Dernière mise à jour
10 octobre 2023
Conditions d'utilisation
Utilisation libre. Obligation d’indiquer la source.

Description

We conducted consecutive loading-relaxation experiments at low strain rates to study the viscoplastic behavior of the intact ice matrix in snow. The experiments were conducted using a micro-compression stage within the X-ray tomography scanner in the SLF cold laboratory.

Next, to evaluate the experiments, a novel, implicit solution of a transient scalar model was developed to estimate the stress exponent and time scales in the effective creep relation (Glen's law). The result reveals that, for the first time, a transition in the exponent in Glen's law depends on geometrical grain size. A cross-over of stress exponent $n=1.9$ for fine grains to $n=4.4$ for coarse grains is interpreted as a transition from grain boundary sliding to dislocation creep.

The dataset includes compression force data from 11 experiments and corresponding 3D image data from tomography scans.

Ressources

Showcases

Informations complémentaires

Identifier
2fbce191-4283-4b68-aa4c-ad90723146ed@envidat
Date de publication
10 octobre 2023
Date de modification
10 octobre 2023
Conforme à
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Editeur
EnviDat
Points de contact
Langues
Anglais
Informations complémentaires
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Landing page
https://www.envidat.ch/#/metadata/slow-snow-compression
Documentation
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Couverture temporelle
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Couverture spatiale
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Intervalle d'actualisation
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