Abstract
Topographic influence on gross soil N transformation was investigated along a slope on a conifer plantation forest. The half of minelarized N was immobilized and the half was left in NH4+ pool at the upper part of the slope, while 93 % of minelarized N was used for immobilization or nitrification at the lower part of the slope. From the similarity of microbial biomass and microbial C/N, microbial flora was similar among the sites. However, the gross mineralization rate was four times faster below 15 m than above 30 m. It indicated that the substrate was decomposable below 15 m. At the upper part of the slope with Oa horizon, humified organic matter with high C/N would be resistible for microbes. It resulted in relatively slow N cycling.
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© 1998 Springer Science+Business Media Dordrecht
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Tokuchi, N., Hirobe, M., Koba, K. (1998). Gross Soil N Transformations in a Coniferous Forest in Japan. In: Sassa, K. (eds) Environmental Forest Science. Forestry Sciences, vol 54. Springer, Dordrecht. https://doi.org/10.1007/978-94-011-5324-9_25
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DOI: https://doi.org/10.1007/978-94-011-5324-9_25
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