The Orientation Polarization in Hexagonal Ice Parallel and Perpendicular to the c-axis
Abstract The relative permittivity and loss of zone-refined single crystals of hexagonal ice have been measured in the temperature range 200–271 K and frequency range 0.5 HZ–0.2 MHz, using brass, stainless steel, and gold-foil electrodes. The c -axis of the crystal was oriented parallel to the elect...
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Language: | English |
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Cambridge University Press (CUP)
1978
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Online Access: | http://dx.doi.org/10.1017/s0022143000033463 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000033463 |
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crcambridgeupr:10.1017/s0022143000033463 2024-03-03T08:45:59+00:00 The Orientation Polarization in Hexagonal Ice Parallel and Perpendicular to the c-axis Johari, G. P. Jones, S. J. 1978 http://dx.doi.org/10.1017/s0022143000033463 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000033463 en eng Cambridge University Press (CUP) Journal of Glaciology volume 21, issue 85, page 259-276 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1978 crcambridgeupr https://doi.org/10.1017/s0022143000033463 2024-02-08T08:41:37Z Abstract The relative permittivity and loss of zone-refined single crystals of hexagonal ice have been measured in the temperature range 200–271 K and frequency range 0.5 HZ–0.2 MHz, using brass, stainless steel, and gold-foil electrodes. The c -axis of the crystal was oriented parallel to the electric field in 14 samples and perpendicular to the field in 8 samples. The equilibrium relative permittivity of orientation polarization ϵ 0 , parallel and perpendicular to the c -axis, is 96.5±1 and the average relaxation time τ a y is 36 μs at 265±0.5K; ϵ 0 = 124±1.5 and τ av = 30 ms, at 210 K. The magnitude of the orientation polarization obeys the Curie-Weiss equation with T 0 = 15±2 K for both the orientations. These values are in contrast with the c. 17% difference in ϵ o for the two orientations reported in the literature. The extrapolated limiting high-frequency relative permittivity ϵ ∞ , measured for both the orientations, is indistinguishable within 0.5%. The logarithmic plot of the product of τ av and temperature against the reciprocal temperature is linear in the range 210–271 K and gives an activation energy and a pre-exponential factor of 51±2 kJ mol –1 and 0.93±0.22 ps K respectively, for both the orientations of the c -axis with respect to the electric field. The decrease in activation energy which has been reported to occur in polycrystalline ice and in single crystal ice near 230 K is not found until a temperature of 210 K. Single crystals of ice stored in the dielectric cell, after the completion of measurements, for periods ranging from 1–11 weeks at 253±2 K showed no change in their ϵ 0 , τ av , ϵ ∞ that could be attributed to the effect of ageing on the orientation polarization. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 21 85 259 276 |
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Open Polar |
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Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
topic |
Earth-Surface Processes |
spellingShingle |
Earth-Surface Processes Johari, G. P. Jones, S. J. The Orientation Polarization in Hexagonal Ice Parallel and Perpendicular to the c-axis |
topic_facet |
Earth-Surface Processes |
description |
Abstract The relative permittivity and loss of zone-refined single crystals of hexagonal ice have been measured in the temperature range 200–271 K and frequency range 0.5 HZ–0.2 MHz, using brass, stainless steel, and gold-foil electrodes. The c -axis of the crystal was oriented parallel to the electric field in 14 samples and perpendicular to the field in 8 samples. The equilibrium relative permittivity of orientation polarization ϵ 0 , parallel and perpendicular to the c -axis, is 96.5±1 and the average relaxation time τ a y is 36 μs at 265±0.5K; ϵ 0 = 124±1.5 and τ av = 30 ms, at 210 K. The magnitude of the orientation polarization obeys the Curie-Weiss equation with T 0 = 15±2 K for both the orientations. These values are in contrast with the c. 17% difference in ϵ o for the two orientations reported in the literature. The extrapolated limiting high-frequency relative permittivity ϵ ∞ , measured for both the orientations, is indistinguishable within 0.5%. The logarithmic plot of the product of τ av and temperature against the reciprocal temperature is linear in the range 210–271 K and gives an activation energy and a pre-exponential factor of 51±2 kJ mol –1 and 0.93±0.22 ps K respectively, for both the orientations of the c -axis with respect to the electric field. The decrease in activation energy which has been reported to occur in polycrystalline ice and in single crystal ice near 230 K is not found until a temperature of 210 K. Single crystals of ice stored in the dielectric cell, after the completion of measurements, for periods ranging from 1–11 weeks at 253±2 K showed no change in their ϵ 0 , τ av , ϵ ∞ that could be attributed to the effect of ageing on the orientation polarization. |
format |
Article in Journal/Newspaper |
author |
Johari, G. P. Jones, S. J. |
author_facet |
Johari, G. P. Jones, S. J. |
author_sort |
Johari, G. P. |
title |
The Orientation Polarization in Hexagonal Ice Parallel and Perpendicular to the c-axis |
title_short |
The Orientation Polarization in Hexagonal Ice Parallel and Perpendicular to the c-axis |
title_full |
The Orientation Polarization in Hexagonal Ice Parallel and Perpendicular to the c-axis |
title_fullStr |
The Orientation Polarization in Hexagonal Ice Parallel and Perpendicular to the c-axis |
title_full_unstemmed |
The Orientation Polarization in Hexagonal Ice Parallel and Perpendicular to the c-axis |
title_sort |
orientation polarization in hexagonal ice parallel and perpendicular to the c-axis |
publisher |
Cambridge University Press (CUP) |
publishDate |
1978 |
url |
http://dx.doi.org/10.1017/s0022143000033463 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000033463 |
genre |
Journal of Glaciology |
genre_facet |
Journal of Glaciology |
op_source |
Journal of Glaciology volume 21, issue 85, page 259-276 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000033463 |
container_title |
Journal of Glaciology |
container_volume |
21 |
container_issue |
85 |
container_start_page |
259 |
op_container_end_page |
276 |
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1792501760883949568 |