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

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 settle...

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Published in:Journal of Glaciology
Main Authors: MAREIKE WIESE, MARTIN SCHNEEBELI
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press 2017
Subjects:
Online Access:https://doi.org/10.1017/jog.2016.143
https://doaj.org/article/adc09eb763a34ca8b68b55e934d422e6
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spelling ftdoajarticles:oai:doaj.org/article:adc09eb763a34ca8b68b55e934d422e6 2023-05-15T16:57:34+02:00 Snowbreeder 5: a Micro-CT device for measuring the snow-microstructure evolution under the simultaneous influence of a temperature gradient and compaction MAREIKE WIESE MARTIN SCHNEEBELI 2017-04-01T00:00:00Z https://doi.org/10.1017/jog.2016.143 https://doaj.org/article/adc09eb763a34ca8b68b55e934d422e6 EN eng Cambridge University Press https://www.cambridge.org/core/product/identifier/S002214301600143X/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2016.143 0022-1430 1727-5652 https://doaj.org/article/adc09eb763a34ca8b68b55e934d422e6 Journal of Glaciology, Vol 63, Pp 355-360 (2017) snow snow mechanics snow metamorphism snow microstructure snow physics Environmental sciences GE1-350 Meteorology. Climatology QC851-999 article 2017 ftdoajarticles https://doi.org/10.1017/jog.2016.143 2023-03-12T01:30:59Z 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 Directory of Open Access Journals: DOAJ Articles Peltier ENVELOPE(-63.495,-63.495,-64.854,-64.854) Journal of Glaciology 63 238 355 360
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic snow
snow mechanics
snow metamorphism
snow microstructure
snow physics
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
spellingShingle snow
snow mechanics
snow metamorphism
snow microstructure
snow physics
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
MAREIKE WIESE
MARTIN SCHNEEBELI
Snowbreeder 5: a Micro-CT device for measuring the snow-microstructure evolution under the simultaneous influence of a temperature gradient and compaction
topic_facet snow
snow mechanics
snow metamorphism
snow microstructure
snow physics
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
description 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 MAREIKE WIESE
MARTIN SCHNEEBELI
author_facet MAREIKE WIESE
MARTIN SCHNEEBELI
author_sort MAREIKE WIESE
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
publishDate 2017
url https://doi.org/10.1017/jog.2016.143
https://doaj.org/article/adc09eb763a34ca8b68b55e934d422e6
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, Vol 63, Pp 355-360 (2017)
op_relation https://www.cambridge.org/core/product/identifier/S002214301600143X/type/journal_article
https://doaj.org/toc/0022-1430
https://doaj.org/toc/1727-5652
doi:10.1017/jog.2016.143
0022-1430
1727-5652
https://doaj.org/article/adc09eb763a34ca8b68b55e934d422e6
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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