Journal article

Microbial ammonium immobilization promoted soil nitrogen retention under high moisture conditions in intensively managed fluvo-aquic soils


Authors listWang, Hui; Yan, Zhifeng; Chen, Zengming; Song, Xiaotong; Zhang, Jinbo; Li, Si-Liang; Müller, Christoph; Ju, Xiaotang; Zhu-Barker, Xia

Publication year2025

Pages641-651

JournalBiology and Fertility of Soils

Volume number61

ISSN0178-2762

eISSN1432-0789

DOI Linkhttps://doi.org/10.1007/s00374-024-01831-y

PublisherSpringer


Abstract
Quantifying the gross rates of individual nitrogen (N) processes is critical for understanding the availability, retention and loss of N and its eco-environmental impacts in agricultural ecosystems. Here, we carried out a N-15 tracing study to quantify the influence of soil moisture on the gross rates of ten different N processes in two intensively managed fluvo-aquic soils. Results showed that the gross N mineralization rates were insensitive to changes in soil moisture, ranging from 40 to 120% water-filled pore space (WFPS). Contrarily, the gross ammonium (NH4+) immobilization rates increased exponentially with elevated soil moisture. Specifically, under high soil moisture conditions (i.e., 90-120%WFPS), the gross NH4+ immobilization rates (4.04 +/- 0.83 and 0.88 +/- 0.28 mg N kg(- 1)d(- 1) for the two soils, respectively) were nearly four times higher than those under medium or low moisture conditions (i.e., 40-80%WFPS). Meanwhile, the high WFPS reduced the gross autotrophic nitrification rates (5.92 +/- 2.15 and 12.31 +/- 3.83 mg-N kg(- 1)d(- 1) for the two soils, respectively) to only one-third to one-half of those that were observed under medium or low WFPS. By contrast, the rates of nitrate (NO3-) immobilization increased in one soil whereas they decreased in another under high moisture conditions, and the other N processes (including heterotrophic nitrification and dissimilatory nitrate reduction to ammonium (DNRA)) were negligible throughout the different WFPS. Overall, our results suggest that under highly saturated conditions, the increase in microbial NH4+ immobilization and decrease in autotrophic nitrification are critical for N retention in the fluvo-aquic soils. These findings provide valuable insights into potential alterations in soil N retention or loss under future climate change scenarios, where more intensive irrigation and extreme rainfall events are anticipated.



Citation Styles

Harvard Citation styleWang, H., Yan, Z., Chen, Z., Song, X., Zhang, J., Li, S., et al. (2025) Microbial ammonium immobilization promoted soil nitrogen retention under high moisture conditions in intensively managed fluvo-aquic soils, Biology and Fertility of Soils, 61, pp. 641-651. https://doi.org/10.1007/s00374-024-01831-y

APA Citation styleWang, H., Yan, Z., Chen, Z., Song, X., Zhang, J., Li, S., Müller, C., Ju, X., & Zhu-Barker, X. (2025). Microbial ammonium immobilization promoted soil nitrogen retention under high moisture conditions in intensively managed fluvo-aquic soils. Biology and Fertility of Soils. 61, 641-651. https://doi.org/10.1007/s00374-024-01831-y


Last updated on 2025-25-06 at 14:16