Ice nucleation efficiency of AgI: review and new insights

AgI is one of the best-investigated ice-nucleating substances. It has relevance for the atmosphere since it is used for glaciogenic cloud seeding. Theoretical and experimental studies over the last 60 years provide a complex picture of silver iodide as an ice-nucleating agent with conflicting and...

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Main Authors: C. Marcolli, B. Nagare, A. Welti, U. Lohmann
Format: Article
Language:English
Published: Copernicus Publications 2016-07-01
Series:Atmospheric Chemistry and Physics
Online Access:https://www.atmos-chem-phys.net/16/8915/2016/acp-16-8915-2016.pdf
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author C. Marcolli
C. Marcolli
B. Nagare
A. Welti
A. Welti
U. Lohmann
author_facet C. Marcolli
C. Marcolli
B. Nagare
A. Welti
A. Welti
U. Lohmann
author_sort C. Marcolli
collection DOAJ
description AgI is one of the best-investigated ice-nucleating substances. It has relevance for the atmosphere since it is used for glaciogenic cloud seeding. Theoretical and experimental studies over the last 60 years provide a complex picture of silver iodide as an ice-nucleating agent with conflicting and inconsistent results. This review compares experimental ice nucleation studies in order to analyze the factors that influence the ice nucleation ability of AgI. The following picture emerges from this analysis: the ice nucleation ability of AgI seems to be enhanced when the AgI particle is on the surface of a droplet, which is indeed the position that a particle takes when it can freely move in a droplet. The ice nucleation by particles with surfaces exposed to air depends on water adsorption. AgI surfaces seem to be most efficient at nucleating ice when they are exposed to relative humidity at or even above water saturation. For AgI particles that are completely immersed in water, the freezing temperature increases with increasing AgI surface area. Higher threshold freezing temperatures seem to correlate with improved lattice matches as can be seen for AgI–AgCl solid solutions and 3AgI&middot;NH<sub>4</sub>I&middot;6H<sub>2</sub>O, which have slightly better lattice matches with ice than AgI and also higher threshold freezing temperatures. However, the effect of a good lattice match is annihilated when the surfaces have charges. Also, the ice nucleation ability seems to decrease during dissolution of AgI particles. This introduces an additional history and time dependence for ice nucleation in cloud chambers with short residence times.
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spelling doaj.art-793a893089454bbb890bdee1e25403a32022-12-22T02:55:52ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242016-07-01168915893710.5194/acp-16-8915-2016Ice nucleation efficiency of AgI: review and new insightsC. Marcolli0C. Marcolli1B. Nagare2A. Welti3A. Welti4U. Lohmann5Institute for Atmospheric and Climate Science, ETH Zurich, Zurich, SwitzerlandMarcolli Chemistry and Physics Consulting GmbH, Zurich, SwitzerlandInstitute for Atmospheric and Climate Science, ETH Zurich, Zurich, SwitzerlandInstitute for Atmospheric and Climate Science, ETH Zurich, Zurich, SwitzerlandLeibniz Institute for Tropospheric Research (TROPOS), Leipzig, GermanyInstitute for Atmospheric and Climate Science, ETH Zurich, Zurich, SwitzerlandAgI is one of the best-investigated ice-nucleating substances. It has relevance for the atmosphere since it is used for glaciogenic cloud seeding. Theoretical and experimental studies over the last 60 years provide a complex picture of silver iodide as an ice-nucleating agent with conflicting and inconsistent results. This review compares experimental ice nucleation studies in order to analyze the factors that influence the ice nucleation ability of AgI. The following picture emerges from this analysis: the ice nucleation ability of AgI seems to be enhanced when the AgI particle is on the surface of a droplet, which is indeed the position that a particle takes when it can freely move in a droplet. The ice nucleation by particles with surfaces exposed to air depends on water adsorption. AgI surfaces seem to be most efficient at nucleating ice when they are exposed to relative humidity at or even above water saturation. For AgI particles that are completely immersed in water, the freezing temperature increases with increasing AgI surface area. Higher threshold freezing temperatures seem to correlate with improved lattice matches as can be seen for AgI–AgCl solid solutions and 3AgI&middot;NH<sub>4</sub>I&middot;6H<sub>2</sub>O, which have slightly better lattice matches with ice than AgI and also higher threshold freezing temperatures. However, the effect of a good lattice match is annihilated when the surfaces have charges. Also, the ice nucleation ability seems to decrease during dissolution of AgI particles. This introduces an additional history and time dependence for ice nucleation in cloud chambers with short residence times.https://www.atmos-chem-phys.net/16/8915/2016/acp-16-8915-2016.pdf
spellingShingle C. Marcolli
C. Marcolli
B. Nagare
A. Welti
A. Welti
U. Lohmann
Ice nucleation efficiency of AgI: review and new insights
Atmospheric Chemistry and Physics
title Ice nucleation efficiency of AgI: review and new insights
title_full Ice nucleation efficiency of AgI: review and new insights
title_fullStr Ice nucleation efficiency of AgI: review and new insights
title_full_unstemmed Ice nucleation efficiency of AgI: review and new insights
title_short Ice nucleation efficiency of AgI: review and new insights
title_sort ice nucleation efficiency of agi review and new insights
url https://www.atmos-chem-phys.net/16/8915/2016/acp-16-8915-2016.pdf
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