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- W85194635 abstract "Publisher Summary Two major components of the atmospheric aerosol are NH4NO3 and (NH4)2SO4. Usually NH4NO3, as a quite volatile component, is enriched in the larger particles. Therefore, the interesting question arises if a particle system with a just opposite distribution of the two components is stable or if redistribution will take place. Two mechanisms for the redistribution compete with each other: coagulation and evaporation with subsequent condensation. Of course, the last process is important only for volatile materials, such as NH4NO 3 or some organic compounds. To quantify the amount of material redistributed by each of the two processes, laboratory experiments were carried out using a system with one nonvolatile and for comparison a second system with two nonvolatile components. At the same time, calculations with the computer model NACHE were performed to analyze the process in more detail and to recalculate the experiments. Because the particle size distributions generated experimentally overlap to some extent, some additional modeling investigations were carried out based on two very narrow and not overlapping size distributions. These calculations can help understand the extent to which and the conditions under which the process that is responsible for the redistribution." @default.
- W85194635 created "2016-06-24" @default.
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- W85194635 date "1996-01-01" @default.
- W85194635 modified "2023-09-26" @default.
- W85194635 title "Redistribution mechanisms for volatile and non-volatile components of atmospheric aerosol particles" @default.
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- W85194635 doi "https://doi.org/10.1016/b978-008042030-1/50112-8" @default.
- W85194635 hasPublicationYear "1996" @default.
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