Forest Science Program

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Short-term effects of forest soil compaction and site organic matter removal on mineralizable soil nitrogen in central British Columbia

Author(s) or contact(s): J.M. Kranabetter and P. Sanborn
Source: Forest Science Program
Subject: Soil Conservation, Soils
Series: LTSPS Research Note
Other details:  Published 2003. Hardcopy is available.


Mineralizable nitrogen (min-N) often correlates well with plant-available nitrogen (N) in soils, and might serve as a useful indicator of whether soils are detrimentally affected by timber harvesting practices. We examined how min-N responded to soil compaction and site organic matter removal after 1 and 5 years on three sites in central British Columbia. Mineral soil min-N was found to change after disturbance, increasing on some plots after 5 years by as much as 20 mg kg-1. Some of the lowest min-N concentrations were found after forest floor removal, but inconsistent responses across compaction treatments and sites made it difficult to generalize on the overall effects of soil disturbance. Forest floor min-N increased across all plots in the first years after tree harvest, but returned to pre-harvest levels by year 5, with no effects detected from compaction or wholetree harvest. The net change in mineral soil min-N was significantly correlated to foliar N of white spruce, but not lodgepole pine. Although levels of min-N were able to demonstrate some differences in soil productivity, its usefulness as a management tool would require a better understanding of mechanisms causing changes in min-N after disturbance.

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Updated December 17, 2008