molecule and to validate recent theoretical predictions from potential functions (5). References for mono-or bisubstituted 17 O or 18 O ozone may be found in (3). The spectrum of 18 O 3 has been analyzed by the microwave technique (8), leading to a set of rotational constants for the ground vibrational state (000), and by the high-resolution infrared technique for ν 2 (9), ν 1 and ν 3 (10), and ν 1 + ν 3 (11); 11 additional band centers up to 4000 cm −1 were derived by low-resolution studies (12).…”
Section: Introductionmentioning
confidence: 99%
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“…Also, modeling of the role of ozone in the lower ionosphere requires direct and dissociative ionization by photons or electrons to be taken into account, and modeling of ozone in the stratosphere requires its ionization energy and electron affinity. Reliable values for the first ionization energy of O 3 and dissociation energies of O 3 and O 3 ϩ are central to such studies. From a spectroscopic point of view, O 3 ϩ is of interest as an isoelectronic species to NO 2 , which has been studied intensively experimentally as well as theoretically ͑see, e.g., Refs.…”
Section: Introductionmentioning
confidence: 99%