Geoderma (Jul 2025)

Biochar stimulates nitrogen loss in anoxic soil through ammonium oxidation coupled with iron reduction

  • Bo Yi,
  • Qichun Zhang,
  • Steven J. Hall,
  • Xiang Zou,
  • Wenjuan Huang,
  • Wenjuan Yu,
  • Qinsi He,
  • Peiyu Cao,
  • Jing Hou,
  • Jiuwei Song,
  • Hongjie Di,
  • Chaoqun Lu

DOI
https://doi.org/10.1016/j.geoderma.2025.117372
Journal volume & issue
Vol. 459
p. 117372

Abstract

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Anaerobic ammonium oxidation coupled with iron (Fe) reduction, known as Feammox, is an important nitrogen (N)-cycling pathway in anoxic soils. Biochar, widely employed as a soil amendment, has been reported to influence N dynamics through its redox-active moieties, but the effects on Feammox of biochar produced with different pyrolysis temperatures remain poorly understood. We conducted a slurry incubation in rice-paddy soil with 15N-isotope tracing to examine the impact of biochar pyrolyzed at 300 °C and 600 °C on Feammox under different Fe availability conditions (addition of ferrihydrite, goethite, or no Fe). Biochar pyrolysis temperature and Fe availability impacted rates of Feammox. Specifically, adding biochar pyrolyzed at 600 °C to soil at a 2 % mass ratio stimulated N loss through Feammox by 0.03 to 0.07 μg N g−1 soil d-1, likely by facilitating electron transfer via its surface redox-active moieties. Feammox was highly correlated with Fe reduction despite contributing only a small fraction to overall Fe reduction. Feammox rates were greatest with ferrihydrite addition and lowest with no Fe addition, and correlated with the abundance of a known Feammox bacterium (Acidimicrobiaceae bacterium A6). In contrast, biochar pyrolyzed at 300 °C did not stimulate Feammox, likely due to a lack of electron shuttling capacity. Overall, our findings highlight a stimulation effect of biochar pyrolyzed at high temperature on promoting N loss as dinitrogen, underscoring its potential utility for environmentally-friendly removal of excess N from anoxic soil.

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