Campus Units
Geological and Atmospheric Sciences
Document Type
Article
Publication Version
Published Version
Publication Date
1998
Journal or Book Title
Journal of Glaciology
Volume
44
Issue
148
First Page
634
Last Page
642
DOI
10.3198/1998JoG44-148-634-642
Abstract
A ring-shear device was used to study the factors that control the ultimate(steady) strength of till at high shear strains.Tests at a steady strain rate and at different stresses normal to the shearing direction yielded ultimate friction angles of 26.3° and 18.6° for tills containing 4% and 30% clay-sized particles, respectively Other tests at steady normal stresses and variable shear-strain rates indicated a tendency for both tills to weaken slightly with increasing strain rate. This weakening may be due to small increases in till porosity.
These results provide no evidence of viscous behavior and suggest that a Coulomb-plastic idealization is reasonable for till deformation. However, viscous behavior has often been suggested on the basis of distributed shear strain observed in subglacial till. We hypothesize that deformation may become distributed in till that is deformed cyclically in response to fluctuations in basal water pressure. During a deformation event, transient dilation of discrete shear zones should cause a reduction in internal pore-water pressure that should strengthen these zones relative to the surrounding till, a process called dilatant hardening. Consequent changes in shear-zone position, when integrated over time, may yield the observed distributed strain.
Rights
Creative Commons Attribution license.
Copyright Owner
International Glaciological Society
Copyright Date
1998
Language
en
File Format
application/pdf
Recommended Citation
Iverson, Neal R.; Hooyer, Thomas S.; and Baker, Robert W., "Ring-shear studies of till deformation: Coulomb-plastic behavior and distributed strain in glacier beds" (1998). Geological and Atmospheric Sciences Publications. 133.
https://lib.dr.iastate.edu/ge_at_pubs/133
Comments
This article is from Journal of Glaciology 44 (1998): 634, doi:10.3198/1998JoG44-148-634-642. Posted with permission.