Interaction of Point Defects in Ice

Abstract The interaction of point detects in ice has been neglected for a long time. Experimental data obtained from dielectric measurements on HF-doped crystals stimulated a new evaluation of the possibility of an interaction between Bjerrum defects and ions. In a previous paper it has been shown t...

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Published in:Journal of Glaciology
Main Authors: Bilgram, J. H., Gränicher, H.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1978
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000033359
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000033359
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spelling crcambridgeupr:10.1017/s0022143000033359 2024-03-03T08:46:01+00:00 Interaction of Point Defects in Ice Bilgram, J. H. Gränicher, H. 1978 http://dx.doi.org/10.1017/s0022143000033359 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000033359 en eng Cambridge University Press (CUP) Journal of Glaciology volume 21, issue 85, page 115-122 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1978 crcambridgeupr https://doi.org/10.1017/s0022143000033359 2024-02-08T08:34:04Z Abstract The interaction of point detects in ice has been neglected for a long time. Experimental data obtained from dielectric measurements on HF-doped crystals stimulated a new evaluation of the possibility of an interaction between Bjerrum defects and ions. In a previous paper it has been shown that this leads us to assume the existence of aggregates of Bjerrum defects and ions. In this paper these aggregates and Bjerrum defects are used to explain the dielectric properties of ice, especially the temperature dependence of the product of the high and low frequency conductivity σ 0 σ ∞ . The interaction of Bjerrum defects and impurity molecules leads to a dependence of the concentration of frenkel pairs on Bjerrum-defect concentration. At HF concentrations above the native Bjerrum-defect concentration the formation of a Frenkel pair is enhanced. This leads to the fast out-diffusion which has been studied in highly doped crystals by means of NMR techniques. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 21 85 115 122
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Bilgram, J. H.
Gränicher, H.
Interaction of Point Defects in Ice
topic_facet Earth-Surface Processes
description Abstract The interaction of point detects in ice has been neglected for a long time. Experimental data obtained from dielectric measurements on HF-doped crystals stimulated a new evaluation of the possibility of an interaction between Bjerrum defects and ions. In a previous paper it has been shown that this leads us to assume the existence of aggregates of Bjerrum defects and ions. In this paper these aggregates and Bjerrum defects are used to explain the dielectric properties of ice, especially the temperature dependence of the product of the high and low frequency conductivity σ 0 σ ∞ . The interaction of Bjerrum defects and impurity molecules leads to a dependence of the concentration of frenkel pairs on Bjerrum-defect concentration. At HF concentrations above the native Bjerrum-defect concentration the formation of a Frenkel pair is enhanced. This leads to the fast out-diffusion which has been studied in highly doped crystals by means of NMR techniques.
format Article in Journal/Newspaper
author Bilgram, J. H.
Gränicher, H.
author_facet Bilgram, J. H.
Gränicher, H.
author_sort Bilgram, J. H.
title Interaction of Point Defects in Ice
title_short Interaction of Point Defects in Ice
title_full Interaction of Point Defects in Ice
title_fullStr Interaction of Point Defects in Ice
title_full_unstemmed Interaction of Point Defects in Ice
title_sort interaction of point defects in ice
publisher Cambridge University Press (CUP)
publishDate 1978
url http://dx.doi.org/10.1017/s0022143000033359
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000033359
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology
volume 21, issue 85, page 115-122
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000033359
container_title Journal of Glaciology
container_volume 21
container_issue 85
container_start_page 115
op_container_end_page 122
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