Line broadening of SO2 and CO2 volcanic activity gases in the Earth’s atmosphere

Calculations of the CO2-broadening coefficients of sulfur oxide lines by the semi-empirical method [Mol. Phys. 102 (2004) 1653] and averaged energy difference method [Atmosph. Ocean. Optics 28 (2015) 403] are presented. In this work, 41 lines are considered, the rotational quantum number J varies fr...

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Main Authors: Dudaryonok Anna S., Lavrentieva Nina N., Lavrentiev Nikolai A.
Format: Article
Language:English
Published: EDP Sciences 2018-01-01
Series:E3S Web of Conferences
Online Access:https://doi.org/10.1051/e3sconf/20186202010
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spelling doaj-8fc7308fa5d24034aefdd75570955aa22021-02-02T02:55:40ZengEDP SciencesE3S Web of Conferences2267-12422018-01-01620201010.1051/e3sconf/20186202010e3sconf_strpep2018_02010Line broadening of SO2 and CO2 volcanic activity gases in the Earth’s atmosphereDudaryonok Anna S.Lavrentieva Nina N.Lavrentiev Nikolai A.Calculations of the CO2-broadening coefficients of sulfur oxide lines by the semi-empirical method [Mol. Phys. 102 (2004) 1653] and averaged energy difference method [Atmosph. Ocean. Optics 28 (2015) 403] are presented. In this work, 41 lines are considered, the rotational quantum number J varies from 14 to 51. Calculations of the line widths are carried out for room temperature (296 K), and also for the temperature range typical for the Ears atmosphere. There is good agreement with the literature data. The carbon dioxide lines broadening coefficients induced by nitrogen, nitrogen oxide, carbon monoxide and carbon dioxide at room temperature (T = 296 K) are obtained for a wide range of the rotational quantum number J (up to 100). The temperature exponents are calculated for every line widths. The calculations were performed by a semi-empirical method, based on the semiclassical impact theory of line broadening and modified by introducing additional correction factor whose parameters can be determined by fitting the broadening or shifting coefficients to the experimental data.https://doi.org/10.1051/e3sconf/20186202010
collection DOAJ
language English
format Article
sources DOAJ
author Dudaryonok Anna S.
Lavrentieva Nina N.
Lavrentiev Nikolai A.
spellingShingle Dudaryonok Anna S.
Lavrentieva Nina N.
Lavrentiev Nikolai A.
Line broadening of SO2 and CO2 volcanic activity gases in the Earth’s atmosphere
E3S Web of Conferences
author_facet Dudaryonok Anna S.
Lavrentieva Nina N.
Lavrentiev Nikolai A.
author_sort Dudaryonok Anna S.
title Line broadening of SO2 and CO2 volcanic activity gases in the Earth’s atmosphere
title_short Line broadening of SO2 and CO2 volcanic activity gases in the Earth’s atmosphere
title_full Line broadening of SO2 and CO2 volcanic activity gases in the Earth’s atmosphere
title_fullStr Line broadening of SO2 and CO2 volcanic activity gases in the Earth’s atmosphere
title_full_unstemmed Line broadening of SO2 and CO2 volcanic activity gases in the Earth’s atmosphere
title_sort line broadening of so2 and co2 volcanic activity gases in the earth’s atmosphere
publisher EDP Sciences
series E3S Web of Conferences
issn 2267-1242
publishDate 2018-01-01
description Calculations of the CO2-broadening coefficients of sulfur oxide lines by the semi-empirical method [Mol. Phys. 102 (2004) 1653] and averaged energy difference method [Atmosph. Ocean. Optics 28 (2015) 403] are presented. In this work, 41 lines are considered, the rotational quantum number J varies from 14 to 51. Calculations of the line widths are carried out for room temperature (296 K), and also for the temperature range typical for the Ears atmosphere. There is good agreement with the literature data. The carbon dioxide lines broadening coefficients induced by nitrogen, nitrogen oxide, carbon monoxide and carbon dioxide at room temperature (T = 296 K) are obtained for a wide range of the rotational quantum number J (up to 100). The temperature exponents are calculated for every line widths. The calculations were performed by a semi-empirical method, based on the semiclassical impact theory of line broadening and modified by introducing additional correction factor whose parameters can be determined by fitting the broadening or shifting coefficients to the experimental data.
url https://doi.org/10.1051/e3sconf/20186202010
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