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Please use this identifier to cite or link to this item: http://hdl.handle.net/11375/24359
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DC FieldValueLanguage
dc.contributor.advisorRadforth, N. W.-
dc.contributor.authorUsik, Lily-
dc.date.accessioned2019-05-09T18:31:22Z-
dc.date.available2019-05-09T18:31:22Z-
dc.date.issued1967-05-
dc.identifier.urihttp://hdl.handle.net/11375/24359-
dc.description.abstractThe annual earlywood, latewood and total radial growth in black spruce from organic and mineral soils of varying depths, composition, ad moisture regimes of three locations in Ontario were investigated. Growth in relation to site, temperature, and precipitation was assessed. Statistical analyses of the radial width increments expressed as percentages of trend over thirty years' growth, showed significant crossdating. Total annual and earlywood increments are correlated with mean March-April and March temperature; latewood increments are not. There is no relationship between growth and precipitation. These findings hold for trees from organic and mineral soil sites up to approximately five hundred miles apart. It is concluded that spring mean temperature is independent of site or other climatic factors, and results suggest that spring temperature indirectly controls radial growth. Primary direct controls are presumably internal, i.e. physiologic and genetic.en_US
dc.language.isoenen_US
dc.subjecttree ringsen_US
dc.subjectgrowth ringsen_US
dc.subjectblack spruceen_US
dc.subjectclimatic factoren_US
dc.titleAnalysis of Growth Rings in Black Spruce (Picea mariana) in Relation to Site and Climatic Factorsen_US
dc.title.alternativeAnalysis of Growth Rings in Black Spruceen_US
dc.typeThesisen_US
dc.contributor.departmentBiologyen_US
dc.description.degreetypeThesisen_US
dc.description.degreeDoctor of Philosophy (PhD)en_US
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