Zuletzt aktualisiert
10. Oktober 2023
Nutzungsbedingungen
Freie Nutzung. Quellenangabe ist Pflicht.

Beschreibung

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.

Ressourcen

Showcases

Zusätzliche Informationen

Identifier
2fbce191-4283-4b68-aa4c-ad90723146ed@envidat
Publikationsdatum
10. Oktober 2023
Änderungsdatum
10. Oktober 2023
Konform mit
-
Publisher
EnviDat
Kontaktstellen
Sprachen
Englisch
Weitere Informationen
-
Landing page
https://www.envidat.ch/#/metadata/slow-snow-compression
Dokumentation
-
Zeitliche Abdeckung
-
Räumliche Abdeckung
-
Aktualisierungsintervall
-
Metadatenzugriff
API (JSON) XML herunterladen