Changing shapes and implied viscosities of suspended submicron particles

The change in shape of atmospherically relevant organic particles is used to estimate the viscosity of the particle material without the need for removal from aerosol suspension. The dynamic shape factors χ of particles produced by α-pinene ozonolysis in a flow tube reactor, under conditions of part...

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Main Authors: Y. Zhang, M. S. Sanchez, C. Douet, Y. Wang, A. P. Bateman, Z. Gong, M. Kuwata, L. Renbaum-Wolff, B. B. Sato, P. F. Liu, A. K. Bertram, F. M. Geiger, S. T. Martin
Format: Article
Language:English
Published: Copernicus Publications 2015-07-01
Series:Atmospheric Chemistry and Physics
Online Access:http://www.atmos-chem-phys.net/15/7819/2015/acp-15-7819-2015.pdf
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author Y. Zhang
M. S. Sanchez
C. Douet
Y. Wang
A. P. Bateman
Z. Gong
M. Kuwata
L. Renbaum-Wolff
B. B. Sato
P. F. Liu
A. K. Bertram
F. M. Geiger
S. T. Martin
author_facet Y. Zhang
M. S. Sanchez
C. Douet
Y. Wang
A. P. Bateman
Z. Gong
M. Kuwata
L. Renbaum-Wolff
B. B. Sato
P. F. Liu
A. K. Bertram
F. M. Geiger
S. T. Martin
author_sort Y. Zhang
collection DOAJ
description The change in shape of atmospherically relevant organic particles is used to estimate the viscosity of the particle material without the need for removal from aerosol suspension. The dynamic shape factors χ of particles produced by α-pinene ozonolysis in a flow tube reactor, under conditions of particle coagulation, were measured while altering the relative humidity (RH) downstream of the flow tube. As relative humidity was increased, the results showed that χ could change from 1.27 to 1.02, corresponding to a transition from aspherical to nearly spherical shapes. The shape change could occur at elevated RH because the organic material had decreased viscosity and was therefore able to flow to form spherical shapes, as favored by the minimization of surface area. Numerical modeling was used to estimate the particle viscosity associated with this flow. Based on particle diameter and RH exposure time, the viscosity dropped from 10<sup>(8.7±2.0)</sup> to 10<sup>(7.0±2.0)</sup> Pa s (two sigma) for an increase in RH from < 5 to 58 % at 293 K. These results imply that the equilibration of the chemical composition of the particle phase with the gas phase can shift from hours at mid-range RH to days at low RH.
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spelling doaj.art-9d404471d52f4319beedb11e28f230fe2022-12-22T03:31:51ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242015-07-0115147819782910.5194/acp-15-7819-2015Changing shapes and implied viscosities of suspended submicron particlesY. Zhang0M. S. Sanchez1C. Douet2Y. Wang3A. P. Bateman4Z. Gong5M. Kuwata6L. Renbaum-Wolff7B. B. Sato8P. F. Liu9A. K. Bertram10F. M. Geiger11S. T. Martin12School of Engineering and Applied Sciences, Harvard University, Cambridge, Massachusetts, USASchool of Engineering and Applied Sciences, Harvard University, Cambridge, Massachusetts, USASchool of Engineering and Applied Sciences, Harvard University, Cambridge, Massachusetts, USASchool of Engineering and Applied Sciences, Harvard University, Cambridge, Massachusetts, USASchool of Engineering and Applied Sciences, Harvard University, Cambridge, Massachusetts, USASchool of Engineering and Applied Sciences, Harvard University, Cambridge, Massachusetts, USASchool of Engineering and Applied Sciences, Harvard University, Cambridge, Massachusetts, USADepartment of Chemistry, University of British Columbia, Vancouver, British Columbia, CanadaSchool of Engineering and Applied Sciences, Harvard University, Cambridge, Massachusetts, USASchool of Engineering and Applied Sciences, Harvard University, Cambridge, Massachusetts, USADepartment of Chemistry, University of British Columbia, Vancouver, British Columbia, CanadaDepartment of Chemistry, Northwestern University, Evanston, Illinois, USASchool of Engineering and Applied Sciences, Harvard University, Cambridge, Massachusetts, USAThe change in shape of atmospherically relevant organic particles is used to estimate the viscosity of the particle material without the need for removal from aerosol suspension. The dynamic shape factors χ of particles produced by α-pinene ozonolysis in a flow tube reactor, under conditions of particle coagulation, were measured while altering the relative humidity (RH) downstream of the flow tube. As relative humidity was increased, the results showed that χ could change from 1.27 to 1.02, corresponding to a transition from aspherical to nearly spherical shapes. The shape change could occur at elevated RH because the organic material had decreased viscosity and was therefore able to flow to form spherical shapes, as favored by the minimization of surface area. Numerical modeling was used to estimate the particle viscosity associated with this flow. Based on particle diameter and RH exposure time, the viscosity dropped from 10<sup>(8.7±2.0)</sup> to 10<sup>(7.0±2.0)</sup> Pa s (two sigma) for an increase in RH from < 5 to 58 % at 293 K. These results imply that the equilibration of the chemical composition of the particle phase with the gas phase can shift from hours at mid-range RH to days at low RH.http://www.atmos-chem-phys.net/15/7819/2015/acp-15-7819-2015.pdf
spellingShingle Y. Zhang
M. S. Sanchez
C. Douet
Y. Wang
A. P. Bateman
Z. Gong
M. Kuwata
L. Renbaum-Wolff
B. B. Sato
P. F. Liu
A. K. Bertram
F. M. Geiger
S. T. Martin
Changing shapes and implied viscosities of suspended submicron particles
Atmospheric Chemistry and Physics
title Changing shapes and implied viscosities of suspended submicron particles
title_full Changing shapes and implied viscosities of suspended submicron particles
title_fullStr Changing shapes and implied viscosities of suspended submicron particles
title_full_unstemmed Changing shapes and implied viscosities of suspended submicron particles
title_short Changing shapes and implied viscosities of suspended submicron particles
title_sort changing shapes and implied viscosities of suspended submicron particles
url http://www.atmos-chem-phys.net/15/7819/2015/acp-15-7819-2015.pdf
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