Solubility of Small AgI Particles in NaI and KI Solutions: Significance to Cloud SeedingSource: Journal of Applied Meteorology:;1972:;volume( 011 ):;issue: 002::page 366Author:Davis, Briant L.
DOI: 10.1175/1520-0450(1972)011<0366:SOSAPI>2.0.CO;2Publisher: American Meteorological Society
Abstract: Utilizing standard solubility data in the literature it is seen that for 2:1 mole ratio AgI:NaI (or KI) aerosol compositions only AgI particles <0.01 ? radius are in danger of complete dissolution into hygroscopically derived solution envelopes containing NaI, or KI. This condition develops only momentarily when sufficient water vapor has accreted to form a saturated solution about the AgI particle. Taking a typical AgI-NaI aerosol such as that studied by Mossop and Tuck-Lee as representative of generated aerosols, only a small part of the AgI can be dissolved under the most favorable atmospheric conditions; particles representing the median size for this aerosol, of 0.042 ? radius, will lose only 35 weight percent of the AgI present. Very similar relations hold for KI-bearing aerosols.
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contributor author | Davis, Briant L. | |
date accessioned | 2017-06-09T17:19:59Z | |
date available | 2017-06-09T17:19:59Z | |
date copyright | 1972/03/01 | |
date issued | 1972 | |
identifier issn | 0021-8952 | |
identifier other | ams-8334.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4226556 | |
description abstract | Utilizing standard solubility data in the literature it is seen that for 2:1 mole ratio AgI:NaI (or KI) aerosol compositions only AgI particles <0.01 ? radius are in danger of complete dissolution into hygroscopically derived solution envelopes containing NaI, or KI. This condition develops only momentarily when sufficient water vapor has accreted to form a saturated solution about the AgI particle. Taking a typical AgI-NaI aerosol such as that studied by Mossop and Tuck-Lee as representative of generated aerosols, only a small part of the AgI can be dissolved under the most favorable atmospheric conditions; particles representing the median size for this aerosol, of 0.042 ? radius, will lose only 35 weight percent of the AgI present. Very similar relations hold for KI-bearing aerosols. | |
publisher | American Meteorological Society | |
title | Solubility of Small AgI Particles in NaI and KI Solutions: Significance to Cloud Seeding | |
type | Journal Paper | |
journal volume | 11 | |
journal issue | 2 | |
journal title | Journal of Applied Meteorology | |
identifier doi | 10.1175/1520-0450(1972)011<0366:SOSAPI>2.0.CO;2 | |
journal fristpage | 366 | |
journal lastpage | 369 | |
tree | Journal of Applied Meteorology:;1972:;volume( 011 ):;issue: 002 | |
contenttype | Fulltext |