2010
DOI: 10.5194/acp-10-3099-2010
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A new modeling tool for the diffusion of gases in ice or amorphous binary mixture in the polar stratosphere and the upper troposphere

Abstract: Abstract. To elaborate stratospheric ozone depletion processes, measurements of diffusion coefficients of selected gas phase molecules (i.e. HCl, CH 3 OH, HCOOH and CH 3 COOH; Katsambas et al., 1997;Kondratyev and Varotsos, 1996;Varotsos et al., 1994Varotsos et al., , 1995 in ice in the temperature range 170-195 K have been analyzed with respect to the mechanisms and rates of diffusion. It is argued that the diffusion in ice of these compounds is governed by a vacancy -mediated mechanism, i.e. H 2 O vacancies … Show more

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Cited by 34 publications
(7 citation statements)
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“…Aerosol and gases produced by biomass burning also affect each other. Taking Ozone as an example; some researches found that the impact of aerosols on photolysis alone is to increase troposphere Ozone by 0.63 Dobson units (DUs) (Varotsos and Zellner, 2010). Small particulates have direct and indirect radiative effects on the climate and can affect human health when they are inhaled, causing respiratory problems.…”
Section: Introductionmentioning
confidence: 99%
“…Aerosol and gases produced by biomass burning also affect each other. Taking Ozone as an example; some researches found that the impact of aerosols on photolysis alone is to increase troposphere Ozone by 0.63 Dobson units (DUs) (Varotsos and Zellner, 2010). Small particulates have direct and indirect radiative effects on the climate and can affect human health when they are inhaled, causing respiratory problems.…”
Section: Introductionmentioning
confidence: 99%
“…In the following years, many experimental studies were carried out using infrared laser resonant desorption (LRD) techniques to calculate diffusion coefficients in ice film [49][50][51][52][53][54][55]. The results from these studies confirmed the linear relationship between lnD and 1/T [56]. This result clearly suggests that Equation ( 8) can be used to estimate the diffusion coefficient at any temperature when the diffusion coefficient at two different temperatures is known.…”
Section: Resultsmentioning
confidence: 83%
“…This result clearly suggests that Equation ( 8) can be used to estimate the diffu coefficient at any temperature when the diffusion coefficient at two different temperat is known. Varotsos and Zellner [56] used the above studies [53,54] and found a significan sult, namely that there is a linear relationship between the natural logarithm of the exponential factor D0 and the activation energy E (i.e., lnD0 vs. E). Summarizing al above studies, it is concluded that it is possible to estimate the diffusion coefficien As has been shown, the diffusion coefficient, D, in a single diffusion mode obeys an Arrhenius-like behavior, as seen in Equation ( 8):…”
Section: Resultsmentioning
confidence: 99%
“…The MSE has a minimum value for the found optimal parameters (i.e. kinetic rate constants): results [12]. The adsorption capacity of ice was estimated to .…”
Section: Example Of Numerical Calculations and An Application For Expmentioning
confidence: 99%