Ploughing of subglacial sediment

Abstract Mechanical conditions at the base of Trapridge Glacier, Yukon Territory, were investigated using a “ploughmeter”. We describe the physical characteristics and the theory of this new instrument as well as its operation. Observational results reveal variations in ploughmeter response that mig...

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Published in:Journal of Glaciology
Main Authors: Fischer, URS H., Clarke, Garry K. C.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1994
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000003853
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000003853
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spelling crcambridgeupr:10.1017/s0022143000003853 2024-09-15T18:15:38+00:00 Ploughing of subglacial sediment Fischer, URS H. Clarke, Garry K. C. 1994 http://dx.doi.org/10.1017/s0022143000003853 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000003853 en eng Cambridge University Press (CUP) Journal of Glaciology volume 40, issue 134, page 97-106 ISSN 0022-1430 1727-5652 journal-article 1994 crcambridgeupr https://doi.org/10.1017/s0022143000003853 2024-08-28T04:00:57Z Abstract Mechanical conditions at the base of Trapridge Glacier, Yukon Territory, were investigated using a “ploughmeter”. We describe the physical characteristics and the theory of this new instrument as well as its operation. Observational results reveal variations in ploughmeter response that might be attributed to spatial variability in subglacial processes or spatial variation in sediment granulometry. Quantitative analysis of the interaction of the ploughmeter with the basal layer yields estimates of rheological parameters. If the sediment is assumed to behave as a Newtonian viscous fluid, the estimated effective viscosity is 3.0 × 10 9 −3.1 × 10 10 Pas; if it is assumed to behave as an ideal plastic solid, the estimated yield strength is 48–57 kPa. In both cases, the estimated shear resistance of subglacial material is comparable to but somewhat less than that required to balance fully the applied basal shear stress. Article in Journal/Newspaper Journal of Glaciology Yukon Cambridge University Press Journal of Glaciology 40 134 97 106
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
description Abstract Mechanical conditions at the base of Trapridge Glacier, Yukon Territory, were investigated using a “ploughmeter”. We describe the physical characteristics and the theory of this new instrument as well as its operation. Observational results reveal variations in ploughmeter response that might be attributed to spatial variability in subglacial processes or spatial variation in sediment granulometry. Quantitative analysis of the interaction of the ploughmeter with the basal layer yields estimates of rheological parameters. If the sediment is assumed to behave as a Newtonian viscous fluid, the estimated effective viscosity is 3.0 × 10 9 −3.1 × 10 10 Pas; if it is assumed to behave as an ideal plastic solid, the estimated yield strength is 48–57 kPa. In both cases, the estimated shear resistance of subglacial material is comparable to but somewhat less than that required to balance fully the applied basal shear stress.
format Article in Journal/Newspaper
author Fischer, URS H.
Clarke, Garry K. C.
spellingShingle Fischer, URS H.
Clarke, Garry K. C.
Ploughing of subglacial sediment
author_facet Fischer, URS H.
Clarke, Garry K. C.
author_sort Fischer, URS H.
title Ploughing of subglacial sediment
title_short Ploughing of subglacial sediment
title_full Ploughing of subglacial sediment
title_fullStr Ploughing of subglacial sediment
title_full_unstemmed Ploughing of subglacial sediment
title_sort ploughing of subglacial sediment
publisher Cambridge University Press (CUP)
publishDate 1994
url http://dx.doi.org/10.1017/s0022143000003853
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000003853
genre Journal of Glaciology
Yukon
genre_facet Journal of Glaciology
Yukon
op_source Journal of Glaciology
volume 40, issue 134, page 97-106
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000003853
container_title Journal of Glaciology
container_volume 40
container_issue 134
container_start_page 97
op_container_end_page 106
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