SOME CHARACTERISTICS OF CRYIC ORGANIC SOILS IN NORTHERN MANITOBA
Two commonly occurring, perennially frozen, organic soils were studied, one from the south-west part of the Discontinuous Permafrost Zone and the other from the Continuous Permafrost Zone of the Hudson Bay Lowland in northern Manitoba. These soils had a characteristic domed or slightly elevated topo...
Published in: | Canadian Journal of Soil Science |
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Format: | Article in Journal/Newspaper |
Language: | English |
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Canadian Science Publishing
1972
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Online Access: | http://dx.doi.org/10.4141/cjss72-060 http://www.nrcresearchpress.com/doi/pdf/10.4141/cjss72-060 |
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crcansciencepubl:10.4141/cjss72-060 2023-12-17T10:31:24+01:00 SOME CHARACTERISTICS OF CRYIC ORGANIC SOILS IN NORTHERN MANITOBA TARNOCAI, C. 1972 http://dx.doi.org/10.4141/cjss72-060 http://www.nrcresearchpress.com/doi/pdf/10.4141/cjss72-060 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Canadian Journal of Soil Science volume 52, issue 3, page 485-496 ISSN 0008-4271 1918-1841 Soil Science journal-article 1972 crcansciencepubl https://doi.org/10.4141/cjss72-060 2023-11-19T13:38:30Z Two commonly occurring, perennially frozen, organic soils were studied, one from the south-west part of the Discontinuous Permafrost Zone and the other from the Continuous Permafrost Zone of the Hudson Bay Lowland in northern Manitoba. These soils had a characteristic domed or slightly elevated topography with a dense cover of black spruce (Picea mariana (Mill.) BSP.), Ledum groenlandicum Oeder, feathermoss, and sphagnum moss. The water content of the active layer was found to be much lower than the water (ice) content of the frozen layer. The exchangeable calcium and hydrogen and pH were higher in the frozen layer than in the active layer but no significant difference was found in the exchangeable magnesium, potassium, and sodium of the two layers. The high concentration of Ca in the frozen layer is likely due both to the transfer of soil moisture and nutrients along the thermal gradient and, as has been found previously, to the high selectivity of organic soils for calcium over magnesium and monovalent cations. Article in Journal/Newspaper Hudson Bay Ice permafrost Canadian Science Publishing (via Crossref) Hudson Bay Hudson Canadian Journal of Soil Science 52 3 485 496 |
institution |
Open Polar |
collection |
Canadian Science Publishing (via Crossref) |
op_collection_id |
crcansciencepubl |
language |
English |
topic |
Soil Science |
spellingShingle |
Soil Science TARNOCAI, C. SOME CHARACTERISTICS OF CRYIC ORGANIC SOILS IN NORTHERN MANITOBA |
topic_facet |
Soil Science |
description |
Two commonly occurring, perennially frozen, organic soils were studied, one from the south-west part of the Discontinuous Permafrost Zone and the other from the Continuous Permafrost Zone of the Hudson Bay Lowland in northern Manitoba. These soils had a characteristic domed or slightly elevated topography with a dense cover of black spruce (Picea mariana (Mill.) BSP.), Ledum groenlandicum Oeder, feathermoss, and sphagnum moss. The water content of the active layer was found to be much lower than the water (ice) content of the frozen layer. The exchangeable calcium and hydrogen and pH were higher in the frozen layer than in the active layer but no significant difference was found in the exchangeable magnesium, potassium, and sodium of the two layers. The high concentration of Ca in the frozen layer is likely due both to the transfer of soil moisture and nutrients along the thermal gradient and, as has been found previously, to the high selectivity of organic soils for calcium over magnesium and monovalent cations. |
format |
Article in Journal/Newspaper |
author |
TARNOCAI, C. |
author_facet |
TARNOCAI, C. |
author_sort |
TARNOCAI, C. |
title |
SOME CHARACTERISTICS OF CRYIC ORGANIC SOILS IN NORTHERN MANITOBA |
title_short |
SOME CHARACTERISTICS OF CRYIC ORGANIC SOILS IN NORTHERN MANITOBA |
title_full |
SOME CHARACTERISTICS OF CRYIC ORGANIC SOILS IN NORTHERN MANITOBA |
title_fullStr |
SOME CHARACTERISTICS OF CRYIC ORGANIC SOILS IN NORTHERN MANITOBA |
title_full_unstemmed |
SOME CHARACTERISTICS OF CRYIC ORGANIC SOILS IN NORTHERN MANITOBA |
title_sort |
some characteristics of cryic organic soils in northern manitoba |
publisher |
Canadian Science Publishing |
publishDate |
1972 |
url |
http://dx.doi.org/10.4141/cjss72-060 http://www.nrcresearchpress.com/doi/pdf/10.4141/cjss72-060 |
geographic |
Hudson Bay Hudson |
geographic_facet |
Hudson Bay Hudson |
genre |
Hudson Bay Ice permafrost |
genre_facet |
Hudson Bay Ice permafrost |
op_source |
Canadian Journal of Soil Science volume 52, issue 3, page 485-496 ISSN 0008-4271 1918-1841 |
op_rights |
http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining |
op_doi |
https://doi.org/10.4141/cjss72-060 |
container_title |
Canadian Journal of Soil Science |
container_volume |
52 |
container_issue |
3 |
container_start_page |
485 |
op_container_end_page |
496 |
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1785584692466024448 |