Snowbreeder 5: a Micro-CT device for measuring the snow-microstructure evolution under the simultaneous influence of a temperature gradient and compaction

ABSTRACT The instrumented sample holder Snowbreeder 5 is used to investigate the simultaneous influence of settlement on temperature-gradient snow metamorphism in time-lapse micro-computed tomography experiments. So far, experiments have only been done on temperature-gradient snow metamorphism witho...

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Published in:Journal of Glaciology
Main Authors: WIESE, MAREIKE, SCHNEEBELI, MARTIN
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2017
Subjects:
Online Access:http://dx.doi.org/10.1017/jog.2016.143
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S002214301600143X
id crcambridgeupr:10.1017/jog.2016.143
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spelling crcambridgeupr:10.1017/jog.2016.143 2024-05-12T08:06:15+00:00 Snowbreeder 5: a Micro-CT device for measuring the snow-microstructure evolution under the simultaneous influence of a temperature gradient and compaction WIESE, MAREIKE SCHNEEBELI, MARTIN 2017 http://dx.doi.org/10.1017/jog.2016.143 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S002214301600143X en eng Cambridge University Press (CUP) http://creativecommons.org/licenses/by/4.0/ Journal of Glaciology volume 63, issue 238, page 355-360 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 2017 crcambridgeupr https://doi.org/10.1017/jog.2016.143 2024-04-18T06:54:11Z ABSTRACT The instrumented sample holder Snowbreeder 5 is used to investigate the simultaneous influence of settlement on temperature-gradient snow metamorphism in time-lapse micro-computed tomography experiments. So far, experiments have only been done on temperature-gradient snow metamorphism without settlement or settlement under isothermal conditions. With the new device we can impose a constant temperature gradient on a snow sample and induce settlement by placing a passive load on top of the snow sample. The weight of the load can be varied, simulating various snow heights on top of the snow sample. Snow-temperature measurements on the passive load are possible due to wireless data transfer via Bluetooth. The temperature gradient is set by controlling the air temperature inside the computer tomograph and by a Peltier element at the bottom of the snow sample. First experiments under isothermal conditions and a constant temperature gradient of 43 K m −1 showed that the settlement was reduced to almost half as soon as a temperature gradient was applied under otherwise almost equal snow conditions. The compactive viscosity in the isothermal experiment was in the range of literature values. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Peltier ENVELOPE(-63.495,-63.495,-64.854,-64.854) Journal of Glaciology 63 238 355 360
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
WIESE, MAREIKE
SCHNEEBELI, MARTIN
Snowbreeder 5: a Micro-CT device for measuring the snow-microstructure evolution under the simultaneous influence of a temperature gradient and compaction
topic_facet Earth-Surface Processes
description ABSTRACT The instrumented sample holder Snowbreeder 5 is used to investigate the simultaneous influence of settlement on temperature-gradient snow metamorphism in time-lapse micro-computed tomography experiments. So far, experiments have only been done on temperature-gradient snow metamorphism without settlement or settlement under isothermal conditions. With the new device we can impose a constant temperature gradient on a snow sample and induce settlement by placing a passive load on top of the snow sample. The weight of the load can be varied, simulating various snow heights on top of the snow sample. Snow-temperature measurements on the passive load are possible due to wireless data transfer via Bluetooth. The temperature gradient is set by controlling the air temperature inside the computer tomograph and by a Peltier element at the bottom of the snow sample. First experiments under isothermal conditions and a constant temperature gradient of 43 K m −1 showed that the settlement was reduced to almost half as soon as a temperature gradient was applied under otherwise almost equal snow conditions. The compactive viscosity in the isothermal experiment was in the range of literature values.
format Article in Journal/Newspaper
author WIESE, MAREIKE
SCHNEEBELI, MARTIN
author_facet WIESE, MAREIKE
SCHNEEBELI, MARTIN
author_sort WIESE, MAREIKE
title Snowbreeder 5: a Micro-CT device for measuring the snow-microstructure evolution under the simultaneous influence of a temperature gradient and compaction
title_short Snowbreeder 5: a Micro-CT device for measuring the snow-microstructure evolution under the simultaneous influence of a temperature gradient and compaction
title_full Snowbreeder 5: a Micro-CT device for measuring the snow-microstructure evolution under the simultaneous influence of a temperature gradient and compaction
title_fullStr Snowbreeder 5: a Micro-CT device for measuring the snow-microstructure evolution under the simultaneous influence of a temperature gradient and compaction
title_full_unstemmed Snowbreeder 5: a Micro-CT device for measuring the snow-microstructure evolution under the simultaneous influence of a temperature gradient and compaction
title_sort snowbreeder 5: a micro-ct device for measuring the snow-microstructure evolution under the simultaneous influence of a temperature gradient and compaction
publisher Cambridge University Press (CUP)
publishDate 2017
url http://dx.doi.org/10.1017/jog.2016.143
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S002214301600143X
long_lat ENVELOPE(-63.495,-63.495,-64.854,-64.854)
geographic Peltier
geographic_facet Peltier
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology
volume 63, issue 238, page 355-360
ISSN 0022-1430 1727-5652
op_rights http://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.1017/jog.2016.143
container_title Journal of Glaciology
container_volume 63
container_issue 238
container_start_page 355
op_container_end_page 360
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