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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1990
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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 |
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Open Polar |
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Canadian Science Publishing (via Crossref) |
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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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1785564570553679872 |