Journalartikel

Heterotrophic nitrification is the predominant NO3 − production pathway in acid coniferous forest soil in subtropical China


AutorenlisteZhang, YC; Zhang, JB; Meng, TZ; Zhu, TB; Müller, C; Cai, ZC

Jahr der Veröffentlichung2013

Seiten955-957

ZeitschriftBiology and Fertility of Soils

Bandnummer49

Heftnummer7

ISSN0178-2762

eISSN1432-0789

DOI Linkhttps://doi.org/10.1007/s00374-012-0772-4

VerlagSpringer


Abstract
To date, occurrence and stimulation of different nitrification pathways in acidic soils remains unclear. Laboratory incubation experiments, using the acetylene inhibition and N-15 tracing methods, were conducted to study the relative importance of heterotrophic and autotrophic nitrification in two acid soils (arable (AR) and coniferous forest) in subtropical China, and to verify the reliability of the N-15 tracing model. The gross rate of autotrophic nitrification was 2.28 mg kg(-1) day(-1), while that of the heterotrophic nitrification (0.01 mg kg(-1) day(-1)) was negligible in the AR soil. On the contrary, the gross rate of autotrophic nitrification was very low (0.05 mg kg(-1) day(-1)) and the heterotrophic nitrification (0.98 mg kg(-1) day(-1)) was the predominant NO3 (-) production pathway accounting for more than 95 % of the total nitrification in the coniferous forest soil. Our results showed that the N-15 tracing model was reliable when used to study soil N transformation in acid subtropical soils.



Zitierstile

Harvard-ZitierstilZhang, Y., Zhang, J., Meng, T., Zhu, T., Müller, C. and Cai, Z. (2013) Heterotrophic nitrification is the predominant NO3 − production pathway in acid coniferous forest soil in subtropical China, Biology and Fertility of Soils, 49(7), pp. 955-957. https://doi.org/10.1007/s00374-012-0772-4

APA-ZitierstilZhang, Y., Zhang, J., Meng, T., Zhu, T., Müller, C., & Cai, Z. (2013). Heterotrophic nitrification is the predominant NO3 − production pathway in acid coniferous forest soil in subtropical China. Biology and Fertility of Soils. 49(7), 955-957. https://doi.org/10.1007/s00374-012-0772-4


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