Charged Dislocation in Ice. II. Contribution of Dielectric Relaxation
The contribution of electrically charged dislocation motion to dielectric relaxation was studied theoretically. Experimentally obtained data on charge density, dislocation density, and segment length and distribution described in Part I of this series were used to calculate dielectric relaxation spe...
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ftdtic:ADA113936 2023-05-15T16:37:05+02:00 Charged Dislocation in Ice. II. Contribution of Dielectric Relaxation Itagaki,Kazuhiko COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER NH 1982-03 text/html http://www.dtic.mil/docs/citations/ADA113936 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA113936 en eng http://www.dtic.mil/docs/citations/ADA113936 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Snow Ice and Permafrost Solid State Physics *Ice *Dislocations Electric charge Motion Dielectric properties Relaxation Spectra Audio frequency Polarization Charge density *Dielectric relaxation PE61102A AST24 WU002 Text 1982 ftdtic 2016-02-19T07:55:43Z The contribution of electrically charged dislocation motion to dielectric relaxation was studied theoretically. Experimentally obtained data on charge density, dislocation density, and segment length and distribution described in Part I of this series were used to calculate dielectric relaxation spectra. The results indicate that the charged dislocation process can produce the observed audio frequency dielectric relaxation as well as the distribution of spectra. (Author) See also AD-A078 775. Text Ice permafrost Defense Technical Information Center: DTIC Technical Reports database |
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Open Polar |
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Defense Technical Information Center: DTIC Technical Reports database |
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ftdtic |
language |
English |
topic |
Snow Ice and Permafrost Solid State Physics *Ice *Dislocations Electric charge Motion Dielectric properties Relaxation Spectra Audio frequency Polarization Charge density *Dielectric relaxation PE61102A AST24 WU002 |
spellingShingle |
Snow Ice and Permafrost Solid State Physics *Ice *Dislocations Electric charge Motion Dielectric properties Relaxation Spectra Audio frequency Polarization Charge density *Dielectric relaxation PE61102A AST24 WU002 Itagaki,Kazuhiko Charged Dislocation in Ice. II. Contribution of Dielectric Relaxation |
topic_facet |
Snow Ice and Permafrost Solid State Physics *Ice *Dislocations Electric charge Motion Dielectric properties Relaxation Spectra Audio frequency Polarization Charge density *Dielectric relaxation PE61102A AST24 WU002 |
description |
The contribution of electrically charged dislocation motion to dielectric relaxation was studied theoretically. Experimentally obtained data on charge density, dislocation density, and segment length and distribution described in Part I of this series were used to calculate dielectric relaxation spectra. The results indicate that the charged dislocation process can produce the observed audio frequency dielectric relaxation as well as the distribution of spectra. (Author) See also AD-A078 775. |
author2 |
COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER NH |
format |
Text |
author |
Itagaki,Kazuhiko |
author_facet |
Itagaki,Kazuhiko |
author_sort |
Itagaki,Kazuhiko |
title |
Charged Dislocation in Ice. II. Contribution of Dielectric Relaxation |
title_short |
Charged Dislocation in Ice. II. Contribution of Dielectric Relaxation |
title_full |
Charged Dislocation in Ice. II. Contribution of Dielectric Relaxation |
title_fullStr |
Charged Dislocation in Ice. II. Contribution of Dielectric Relaxation |
title_full_unstemmed |
Charged Dislocation in Ice. II. Contribution of Dielectric Relaxation |
title_sort |
charged dislocation in ice. ii. contribution of dielectric relaxation |
publishDate |
1982 |
url |
http://www.dtic.mil/docs/citations/ADA113936 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA113936 |
genre |
Ice permafrost |
genre_facet |
Ice permafrost |
op_source |
DTIC AND NTIS |
op_relation |
http://www.dtic.mil/docs/citations/ADA113936 |
op_rights |
APPROVED FOR PUBLIC RELEASE |
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1766027384103895040 |