Grain growth of natural and synthetic ice at 0 °C ...

Abstract. Grain growth can modify the microstructure of natural ice, including the grain size and crystallographic preferred orientation (CPO). To better understand grain-growth processes and kinetics, we compared microstructural data from synthetic and natural ice samples of similar starting grain...

Full description

Bibliographic Details
Main Authors: Fan, Sheng, Prior, David J, Pooley, Brent, Bowman, Hamish, Davidson, Lucy, Wallis, David, Piazolo, Sandra, Qi, Chao, Goldsby, David L, Hager, Travis F
Format: Article in Journal/Newspaper
Language:unknown
Published: Copernicus GmbH 2023
Subjects:
Online Access:https://dx.doi.org/10.17863/cam.100595
https://www.repository.cam.ac.uk/handle/1810/355723
id ftdatacite:10.17863/cam.100595
record_format openpolar
spelling ftdatacite:10.17863/cam.100595 2023-10-01T03:50:31+02:00 Grain growth of natural and synthetic ice at 0 °C ... Fan, Sheng Prior, David J Pooley, Brent Bowman, Hamish Davidson, Lucy Wallis, David Piazolo, Sandra Qi, Chao Goldsby, David L Hager, Travis F 2023 https://dx.doi.org/10.17863/cam.100595 https://www.repository.cam.ac.uk/handle/1810/355723 unknown Copernicus GmbH Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 ScholarlyArticle Article article-journal JournalArticle 2023 ftdatacite https://doi.org/10.17863/cam.100595 2023-09-04T14:57:47Z Abstract. Grain growth can modify the microstructure of natural ice, including the grain size and crystallographic preferred orientation (CPO). To better understand grain-growth processes and kinetics, we compared microstructural data from synthetic and natural ice samples of similar starting grain sizes that were annealed at the solidus temperature (0 ∘C) for durations of a few hours to 33 d. The synthetic ice has a homogeneous initial microstructure characterized by polygonal grains, little intragranular distortion, few bubbles, and a near-random CPO. The natural ice samples were subsampled from ice cores acquired from the Priestley Glacier, Antarctica. This natural ice has a heterogeneous microstructure characterized by a considerable number of air bubbles, widespread intragranular distortion, and a CPO. During annealing, the average grain size of the natural ice barely changes, whereas the average grain size of the synthetic ice gradually increases. These observations demonstrate that grain growth in ... Article in Journal/Newspaper Antarc* Antarctica Priestley Glacier DataCite Metadata Store (German National Library of Science and Technology) Priestley ENVELOPE(161.883,161.883,-75.183,-75.183) Priestley Glacier ENVELOPE(163.367,163.367,-74.333,-74.333)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language unknown
description Abstract. Grain growth can modify the microstructure of natural ice, including the grain size and crystallographic preferred orientation (CPO). To better understand grain-growth processes and kinetics, we compared microstructural data from synthetic and natural ice samples of similar starting grain sizes that were annealed at the solidus temperature (0 ∘C) for durations of a few hours to 33 d. The synthetic ice has a homogeneous initial microstructure characterized by polygonal grains, little intragranular distortion, few bubbles, and a near-random CPO. The natural ice samples were subsampled from ice cores acquired from the Priestley Glacier, Antarctica. This natural ice has a heterogeneous microstructure characterized by a considerable number of air bubbles, widespread intragranular distortion, and a CPO. During annealing, the average grain size of the natural ice barely changes, whereas the average grain size of the synthetic ice gradually increases. These observations demonstrate that grain growth in ...
format Article in Journal/Newspaper
author Fan, Sheng
Prior, David J
Pooley, Brent
Bowman, Hamish
Davidson, Lucy
Wallis, David
Piazolo, Sandra
Qi, Chao
Goldsby, David L
Hager, Travis F
spellingShingle Fan, Sheng
Prior, David J
Pooley, Brent
Bowman, Hamish
Davidson, Lucy
Wallis, David
Piazolo, Sandra
Qi, Chao
Goldsby, David L
Hager, Travis F
Grain growth of natural and synthetic ice at 0 °C ...
author_facet Fan, Sheng
Prior, David J
Pooley, Brent
Bowman, Hamish
Davidson, Lucy
Wallis, David
Piazolo, Sandra
Qi, Chao
Goldsby, David L
Hager, Travis F
author_sort Fan, Sheng
title Grain growth of natural and synthetic ice at 0 °C ...
title_short Grain growth of natural and synthetic ice at 0 °C ...
title_full Grain growth of natural and synthetic ice at 0 °C ...
title_fullStr Grain growth of natural and synthetic ice at 0 °C ...
title_full_unstemmed Grain growth of natural and synthetic ice at 0 °C ...
title_sort grain growth of natural and synthetic ice at 0 °c ...
publisher Copernicus GmbH
publishDate 2023
url https://dx.doi.org/10.17863/cam.100595
https://www.repository.cam.ac.uk/handle/1810/355723
long_lat ENVELOPE(161.883,161.883,-75.183,-75.183)
ENVELOPE(163.367,163.367,-74.333,-74.333)
geographic Priestley
Priestley Glacier
geographic_facet Priestley
Priestley Glacier
genre Antarc*
Antarctica
Priestley Glacier
genre_facet Antarc*
Antarctica
Priestley Glacier
op_rights Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
op_doi https://doi.org/10.17863/cam.100595
_version_ 1778524138432888832