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Titlebook: Atmospheric Aerosols and Nucleation; Proceedings of the T Paul E. Wagner,Gabor Vali Conference proceedings 1988 Springer-Verlag Berlin Heid

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Time-size structure of atmospheric aerosol,cal aerosol spectrometer. The role of photo-chemical processes in the generation of particles is discussed. Estimates of the stability of size-fractions of particles and characteristic times of particle transformation from one fraction to another have been obtained by correlation analysis.
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https://doi.org/10.1007/3-540-50108-8atmosphere; chemistry; environment; environmental science; environmental sciences; phase transition; air p
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978-3-662-15925-5Springer-Verlag Berlin Heidelberg 1988
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https://doi.org/10.1007/978-3-8274-2299-6cient to remove appreciable amount of trace gases from the atmosphere through gas-to-particle conversion. In this article, we rapidly review the present state of the theory and we compare some experimental results to the theoretical predictions. Some possible atmospheric applications are discussed.
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Mehak Kaur,Hishita Peshwani,Mayurika Goelcal aerosol spectrometer. The role of photo-chemical processes in the generation of particles is discussed. Estimates of the stability of size-fractions of particles and characteristic times of particle transformation from one fraction to another have been obtained by correlation analysis.
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Mehak Kaur,Hishita Peshwani,Mayurika Goelhysics and liquid phase chemical reactions. The calculations are based on size-segregated measurements of the chemical composition of aerosol particles. The results show: The sulfate mass fraction of the activated particles increases rapidly because the water volume, in which the sulfate production
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Mehak Kaur,Hishita Peshwani,Mayurika Goelcal aerosol spectrometer. The role of photo-chemical processes in the generation of particles is discussed. Estimates of the stability of size-fractions of particles and characteristic times of particle transformation from one fraction to another have been obtained by correlation analysis.
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