A coupled consolidation shear model for the process of formation of glaciated soils

It has been generally observed that the measured preconsolidation pressure values for glaciated soils are not compatible with the measured effective pressure values at the bed of the glacier if one-dimensional consolidation alone is considered as the formation process for these soils. In this paper,...

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Published in:Canadian Geotechnical Journal
Main Authors: Huang, Bingquan, Sharma, Jitendra S.
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 2008
Subjects:
Online Access:http://dx.doi.org/10.1139/t07-092
http://www.nrcresearchpress.com/doi/full-xml/10.1139/T07-092
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spelling crcansciencepubl:10.1139/t07-092 2023-12-17T10:30:36+01:00 A coupled consolidation shear model for the process of formation of glaciated soils Huang, Bingquan Sharma, Jitendra S. 2008 http://dx.doi.org/10.1139/t07-092 http://www.nrcresearchpress.com/doi/full-xml/10.1139/T07-092 http://www.nrcresearchpress.com/doi/pdf/10.1139/T07-092 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Canadian Geotechnical Journal volume 45, issue 2, page 226-237 ISSN 0008-3674 1208-6010 Civil and Structural Engineering Geotechnical Engineering and Engineering Geology journal-article 2008 crcansciencepubl https://doi.org/10.1139/t07-092 2023-11-19T13:38:17Z It has been generally observed that the measured preconsolidation pressure values for glaciated soils are not compatible with the measured effective pressure values at the bed of the glacier if one-dimensional consolidation alone is considered as the formation process for these soils. In this paper, a new model for the process of formation of glaciated soil, termed the coupled consolidation shear (CCS) model, is developed using the frameworks of critical state soil mechanics and small-strain consolidation theory. The CCS model includes simultaneous shearing and consolidation of subglacial sediments and is able to simulate profiles of preconsolidation pressure versus depth that closely resemble those observed in glaciated soils. The CCS model is validated by successfully simulating the profile of preconsolidation pressure versus depth for an 80 m deep Battleford till layer in Birsay, Saskatchewan, Canada. The CCS model suggests the existence of anisotropic yield strength and stiffness in glaciated soils as a consequence of coupling subglacial shear and consolidation. Article in Journal/Newspaper glacier* Canadian Science Publishing (via Crossref) Canada Canadian Geotechnical Journal 45 2 226 237
institution Open Polar
collection Canadian Science Publishing (via Crossref)
op_collection_id crcansciencepubl
language English
topic Civil and Structural Engineering
Geotechnical Engineering and Engineering Geology
spellingShingle Civil and Structural Engineering
Geotechnical Engineering and Engineering Geology
Huang, Bingquan
Sharma, Jitendra S.
A coupled consolidation shear model for the process of formation of glaciated soils
topic_facet Civil and Structural Engineering
Geotechnical Engineering and Engineering Geology
description It has been generally observed that the measured preconsolidation pressure values for glaciated soils are not compatible with the measured effective pressure values at the bed of the glacier if one-dimensional consolidation alone is considered as the formation process for these soils. In this paper, a new model for the process of formation of glaciated soil, termed the coupled consolidation shear (CCS) model, is developed using the frameworks of critical state soil mechanics and small-strain consolidation theory. The CCS model includes simultaneous shearing and consolidation of subglacial sediments and is able to simulate profiles of preconsolidation pressure versus depth that closely resemble those observed in glaciated soils. The CCS model is validated by successfully simulating the profile of preconsolidation pressure versus depth for an 80 m deep Battleford till layer in Birsay, Saskatchewan, Canada. The CCS model suggests the existence of anisotropic yield strength and stiffness in glaciated soils as a consequence of coupling subglacial shear and consolidation.
format Article in Journal/Newspaper
author Huang, Bingquan
Sharma, Jitendra S.
author_facet Huang, Bingquan
Sharma, Jitendra S.
author_sort Huang, Bingquan
title A coupled consolidation shear model for the process of formation of glaciated soils
title_short A coupled consolidation shear model for the process of formation of glaciated soils
title_full A coupled consolidation shear model for the process of formation of glaciated soils
title_fullStr A coupled consolidation shear model for the process of formation of glaciated soils
title_full_unstemmed A coupled consolidation shear model for the process of formation of glaciated soils
title_sort coupled consolidation shear model for the process of formation of glaciated soils
publisher Canadian Science Publishing
publishDate 2008
url http://dx.doi.org/10.1139/t07-092
http://www.nrcresearchpress.com/doi/full-xml/10.1139/T07-092
http://www.nrcresearchpress.com/doi/pdf/10.1139/T07-092
geographic Canada
geographic_facet Canada
genre glacier*
genre_facet glacier*
op_source Canadian Geotechnical Journal
volume 45, issue 2, page 226-237
ISSN 0008-3674 1208-6010
op_rights http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining
op_doi https://doi.org/10.1139/t07-092
container_title Canadian Geotechnical Journal
container_volume 45
container_issue 2
container_start_page 226
op_container_end_page 237
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