Electrical Behaviour of Finely Divided Ice

Abstract The electrical behaviour of ice which has been finely ground and compressed was investigated during ageing in air and over a range of temperatures. The dielectric behaviour may be accurately represented as the sum of two elliptical relaxation spectra. The behaviour eventually stabilizes wit...

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Published in:Journal of Glaciology
Main Authors: Paren, J. G., Glen, J. W.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1978
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000033396
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000033396
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spelling crcambridgeupr:10.1017/s0022143000033396 2024-03-03T08:46:02+00:00 Electrical Behaviour of Finely Divided Ice Paren, J. G. Glen, J. W. 1978 http://dx.doi.org/10.1017/s0022143000033396 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000033396 en eng Cambridge University Press (CUP) Journal of Glaciology volume 21, issue 85, page 173-191 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1978 crcambridgeupr https://doi.org/10.1017/s0022143000033396 2024-02-08T08:36:10Z Abstract The electrical behaviour of ice which has been finely ground and compressed was investigated during ageing in air and over a range of temperatures. The dielectric behaviour may be accurately represented as the sum of two elliptical relaxation spectra. The behaviour eventually stabilizes with similar activation energies for the mean relaxation time of each spectrum c. 0.25 eV, and the ratio of the relaxation times is ten in samples of density c . 0.42 Mg m -3 . Arguments are presented on whether the higher-frequency dispersion is a consequence of the heterogeneous nature of the samples or is a bulk relaxation process. The similarities between the behaviour of such finely ground ice and of deposited snow and polar glacier ice are discussed. The extent to which the results may be attributed to surface adsorption of CO 2 are examined by reference to measurements of the CO 2 content of finely divided ice and ice from polar regions. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 21 85 173 191
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Paren, J. G.
Glen, J. W.
Electrical Behaviour of Finely Divided Ice
topic_facet Earth-Surface Processes
description Abstract The electrical behaviour of ice which has been finely ground and compressed was investigated during ageing in air and over a range of temperatures. The dielectric behaviour may be accurately represented as the sum of two elliptical relaxation spectra. The behaviour eventually stabilizes with similar activation energies for the mean relaxation time of each spectrum c. 0.25 eV, and the ratio of the relaxation times is ten in samples of density c . 0.42 Mg m -3 . Arguments are presented on whether the higher-frequency dispersion is a consequence of the heterogeneous nature of the samples or is a bulk relaxation process. The similarities between the behaviour of such finely ground ice and of deposited snow and polar glacier ice are discussed. The extent to which the results may be attributed to surface adsorption of CO 2 are examined by reference to measurements of the CO 2 content of finely divided ice and ice from polar regions.
format Article in Journal/Newspaper
author Paren, J. G.
Glen, J. W.
author_facet Paren, J. G.
Glen, J. W.
author_sort Paren, J. G.
title Electrical Behaviour of Finely Divided Ice
title_short Electrical Behaviour of Finely Divided Ice
title_full Electrical Behaviour of Finely Divided Ice
title_fullStr Electrical Behaviour of Finely Divided Ice
title_full_unstemmed Electrical Behaviour of Finely Divided Ice
title_sort electrical behaviour of finely divided ice
publisher Cambridge University Press (CUP)
publishDate 1978
url http://dx.doi.org/10.1017/s0022143000033396
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000033396
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology
volume 21, issue 85, page 173-191
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000033396
container_title Journal of Glaciology
container_volume 21
container_issue 85
container_start_page 173
op_container_end_page 191
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