Deposition nucleation on mineral dust particles: a case against classical nucleation theory with the assumption of a single contact angle

Deposition nucleation on two mineral species, kaolinite and illite, was studied using a flow cell coupled to an optical microscope. The results show that the <i>S</i><sub>ice</sub> conditions when ice first nucleated, defined as the onset &...

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Main Authors: M. J. Wheeler, A. K. Bertram
Format: Article
Language:English
Published: Copernicus Publications 2012-01-01
Series:Atmospheric Chemistry and Physics
Online Access:http://www.atmos-chem-phys.net/12/1189/2012/acp-12-1189-2012.pdf
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author M. J. Wheeler
A. K. Bertram
author_facet M. J. Wheeler
A. K. Bertram
author_sort M. J. Wheeler
collection DOAJ
description Deposition nucleation on two mineral species, kaolinite and illite, was studied using a flow cell coupled to an optical microscope. The results show that the <i>S</i><sub>ice</sub> conditions when ice first nucleated, defined as the onset <i>S</i><sub>ice</sub> (<i>S</i><sub>ice,onset</sub>), is a strong function of the surface area available for nucleation, varying from 100% to 125% at temperatures between 242 and 239 K. The surface area dependent data could not be described accurately using classical nucleation theory and the assumption of a single contact angle (defined here as the single-α model). These results suggest that caution should be applied when using contact angles determined from <i>S</i><sub>ice,onset</sub> data and the single-α model. In contrast to the single-α model, the active site model, the deterministic model, and a model with a distribution of contact angles fit the data within experimental uncertainties. Parameters from the fits to the data are presented.
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spelling doaj.art-57ba9e1af84b460bafa019bd3dcd9e9e2022-12-21T17:16:07ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242012-01-011221189120110.5194/acp-12-1189-2012Deposition nucleation on mineral dust particles: a case against classical nucleation theory with the assumption of a single contact angleM. J. WheelerA. K. BertramDeposition nucleation on two mineral species, kaolinite and illite, was studied using a flow cell coupled to an optical microscope. The results show that the <i>S</i><sub>ice</sub> conditions when ice first nucleated, defined as the onset <i>S</i><sub>ice</sub> (<i>S</i><sub>ice,onset</sub>), is a strong function of the surface area available for nucleation, varying from 100% to 125% at temperatures between 242 and 239 K. The surface area dependent data could not be described accurately using classical nucleation theory and the assumption of a single contact angle (defined here as the single-α model). These results suggest that caution should be applied when using contact angles determined from <i>S</i><sub>ice,onset</sub> data and the single-α model. In contrast to the single-α model, the active site model, the deterministic model, and a model with a distribution of contact angles fit the data within experimental uncertainties. Parameters from the fits to the data are presented.http://www.atmos-chem-phys.net/12/1189/2012/acp-12-1189-2012.pdf
spellingShingle M. J. Wheeler
A. K. Bertram
Deposition nucleation on mineral dust particles: a case against classical nucleation theory with the assumption of a single contact angle
Atmospheric Chemistry and Physics
title Deposition nucleation on mineral dust particles: a case against classical nucleation theory with the assumption of a single contact angle
title_full Deposition nucleation on mineral dust particles: a case against classical nucleation theory with the assumption of a single contact angle
title_fullStr Deposition nucleation on mineral dust particles: a case against classical nucleation theory with the assumption of a single contact angle
title_full_unstemmed Deposition nucleation on mineral dust particles: a case against classical nucleation theory with the assumption of a single contact angle
title_short Deposition nucleation on mineral dust particles: a case against classical nucleation theory with the assumption of a single contact angle
title_sort deposition nucleation on mineral dust particles a case against classical nucleation theory with the assumption of a single contact angle
url http://www.atmos-chem-phys.net/12/1189/2012/acp-12-1189-2012.pdf
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