Downslope movements at shallow depths related to cyclic pore-pressure changes

Slow, shallow ground movements in a slope near Yellowknife caused excessive tilting of timber piles that supported an engineering structure. To avoid damage to the structure, the pile foundations had to be replaced by rigid concrete piers that were designed to resist the forces of the moving soil ma...

Full description

Bibliographic Details
Published in:Canadian Geotechnical Journal
Main Author: Eigenbrod, K.D.
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 1993
Subjects:
Online Access:http://dx.doi.org/10.1139/t93-040
http://www.nrcresearchpress.com/doi/pdf/10.1139/t93-040
id crcansciencepubl:10.1139/t93-040
record_format openpolar
spelling crcansciencepubl:10.1139/t93-040 2023-12-17T10:48:39+01:00 Downslope movements at shallow depths related to cyclic pore-pressure changes Eigenbrod, K.D. 1993 http://dx.doi.org/10.1139/t93-040 http://www.nrcresearchpress.com/doi/pdf/10.1139/t93-040 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Canadian Geotechnical Journal volume 30, issue 3, page 464-475 ISSN 0008-3674 1208-6010 Civil and Structural Engineering Geotechnical Engineering and Engineering Geology journal-article 1993 crcansciencepubl https://doi.org/10.1139/t93-040 2023-11-19T13:39:15Z Slow, shallow ground movements in a slope near Yellowknife caused excessive tilting of timber piles that supported an engineering structure. To avoid damage to the structure, the pile foundations had to be replaced by rigid concrete piers that were designed to resist the forces of the moving soil mass. Downhill movements were rather slow and, during an initial inspection, were indicated only by soil that was pushed up against a series of piles on their uphill sides, while gaps had formed on their downhill sides. No open cracks or bulging was observed on the slope. A stability analysis indicated that the slope was not in a state of limit equilibrium. To obtain a better understanding of the creep movements in the slope and their effect on the rigid concrete piers, extensive instrumentation was carried out after the construction of the piers. This included slope indicators, piezometers, thermistors, and total-pressure cells against one of the concrete piers. In addition, a triaxial testing program was undertaken in which the effect of cyclic pore-water pressure changes on the long-term deformations of the shallow clay layer was investigated. From the data collected in the field and laboratory, it could be concluded that (i) tilting of the original timber piles was caused by downslope movements related to cyclic pore-water increases; (ii) the lateral soil movements increased almost linearly with depth from 2 m below the ground surface, with no indication of a slip surface; and (iii) the pressures exerted by the moving soil mass against the rigid concrete piers within the soil mass were equal to the passive resistance activated within the moving soil mass. Key words : soil creep, slope movements, soil pressures, pore-water pressures, freezing pressures, permafrost, cyclic loading. Article in Journal/Newspaper permafrost Yellowknife Canadian Science Publishing (via Crossref) Yellowknife Tilting ENVELOPE(-54.065,-54.065,49.700,49.700) Canadian Geotechnical Journal 30 3 464 475
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
Eigenbrod, K.D.
Downslope movements at shallow depths related to cyclic pore-pressure changes
topic_facet Civil and Structural Engineering
Geotechnical Engineering and Engineering Geology
description Slow, shallow ground movements in a slope near Yellowknife caused excessive tilting of timber piles that supported an engineering structure. To avoid damage to the structure, the pile foundations had to be replaced by rigid concrete piers that were designed to resist the forces of the moving soil mass. Downhill movements were rather slow and, during an initial inspection, were indicated only by soil that was pushed up against a series of piles on their uphill sides, while gaps had formed on their downhill sides. No open cracks or bulging was observed on the slope. A stability analysis indicated that the slope was not in a state of limit equilibrium. To obtain a better understanding of the creep movements in the slope and their effect on the rigid concrete piers, extensive instrumentation was carried out after the construction of the piers. This included slope indicators, piezometers, thermistors, and total-pressure cells against one of the concrete piers. In addition, a triaxial testing program was undertaken in which the effect of cyclic pore-water pressure changes on the long-term deformations of the shallow clay layer was investigated. From the data collected in the field and laboratory, it could be concluded that (i) tilting of the original timber piles was caused by downslope movements related to cyclic pore-water increases; (ii) the lateral soil movements increased almost linearly with depth from 2 m below the ground surface, with no indication of a slip surface; and (iii) the pressures exerted by the moving soil mass against the rigid concrete piers within the soil mass were equal to the passive resistance activated within the moving soil mass. Key words : soil creep, slope movements, soil pressures, pore-water pressures, freezing pressures, permafrost, cyclic loading.
format Article in Journal/Newspaper
author Eigenbrod, K.D.
author_facet Eigenbrod, K.D.
author_sort Eigenbrod, K.D.
title Downslope movements at shallow depths related to cyclic pore-pressure changes
title_short Downslope movements at shallow depths related to cyclic pore-pressure changes
title_full Downslope movements at shallow depths related to cyclic pore-pressure changes
title_fullStr Downslope movements at shallow depths related to cyclic pore-pressure changes
title_full_unstemmed Downslope movements at shallow depths related to cyclic pore-pressure changes
title_sort downslope movements at shallow depths related to cyclic pore-pressure changes
publisher Canadian Science Publishing
publishDate 1993
url http://dx.doi.org/10.1139/t93-040
http://www.nrcresearchpress.com/doi/pdf/10.1139/t93-040
long_lat ENVELOPE(-54.065,-54.065,49.700,49.700)
geographic Yellowknife
Tilting
geographic_facet Yellowknife
Tilting
genre permafrost
Yellowknife
genre_facet permafrost
Yellowknife
op_source Canadian Geotechnical Journal
volume 30, issue 3, page 464-475
ISSN 0008-3674 1208-6010
op_rights http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining
op_doi https://doi.org/10.1139/t93-040
container_title Canadian Geotechnical Journal
container_volume 30
container_issue 3
container_start_page 464
op_container_end_page 475
_version_ 1785572885794914304