A Study of the Mechanism of Contact Ice NucleationSource: Journal of the Atmospheric Sciences:;1975:;Volume( 032 ):;issue: 008::page 1597Author:Fukuta, Norihiko
DOI: 10.1175/1520-0469(1975)032<1597:ASOTMO>2.0.CO;2Publisher: American Meteorological Society
Abstract: The nucleation of freezing of supercooled water drops by metaldehyde, phloroglucinol and 1,5?dihydroxynaphthalene was studied. It was found that the threshold temperature for nucleation by contact of the particles with the supercooled drops was 2?3°C warmer than the threshold when the same drops were melted and re?frozen with the nuclei already partly immersed. There was no evidence that the high threshold for contact nucleation was due to active sites that were subsequently destroyed. Rather, it was thought to be associated with the movement of the water front along the surface of the nucleus during the contact process. It is suggested that this process gives rise to a transient high free energy zone which facilitates nucleation. In support of this theory, measurements were made of the contact angles of water on the three compounds.
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| contributor author | Fukuta, Norihiko | |
| date accessioned | 2017-06-09T14:18:23Z | |
| date available | 2017-06-09T14:18:23Z | |
| date copyright | 1975/08/01 | |
| date issued | 1975 | |
| identifier issn | 0022-4928 | |
| identifier other | ams-16888.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4152720 | |
| description abstract | The nucleation of freezing of supercooled water drops by metaldehyde, phloroglucinol and 1,5?dihydroxynaphthalene was studied. It was found that the threshold temperature for nucleation by contact of the particles with the supercooled drops was 2?3°C warmer than the threshold when the same drops were melted and re?frozen with the nuclei already partly immersed. There was no evidence that the high threshold for contact nucleation was due to active sites that were subsequently destroyed. Rather, it was thought to be associated with the movement of the water front along the surface of the nucleus during the contact process. It is suggested that this process gives rise to a transient high free energy zone which facilitates nucleation. In support of this theory, measurements were made of the contact angles of water on the three compounds. | |
| publisher | American Meteorological Society | |
| title | A Study of the Mechanism of Contact Ice Nucleation | |
| type | Journal Paper | |
| journal volume | 32 | |
| journal issue | 8 | |
| journal title | Journal of the Atmospheric Sciences | |
| identifier doi | 10.1175/1520-0469(1975)032<1597:ASOTMO>2.0.CO;2 | |
| journal fristpage | 1597 | |
| journal lastpage | 1603 | |
| tree | Journal of the Atmospheric Sciences:;1975:;Volume( 032 ):;issue: 008 | |
| contenttype | Fulltext |