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  • Canadian Science Publishing  (2)
  • 2000-2004  (2)
  • 1975-1979
  • 1960-1964
  • 1940-1944
  • 1930-1934
  • 1
    Publication Date: 2003-02-01
    Description: In coastal forests of the Pacific Northwest, vine maple (Acer circinatum Pursh) is a common understory tree species. We studied the influence of vine maple, growing in the understory of a stand of Douglas-fir [Pseudotsuga menziesii (Mirb.) Franco] and western hemlock [Tsuga heterophylla (RAF.) Sarg.], on forest floor and mineral soil properties. Fifteen (in a 75-yr-old stand) and 12 (in a 130-yr-old stand) plots containing vine maple were compared to paired plots without the influence of vine maple. Mull humus was dominant under vine maples, while mor humus was mainly found under conifers at the 130 yr-old stand. Common to both stands in the upper mineral soil were greater mineralizable N and total exchangeable bases under vine maple. At the 75-yr-old stand, the forest floor had a higher pH and greater total exchangeable base concentration, while the mineral soil had a lower C:N ratio, greater NO3-availability and lower available P concentration and content under vine maple compared to conifers. The 130-yr-old stand had less available P content and greater concentrations of mineralizable N and exchangeable Mg in the forest floor under vine maple. Results suggest that the presence of vine maple may enhance the availability of N and exchangeable bases, but may adversely affect P availability. Key words: Vine maple, soil-plant interactions, forest floor, Acer circinatum
    Print ISSN: 0008-4271
    Electronic ISSN: 1918-1841
    Topics: Geosciences , Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
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  • 2
    Publication Date: 2003-02-01
    Description: To investigate if timber harvesting influences spatial patterns of soil micro climate, forest floor soil temperature and moisture were examined across forest-clearcut edges. Transects were sampled during the 2000 growing season across a 1-ha clearcut at a subalpine forest site in the southern interior of British Columbia, Canada. Forest floor temperature measurements were made twice, once under sunny and once under overcast conditions. Moisture status, measured under wet and dry conditions, was expressed as gravimetric and volumetric moisture content and matric potential. Wavelet analysis was used to detect and compare the location of edges in soil properties, and variance partitioning was used to examine the environmental and spatial sources of variability in temperature and moisture. Based on the wavelet analyses, the transition zone, in both temperature and moisture between forest and clearcut occurred at 7–15 m into the clearcut from the south edge and at 8–18 m into the forest from the north edge. Spatial patterns were consistent between clear and overcast conditions and wet and dry conditions. Distance from the edge was a minor source of spatial variability in temperature and moisture relative to the strong contrast between forest and clearcut conditions. The edge influences may have implications for nutrient cycling, plant available water and forest regeneration. Key words: Soil temperature, soil moisture, forest floor, subalpine forest, wavelet analysis, edge effects
    Print ISSN: 0008-4271
    Electronic ISSN: 1918-1841
    Topics: Geosciences , Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
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