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U.S. Department of Energy
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Forest nutrient cycles as affected by climate, species composition, stand age, and intensive harvesting

Conference ·
OSTI ID:6518656
Patterns of nutrient cycling and distribution vary systematically with respect to climate, species, and stand age. Forest floor mass and nutrient content increase with stand age up to a maximum value which is determined by litterfall and decomposition rate. Litterfall and decomposition increase from cool to warm climates, but maximum forest floor weight decreases in warm climates because decomposition rates increase more rapidly than litterfall with increasing temperature. Thus, the age at which the forest floor reaches a steady state decreases from cooler to warmer climates. Maximum forest floor mass and the age at which it is reached are generally lower in deciduous forests than in coniferous forests. Deciduous forests take up, recycle, and accumulate greater amounts of nutrients per unit biomass produced than coniferous species do, but exceptions to this rule are noted. Intensive, short-rotation harvesting will cause large changes in nutrient distribution and fluxes, especially in cooler climates. Shortening rotations will accelerate nutrient outputs (both by biomass removal and leaching) and may require increased inputs (fertilization) while simultaneously reducing the maximum accumulation of nutrients in tree biomass and forest floor. Prevention of large forest floor accumulations is an especially significant change for cool, coniferous forests but is less so for warm and/or deciduous forests where forest floors naturally reach steady state early in stand development. 36 references, 5 figures.
Research Organization:
Oak Ridge National Lab., TN (USA)
DOE Contract Number:
AC05-84OR21400
OSTI ID:
6518656
Report Number(s):
CONF-8310316-1; ON: DE85000968
Country of Publication:
United States
Language:
English