Directionality of compression wood in balsam fir wave forest trees

Wind is often cited as one of the main causes of compression wood formation. While many papers have alluded to direction of compression wood, this paper provides a detailed circular statistical analysis of the angular distribution of compression-wood zones in balsam fir trees. Discs were sampled fro...

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Published in:Canadian Journal of Forest Research
Main Author: Robertson, Alexander
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 1990
Subjects:
Online Access:http://dx.doi.org/10.1139/x90-152
http://www.nrcresearchpress.com/doi/pdf/10.1139/x90-152
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spelling crcansciencepubl:10.1139/x90-152 2023-12-17T10:44:56+01:00 Directionality of compression wood in balsam fir wave forest trees Robertson, Alexander 1990 http://dx.doi.org/10.1139/x90-152 http://www.nrcresearchpress.com/doi/pdf/10.1139/x90-152 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Canadian Journal of Forest Research volume 20, issue 8, page 1143-1148 ISSN 0045-5067 1208-6037 Ecology Forestry Global and Planetary Change journal-article 1990 crcansciencepubl https://doi.org/10.1139/x90-152 2023-11-19T13:39:39Z Wind is often cited as one of the main causes of compression wood formation. While many papers have alluded to direction of compression wood, this paper provides a detailed circular statistical analysis of the angular distribution of compression-wood zones in balsam fir trees. Discs were sampled from trees in a balsam fir (Abiesbalsamea (L.) Mill.) wave forest in northwestern Newfoundland, from sapling to mature stages. The directionality, with respect to compass bearing, of compression-wood zones in basal discs was found to be initially randomly distributed around the pith, becoming unidirectional towards the northeast at about 10 mm from the pith. Random circular distribution of compression-wood zones mostly within 10 mm of the pith is interpreted as resulting from a combination of environmental perturbations, such as glaze and rain loading, and asymmetric crown growth due to competition. Because of the very high density of immature stands, wind turbulence is not expected to be a major factor stimulating compression wood in saplings. The role of snow loading, which causes bending of stems for long periods during the winter (dormant season), is uncertain. In older trees, i.e., beyond approximately 10 mm from the pith, compression wood gradually becomes directional towards the northeast, indicating that prevailing southwesterly winds are mainly responsible for compression-wood formation. Article in Journal/Newspaper Newfoundland Canadian Science Publishing (via Crossref) Canadian Journal of Forest Research 20 8 1143 1148
institution Open Polar
collection Canadian Science Publishing (via Crossref)
op_collection_id crcansciencepubl
language English
topic Ecology
Forestry
Global and Planetary Change
spellingShingle Ecology
Forestry
Global and Planetary Change
Robertson, Alexander
Directionality of compression wood in balsam fir wave forest trees
topic_facet Ecology
Forestry
Global and Planetary Change
description Wind is often cited as one of the main causes of compression wood formation. While many papers have alluded to direction of compression wood, this paper provides a detailed circular statistical analysis of the angular distribution of compression-wood zones in balsam fir trees. Discs were sampled from trees in a balsam fir (Abiesbalsamea (L.) Mill.) wave forest in northwestern Newfoundland, from sapling to mature stages. The directionality, with respect to compass bearing, of compression-wood zones in basal discs was found to be initially randomly distributed around the pith, becoming unidirectional towards the northeast at about 10 mm from the pith. Random circular distribution of compression-wood zones mostly within 10 mm of the pith is interpreted as resulting from a combination of environmental perturbations, such as glaze and rain loading, and asymmetric crown growth due to competition. Because of the very high density of immature stands, wind turbulence is not expected to be a major factor stimulating compression wood in saplings. The role of snow loading, which causes bending of stems for long periods during the winter (dormant season), is uncertain. In older trees, i.e., beyond approximately 10 mm from the pith, compression wood gradually becomes directional towards the northeast, indicating that prevailing southwesterly winds are mainly responsible for compression-wood formation.
format Article in Journal/Newspaper
author Robertson, Alexander
author_facet Robertson, Alexander
author_sort Robertson, Alexander
title Directionality of compression wood in balsam fir wave forest trees
title_short Directionality of compression wood in balsam fir wave forest trees
title_full Directionality of compression wood in balsam fir wave forest trees
title_fullStr Directionality of compression wood in balsam fir wave forest trees
title_full_unstemmed Directionality of compression wood in balsam fir wave forest trees
title_sort directionality of compression wood in balsam fir wave forest trees
publisher Canadian Science Publishing
publishDate 1990
url http://dx.doi.org/10.1139/x90-152
http://www.nrcresearchpress.com/doi/pdf/10.1139/x90-152
genre Newfoundland
genre_facet Newfoundland
op_source Canadian Journal of Forest Research
volume 20, issue 8, page 1143-1148
ISSN 0045-5067 1208-6037
op_rights http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining
op_doi https://doi.org/10.1139/x90-152
container_title Canadian Journal of Forest Research
container_volume 20
container_issue 8
container_start_page 1143
op_container_end_page 1148
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