Journalartikel

Soil clay minerals: An overlooked mediator of gross N transformations in Regosolic soils of subtropical montane landscapes


AutorenlisteZhang, Bowen; Zhou, Minghua; Zhu, Bo; Xiao, Qianying; Zheng, Xunhua; Zhang, Jinbo; Müller, Christoph; Butterbach-Bahl, Klaus

Jahr der Veröffentlichung2022

ZeitschriftSoil Biology and Biochemistry

Bandnummer168

ISSN0038-0717

eISSN1879-3428

DOI Linkhttps://doi.org/10.1016/j.soilbio.2022.108612

VerlagElsevier


Abstract
Soil physiochemical and biological properties have been demonstrated as key controllers of nitrogen (N) transformation in soil; however, the roles of different soil properties in regulating the transformation processes and rates of N remain largely uncertain. Therefore, we quantified the gross transformation rate of N in soil and examined its relationships with N transformation-related functional gene abundances, clay minerals, and soil physiochemical properties across seven Regosolic soils within a subtropical montane agricultural landscape using the N-15 tracing approach. We detected substantial variations in gross N mineralization, nitrification, and immobilization rates of NH4+ and NO3- across these Regosolic soils; however, across all soils, the immobilization rate of NH4+ was relatively high to NO3- and the soil's capacity to retain NO3- remained very low. The substantial variation in the gross N transformation in soil was primarily attributed to the influences of microbial functional genes (e.g., bacteria amoA for autotrophic nitrification) and soil properties (e.g., soil pH and sand content for organic N mineralization rates). Moreover, the clay mineral content and soil type regulated rates of gross N transformation processes, including autotrophic nitrification, mineralization, and NH4+ immobilization of Regosolic soils in subtropical montane landscapes. These findings suggest that clay minerals should no longer be overlooked as mediators of gross N transformations in soil.



Zitierstile

Harvard-ZitierstilZhang, B., Zhou, M., Zhu, B., Xiao, Q., Zheng, X., Zhang, J., et al. (2022) Soil clay minerals: An overlooked mediator of gross N transformations in Regosolic soils of subtropical montane landscapes, Soil Biology and Biochemistry, 168, Article 108612. https://doi.org/10.1016/j.soilbio.2022.108612

APA-ZitierstilZhang, B., Zhou, M., Zhu, B., Xiao, Q., Zheng, X., Zhang, J., Müller, C., & Butterbach-Bahl, K. (2022). Soil clay minerals: An overlooked mediator of gross N transformations in Regosolic soils of subtropical montane landscapes. Soil Biology and Biochemistry. 168, Article 108612. https://doi.org/10.1016/j.soilbio.2022.108612


Zuletzt aktualisiert 2025-21-05 um 17:39