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Electrical conductivity of ice VII

It was discovered that a peak appears near a pressure of P(c) = 10 GPa in the electrical conductivity of ice VII as measured through impedance spectroscopy in a diamond anvil cell (DAC) during the process of compression from 2 GPa to 40 GPa at room temperature. The activation energy for the conducti...

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Autores principales: Okada, Taku, Iitaka, Toshiaki, Yagi, Takehiko, Aoki, Katsutoshi
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group 2014
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4105784/
https://www.ncbi.nlm.nih.gov/pubmed/25047728
http://dx.doi.org/10.1038/srep05778
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author Okada, Taku
Iitaka, Toshiaki
Yagi, Takehiko
Aoki, Katsutoshi
author_facet Okada, Taku
Iitaka, Toshiaki
Yagi, Takehiko
Aoki, Katsutoshi
author_sort Okada, Taku
collection PubMed
description It was discovered that a peak appears near a pressure of P(c) = 10 GPa in the electrical conductivity of ice VII as measured through impedance spectroscopy in a diamond anvil cell (DAC) during the process of compression from 2 GPa to 40 GPa at room temperature. The activation energy for the conductivity measured in the cooling/heating process between 278 K and 303 K reached a minimum near P(c). Theoretical modelling and molecular dynamics simulations suggest that the origin of this unique peak is the transition of the major charge carriers from the rotational defects to the ionic defects.
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spelling pubmed-41057842014-07-22 Electrical conductivity of ice VII Okada, Taku Iitaka, Toshiaki Yagi, Takehiko Aoki, Katsutoshi Sci Rep Article It was discovered that a peak appears near a pressure of P(c) = 10 GPa in the electrical conductivity of ice VII as measured through impedance spectroscopy in a diamond anvil cell (DAC) during the process of compression from 2 GPa to 40 GPa at room temperature. The activation energy for the conductivity measured in the cooling/heating process between 278 K and 303 K reached a minimum near P(c). Theoretical modelling and molecular dynamics simulations suggest that the origin of this unique peak is the transition of the major charge carriers from the rotational defects to the ionic defects. Nature Publishing Group 2014-07-22 /pmc/articles/PMC4105784/ /pubmed/25047728 http://dx.doi.org/10.1038/srep05778 Text en Copyright © 2014, Macmillan Publishers Limited. All rights reserved http://creativecommons.org/licenses/by-nc-nd/4.0/ This work is licensed under a Creative Commons Attribution-NonCommercial-NoDerivs 4.0 International License. The images or other third party material in this article are included in the article's Creative Commons license, unless indicated otherwise in the credit line; if the material is not included under the Creative Commons license, users will need to obtain permission from the license holder in order to reproduce the material. To view a copy of this license, visit http://creativecommons.org/licenses/by-nc-nd/4.0/
spellingShingle Article
Okada, Taku
Iitaka, Toshiaki
Yagi, Takehiko
Aoki, Katsutoshi
Electrical conductivity of ice VII
title Electrical conductivity of ice VII
title_full Electrical conductivity of ice VII
title_fullStr Electrical conductivity of ice VII
title_full_unstemmed Electrical conductivity of ice VII
title_short Electrical conductivity of ice VII
title_sort electrical conductivity of ice vii
topic Article
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4105784/
https://www.ncbi.nlm.nih.gov/pubmed/25047728
http://dx.doi.org/10.1038/srep05778
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