Mineral soil carbon and nitrogen still low three decades following clearcut harvesting in a typical Acadian Forest stand
Intensive forest management practices can alter forest soil organic matter (SOM) storage (kgCha−1) due to changes in the environmental variables that control SOM cycling and stability. Here we investigate whether SOM losses are observed three decades following clearcut harvesting in a temperate fore...
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Published in | Geoderma Vol. 214-215; pp. 62 - 69 |
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Main Authors | , , |
Format | Journal Article |
Language | English |
Published |
Amsterdam
Elsevier B.V
01.02.2014
Elsevier |
Subjects | |
Online Access | Get full text |
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Summary: | Intensive forest management practices can alter forest soil organic matter (SOM) storage (kgCha−1) due to changes in the environmental variables that control SOM cycling and stability. Here we investigate whether SOM losses are observed three decades following clearcut harvesting in a temperate forest ecosystem that includes the deep mineral soil (to a depth of 50cm). We compared SOM stored as carbon (C) and nitrogen (N) in paired (35-year-old; 110-year-old reference) Acadian Forest sites that differed only in their time since harvest. We found lower mineral soil carbon (C) and nitrogen (N) storage (27% and 26% respectively), and lower C and N concentrations at the 35-year-old site compared with the 110-year-old reference site. Isotopic compositions of C and N through the soil profile did not provide insight into the dominant mechanisms driving SOM losses at the 35-year-old site in this study. This is the second study to document decreases in mineral soil C and N storage in a red spruce forest within the Acadian Forest Region three decades following clearcut harvesting.
•Decrease in mineral SOM was observed 3 decades following clearcut harvesting.•Losses of soil C and N may not be evident without inclusion of deep soil.•Mineral soil pool is more susceptible to harvesting impacts than previously thought. |
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Bibliography: | ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 23 |
ISSN: | 0016-7061 1872-6259 |
DOI: | 10.1016/j.geoderma.2013.10.002 |