Dielectric anisotropy as indicator of crystal orientation fabric in Dome Fuji ice core: method and initial results

Abstract Polycrystalline ice is known to exhibit macroscopic anisotropy in relative permittivity ( ɛ ) depending on the crystal orientation fabric (COF). Using a new system designed to measure the tensorial components of ɛ , we investigated the dielectric anisotropy (Δ ɛ ) of a deep ice core sample...

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Bibliographic Details
Published in:Journal of Glaciology
Main Authors: Saruya, Tomotaka, Fujita, Shuji, Inoue, Ryo
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2021
Subjects:
Online Access:http://dx.doi.org/10.1017/jog.2021.73
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143021000733