Organic amendment enhanced microbial nitrate immobilization with negligible denitrification nitrogen loss in an upland soil

Both soil microbial nitrate (NO₃⁻-N) immobilization and denitrification are carbon (C)-limited; however, to what extent organic C addition may increase NO₃⁻-N immobilization while stimulate denitrification nitrogen (N) loss remains unclear. Here, ¹⁵N tracing coupled with acetylene inhibition methods were used to assess the effect of adding glucose, wheat straw and peanut straw on NO₃⁻-N immobilization and denitrification under aerobic conditions in an upland soil, in which NO₃⁻-N immobilization has been previously demonstrated to be negligible. The organic C sources (5 g C kg⁻¹ soil) were added in a factorial experiment with 100, 500, and 1000 mg N kg⁻¹ soil (as K¹⁵NO₃) in a 12-d laboratory incubation. Microbial NO₃⁻-N immobilization in the 12-d incubation in the three N treatments was 5.5, 7.7, and 8.2 mg N kg⁻¹ d⁻¹, respectively, in the glucose-amended soil, 5.9, 4.2, and 2.4 mg N kg⁻¹ d⁻¹, respectively, in the wheat straw-amended soil, and 4.9, 5.1 and 4.4 mg N kg⁻¹ d⁻¹, respectively, in the peanut straw-amended soil. Therefore, under sufficient NO₃⁻-N substrate, the higher microbial NO₃⁻-N immobilization in the glucose than in the crop residue treatments was likely due to the slow decomposition of the latter that provided low available C. The ¹⁵N recovery in the N₂O + N₂ pool over the12-day incubation was <2% for all treatments, indicating negligible denitrification N loss due to low denitrification rates in the aerobic incubation in spite of increasing C availability. We conclude that external C addition can enhance microbial NO₃⁻-N immobilization without causing large N losses through denitrification. This has significant implications for reducing soil NO₃⁻-N accumulation by enhancing microbial NO₃⁻-N immobilization through increasing C inputs using organic materials and subsequently mitigating nitrate pollution of water bodies.