Permafrost investigations at Aklavik, 1953: drilling and sampling

The Aklavik investigations were located at the site of a proposed ten-room school and an eight-room teacherage on the northern end of the settlement. The site was low lying and covered with an organic layer about 12 inches thick. Fifteen bore holes were drilled; three exploratory and twelve for ther...

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Main Authors: Pihlainen, J. A., Johnston, G. H.
Format: Report
Language:English
Published: National Research Council of Canada 1954
Subjects:
sol
Ice
Online Access:https://doi.org/10.4224/20358965
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spelling ftnrccanada:oai:cisti-icist.nrc-cnrc.ca:cistinparc:20358965 2023-05-15T13:07:57+02:00 Permafrost investigations at Aklavik, 1953: drilling and sampling Pihlainen, J. A. Johnston, G. H. 1954-01 text 47 p. https://doi.org/10.4224/20358965 https://nrc-publications.canada.ca/eng/view/ft/?id=d37017c1-9e65-4673-b83b-1ed528c16803 https://nrc-publications.canada.ca/eng/view/object/?id=d37017c1-9e65-4673-b83b-1ed528c16803 https://nrc-publications.canada.ca/fra/voir/objet/?id=d37017c1-9e65-4673-b83b-1ed528c16803 eng eng National Research Council of Canada Technical Paper (National Research Council of Canada. Division of Building Research); no. DBR-TP-16, Publication date: 1954-01 doi:10.4224/20358965 open access permafrost pergélisol soils sol soil investigation reconnaissance du sol soil tests essai de sol site surveying planimétrie temperature température sol (terre) technical report 1954 ftnrccanada https://doi.org/10.4224/20358965 2022-07-30T23:01:07Z The Aklavik investigations were located at the site of a proposed ten-room school and an eight-room teacherage on the northern end of the settlement. The site was low lying and covered with an organic layer about 12 inches thick. Fifteen bore holes were drilled; three exploratory and twelve for thermocouple installations. Cuttings at the cylindrical core bit face were carried away with the wash water; the frozen core was retained inside. Core recovery averaged around 60%. Poor core recovery was directly attributable to unsatisfactory wash water systems. Soil constituents of the permafrost were described using the Unified Classification System, although it lacked proper descriptions for organic soils. The ice in the permafrost cores was described according to the Frozen Soil Classification System of the U.S. Corps of Engineers. Simple classification tests involved moisture content, field density, specific gravity, grain size, distribution and Atterberg limits. Volume of ice was estimated visually. Grain size distribution determinations showed that almost all soils were finer than the No. 60 sieve. Plastic soils were scarce at Aklavik. Average values were 38.0 and 28.4% while the plasticity index averaged 9.6%. All moisture contents of the soils investigated were above the liquid limit. Present methods of reporting organic matter are based on a weight basis; hence the rather large organic matter contents appear relatively small. Les études réalisées à Aklavik ont porté sur le site prévu pour une école de dix pièces et une résidence d'enseignants de huit pièces à la limite nord de la localité. Le site en question est situé sur un terrain bas recouvert d'une couche organique l'environ 12 pouces d'épaisseur. Quinze trous de sondage ont été forés, dont trois pour l'exploration et douze pour l'installation de thermocouples. Les déblais accumulés à la surface des carottiers cylindriques ont été é vacués par l'eau de lavage et la corotte gelée a été conservé e à l'intérieur. Le taux de récupération des carottes a été ... Report Aklavik Ice permafrost pergélisol National Research Council Canada: NRC Publications Archive Aklavik ENVELOPE(-135.011,-135.011,68.219,68.219)
institution Open Polar
collection National Research Council Canada: NRC Publications Archive
op_collection_id ftnrccanada
language English
topic permafrost
pergélisol
soils
sol
soil investigation
reconnaissance du sol
soil tests
essai de sol
site surveying
planimétrie
temperature
température
sol (terre)
spellingShingle permafrost
pergélisol
soils
sol
soil investigation
reconnaissance du sol
soil tests
essai de sol
site surveying
planimétrie
temperature
température
sol (terre)
Pihlainen, J. A.
Johnston, G. H.
Permafrost investigations at Aklavik, 1953: drilling and sampling
topic_facet permafrost
pergélisol
soils
sol
soil investigation
reconnaissance du sol
soil tests
essai de sol
site surveying
planimétrie
temperature
température
sol (terre)
description The Aklavik investigations were located at the site of a proposed ten-room school and an eight-room teacherage on the northern end of the settlement. The site was low lying and covered with an organic layer about 12 inches thick. Fifteen bore holes were drilled; three exploratory and twelve for thermocouple installations. Cuttings at the cylindrical core bit face were carried away with the wash water; the frozen core was retained inside. Core recovery averaged around 60%. Poor core recovery was directly attributable to unsatisfactory wash water systems. Soil constituents of the permafrost were described using the Unified Classification System, although it lacked proper descriptions for organic soils. The ice in the permafrost cores was described according to the Frozen Soil Classification System of the U.S. Corps of Engineers. Simple classification tests involved moisture content, field density, specific gravity, grain size, distribution and Atterberg limits. Volume of ice was estimated visually. Grain size distribution determinations showed that almost all soils were finer than the No. 60 sieve. Plastic soils were scarce at Aklavik. Average values were 38.0 and 28.4% while the plasticity index averaged 9.6%. All moisture contents of the soils investigated were above the liquid limit. Present methods of reporting organic matter are based on a weight basis; hence the rather large organic matter contents appear relatively small. Les études réalisées à Aklavik ont porté sur le site prévu pour une école de dix pièces et une résidence d'enseignants de huit pièces à la limite nord de la localité. Le site en question est situé sur un terrain bas recouvert d'une couche organique l'environ 12 pouces d'épaisseur. Quinze trous de sondage ont été forés, dont trois pour l'exploration et douze pour l'installation de thermocouples. Les déblais accumulés à la surface des carottiers cylindriques ont été é vacués par l'eau de lavage et la corotte gelée a été conservé e à l'intérieur. Le taux de récupération des carottes a été ...
format Report
author Pihlainen, J. A.
Johnston, G. H.
author_facet Pihlainen, J. A.
Johnston, G. H.
author_sort Pihlainen, J. A.
title Permafrost investigations at Aklavik, 1953: drilling and sampling
title_short Permafrost investigations at Aklavik, 1953: drilling and sampling
title_full Permafrost investigations at Aklavik, 1953: drilling and sampling
title_fullStr Permafrost investigations at Aklavik, 1953: drilling and sampling
title_full_unstemmed Permafrost investigations at Aklavik, 1953: drilling and sampling
title_sort permafrost investigations at aklavik, 1953: drilling and sampling
publisher National Research Council of Canada
publishDate 1954
url https://doi.org/10.4224/20358965
https://nrc-publications.canada.ca/eng/view/ft/?id=d37017c1-9e65-4673-b83b-1ed528c16803
https://nrc-publications.canada.ca/eng/view/object/?id=d37017c1-9e65-4673-b83b-1ed528c16803
https://nrc-publications.canada.ca/fra/voir/objet/?id=d37017c1-9e65-4673-b83b-1ed528c16803
long_lat ENVELOPE(-135.011,-135.011,68.219,68.219)
geographic Aklavik
geographic_facet Aklavik
genre Aklavik
Ice
permafrost
pergélisol
genre_facet Aklavik
Ice
permafrost
pergélisol
op_relation Technical Paper (National Research Council of Canada. Division of Building Research); no. DBR-TP-16, Publication date: 1954-01
doi:10.4224/20358965
op_rights open access
op_doi https://doi.org/10.4224/20358965
_version_ 1766069989998067712