Building foundations on permafrost: Mackenzie Valley, N.W.T.

Exploratory investigations of the foundations on permafrost at the settlements of the Mackenzie River District were undertaken during the summer of 1950. Timber mudsill foundations were the most common type used, followed by wood, steel, concrete piles, and concrete wall footings. More than half of...

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Bibliographic Details
Main Author: Pihlainen, J. A.
Format: Report
Language:English
Published: National Research Council of Canada. Division of Building Research 1951
Subjects:
sol
Ice
Online Access:https://dx.doi.org/10.4224/20358458
https://nrc-publications.canada.ca/eng/view/object/?id=c5f8a810-8f2f-4de7-b8d6-1d60c2f5003f
id ftdatacite:10.4224/20358458
record_format openpolar
spelling ftdatacite:10.4224/20358458 2023-05-15T16:37:18+02:00 Building foundations on permafrost: Mackenzie Valley, N.W.T. Pihlainen, J. A. 1951 https://dx.doi.org/10.4224/20358458 https://nrc-publications.canada.ca/eng/view/object/?id=c5f8a810-8f2f-4de7-b8d6-1d60c2f5003f en eng National Research Council of Canada. Division of Building Research permafrost soils foundations frost heaving settlement pergélisol sol fondation ouvrage foisonnement par le gel tassement Basements and foundations Sous-sol et fondations Text Report report ScholarlyArticle 1951 ftdatacite https://doi.org/10.4224/20358458 2021-11-05T12:55:41Z Exploratory investigations of the foundations on permafrost at the settlements of the Mackenzie River District were undertaken during the summer of 1950. Timber mudsill foundations were the most common type used, followed by wood, steel, concrete piles, and concrete wall footings. More than half of the foundations studied showed some failure either as a result of frost heaving or settlement. Twenty-five structures were examined in detail giving building type, soil conditions and foundation type. Surface timber mudsill foundations were found unsuitable in frost susceptible soils and showed deterioration in as little as five years. Timber and concrete pad foundations showed similar failures. Recommendations for foundation selection should be preceded by a reconnaisance survey consisting of detailed information on topography, drainage, vegetation, permafrost and housing in the general area. Next, site surveys should be carried out giving details of the soil profile, groundwater level, extent and depth of the permafrost and location and size of ice lenses. Preference should be given to sites with suitable foundation materials such as gravels; to areas free from permafrost or where permafrost occurs permanently; to areas having good drainage; and to areas having non-frost susceptible soils. Lastly a cost and function study should precede the final selection of the foundation type. : Au cours de l'été de 1950, des études exploratoires ont été menées sur les fondations implantées dans le pergélisol lors d'une visite des agglomérations du district du Mackenzie. Les fondations les plus communes étaient les semelles de madriers, suivies du bois, de l'acier, de pieux de béton et de semelles de béton. Plus de la moitié des fondations examinées ont montré des signes de détérioration, soit à la suite de soulèvements dûs au gel, soit à la suite de tassements. Vingt-cinq structures ont été étudiées en dé tail en tenant compte du genre de bâtiment, des conditions du sol et du type de fondation. Report Ice Mackenzie river Mackenzie Valley permafrost pergélisol DataCite Metadata Store (German National Library of Science and Technology) Mackenzie River Mackenzie Valley ENVELOPE(-126.070,-126.070,52.666,52.666)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic permafrost
soils
foundations
frost heaving
settlement
pergélisol
sol
fondation ouvrage
foisonnement par le gel
tassement
Basements and foundations
Sous-sol et fondations
spellingShingle permafrost
soils
foundations
frost heaving
settlement
pergélisol
sol
fondation ouvrage
foisonnement par le gel
tassement
Basements and foundations
Sous-sol et fondations
Pihlainen, J. A.
Building foundations on permafrost: Mackenzie Valley, N.W.T.
topic_facet permafrost
soils
foundations
frost heaving
settlement
pergélisol
sol
fondation ouvrage
foisonnement par le gel
tassement
Basements and foundations
Sous-sol et fondations
description Exploratory investigations of the foundations on permafrost at the settlements of the Mackenzie River District were undertaken during the summer of 1950. Timber mudsill foundations were the most common type used, followed by wood, steel, concrete piles, and concrete wall footings. More than half of the foundations studied showed some failure either as a result of frost heaving or settlement. Twenty-five structures were examined in detail giving building type, soil conditions and foundation type. Surface timber mudsill foundations were found unsuitable in frost susceptible soils and showed deterioration in as little as five years. Timber and concrete pad foundations showed similar failures. Recommendations for foundation selection should be preceded by a reconnaisance survey consisting of detailed information on topography, drainage, vegetation, permafrost and housing in the general area. Next, site surveys should be carried out giving details of the soil profile, groundwater level, extent and depth of the permafrost and location and size of ice lenses. Preference should be given to sites with suitable foundation materials such as gravels; to areas free from permafrost or where permafrost occurs permanently; to areas having good drainage; and to areas having non-frost susceptible soils. Lastly a cost and function study should precede the final selection of the foundation type. : Au cours de l'été de 1950, des études exploratoires ont été menées sur les fondations implantées dans le pergélisol lors d'une visite des agglomérations du district du Mackenzie. Les fondations les plus communes étaient les semelles de madriers, suivies du bois, de l'acier, de pieux de béton et de semelles de béton. Plus de la moitié des fondations examinées ont montré des signes de détérioration, soit à la suite de soulèvements dûs au gel, soit à la suite de tassements. Vingt-cinq structures ont été étudiées en dé tail en tenant compte du genre de bâtiment, des conditions du sol et du type de fondation.
format Report
author Pihlainen, J. A.
author_facet Pihlainen, J. A.
author_sort Pihlainen, J. A.
title Building foundations on permafrost: Mackenzie Valley, N.W.T.
title_short Building foundations on permafrost: Mackenzie Valley, N.W.T.
title_full Building foundations on permafrost: Mackenzie Valley, N.W.T.
title_fullStr Building foundations on permafrost: Mackenzie Valley, N.W.T.
title_full_unstemmed Building foundations on permafrost: Mackenzie Valley, N.W.T.
title_sort building foundations on permafrost: mackenzie valley, n.w.t.
publisher National Research Council of Canada. Division of Building Research
publishDate 1951
url https://dx.doi.org/10.4224/20358458
https://nrc-publications.canada.ca/eng/view/object/?id=c5f8a810-8f2f-4de7-b8d6-1d60c2f5003f
long_lat ENVELOPE(-126.070,-126.070,52.666,52.666)
geographic Mackenzie River
Mackenzie Valley
geographic_facet Mackenzie River
Mackenzie Valley
genre Ice
Mackenzie river
Mackenzie Valley
permafrost
pergélisol
genre_facet Ice
Mackenzie river
Mackenzie Valley
permafrost
pergélisol
op_doi https://doi.org/10.4224/20358458
_version_ 1766027588594040832