Shear dilation of subglacial till results in time-dependent sliding laws

The dynamics of glacial sliding over water-saturated tills are poorly constrained and difficult to capture realistically in large-scale models. Experiments characterize till as a plastic material with a pressure-dependent yield stress, but the subglacial water pressure may fluctuate on annual to dai...

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Main Authors: Warburton, KLP, Hewitt, DR, Neufeld, JA
Format: Article in Journal/Newspaper
Language:English
Published: The Royal Society 2023
Subjects:
Online Access:https://discovery.ucl.ac.uk/id/eprint/10164131/1/Hewitt_Shear%20dilation%20of%20subglacial%20till%20results%20in%20time-dependent%20sliding%20laws_VoR.pdf
https://discovery.ucl.ac.uk/id/eprint/10164131/
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author Warburton, KLP
Hewitt, DR
Neufeld, JA
author_facet Warburton, KLP
Hewitt, DR
Neufeld, JA
author_sort Warburton, KLP
collection University College London: UCL Discovery
description The dynamics of glacial sliding over water-saturated tills are poorly constrained and difficult to capture realistically in large-scale models. Experiments characterize till as a plastic material with a pressure-dependent yield stress, but the subglacial water pressure may fluctuate on annual to daily timescales, leading to transient adjustment of the till. We construct a continuum two-phase model of coupled fluid and solid deformation, describing the movement of water through the pore space of a till that is itself dilating and deforming. By forcing the model with time-dependent effective pressure at the ice-till interface, we infer the resulting relationships between basal traction, solid fraction and rate of deformation. We find that shear dilation introduces internal pressure variations and transient dilatant strengthening emerges, leading to hysteretic behaviour in low-permeability materials. The result is a time-dependent effective sliding law, with permeability-dependent lag between changes in effective pressure and the slidingspeed. This deviation from traditional steady-state sliding laws may play an important role in a wide range of transient ice-sheet phenomena, from glacier surges to the tidal response of ice streams.
format Article in Journal/Newspaper
genre Ice Sheet
genre_facet Ice Sheet
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institution Open Polar
language English
op_collection_id ftucl
op_relation https://discovery.ucl.ac.uk/id/eprint/10164131/1/Hewitt_Shear%20dilation%20of%20subglacial%20till%20results%20in%20time-dependent%20sliding%20laws_VoR.pdf
https://discovery.ucl.ac.uk/id/eprint/10164131/
op_rights open
op_source Proceedings of the Royal Society A: Mathematical, Physical and Engineering Sciences , 479 (2269) , Article 20220536. (2023)
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spelling ftucl:oai:eprints.ucl.ac.uk.OAI2:10164131 2025-01-16T22:26:40+00:00 Shear dilation of subglacial till results in time-dependent sliding laws Warburton, KLP Hewitt, DR Neufeld, JA 2023-01-25 text https://discovery.ucl.ac.uk/id/eprint/10164131/1/Hewitt_Shear%20dilation%20of%20subglacial%20till%20results%20in%20time-dependent%20sliding%20laws_VoR.pdf https://discovery.ucl.ac.uk/id/eprint/10164131/ eng eng The Royal Society https://discovery.ucl.ac.uk/id/eprint/10164131/1/Hewitt_Shear%20dilation%20of%20subglacial%20till%20results%20in%20time-dependent%20sliding%20laws_VoR.pdf https://discovery.ucl.ac.uk/id/eprint/10164131/ open Proceedings of the Royal Society A: Mathematical, Physical and Engineering Sciences , 479 (2269) , Article 20220536. (2023) subglacial till glacier dynamics basal sliding Article 2023 ftucl 2023-11-27T13:07:32Z The dynamics of glacial sliding over water-saturated tills are poorly constrained and difficult to capture realistically in large-scale models. Experiments characterize till as a plastic material with a pressure-dependent yield stress, but the subglacial water pressure may fluctuate on annual to daily timescales, leading to transient adjustment of the till. We construct a continuum two-phase model of coupled fluid and solid deformation, describing the movement of water through the pore space of a till that is itself dilating and deforming. By forcing the model with time-dependent effective pressure at the ice-till interface, we infer the resulting relationships between basal traction, solid fraction and rate of deformation. We find that shear dilation introduces internal pressure variations and transient dilatant strengthening emerges, leading to hysteretic behaviour in low-permeability materials. The result is a time-dependent effective sliding law, with permeability-dependent lag between changes in effective pressure and the slidingspeed. This deviation from traditional steady-state sliding laws may play an important role in a wide range of transient ice-sheet phenomena, from glacier surges to the tidal response of ice streams. Article in Journal/Newspaper Ice Sheet University College London: UCL Discovery
spellingShingle subglacial till
glacier dynamics
basal sliding
Warburton, KLP
Hewitt, DR
Neufeld, JA
Shear dilation of subglacial till results in time-dependent sliding laws
title Shear dilation of subglacial till results in time-dependent sliding laws
title_full Shear dilation of subglacial till results in time-dependent sliding laws
title_fullStr Shear dilation of subglacial till results in time-dependent sliding laws
title_full_unstemmed Shear dilation of subglacial till results in time-dependent sliding laws
title_short Shear dilation of subglacial till results in time-dependent sliding laws
title_sort shear dilation of subglacial till results in time-dependent sliding laws
topic subglacial till
glacier dynamics
basal sliding
topic_facet subglacial till
glacier dynamics
basal sliding
url https://discovery.ucl.ac.uk/id/eprint/10164131/1/Hewitt_Shear%20dilation%20of%20subglacial%20till%20results%20in%20time-dependent%20sliding%20laws_VoR.pdf
https://discovery.ucl.ac.uk/id/eprint/10164131/