Nitrapyrin effectiveness in reducing nitrous oxide emissions decreases at low doses of urea in an Andosol
2021
MONGE-MUÑOZ, Mayela | URQUIAGA, Segundo | Müller, Christoph | CAMBRONERO-HEINRICHS, Juan Carlos | ZAMAN, Mohammad | CHINCHILLA-SOTO, Cristina | BORZOUEI, Azam | DAWAR, Khadim | RODRÍGUEZ-RODRÍGUEZ, Carlos E. | PÉREZ-CASTILLO, Ana Gabriela
In the tropics, frequent nitrogen (N) fertilization of grazing areas can potentially increase nitrous oxide (N₂O) emissions. The application of nitrification inhibitors has been reported as an effective management practice for potentially reducing N loss from the soil-plant system and improving N use efficiency (NUE). The aim of this study was to determine the effect of the co-application of nitrapyrin (a nitrification inhibitor, NI) and urea in a tropical Andosol on the behavior of N and the emissions of N₂O from autotrophic and heterotrophic nitrification. A greenhouse experiment was performed using a soil (pH 5.9, organic matter content 78 g kg–¹, and N 5.6 g kg–¹) sown with Cynodon nlemfuensis at 60% water-filled pore space to quantify total N₂O emissions, N₂O derived from fertilizer, soil ammonium (NH₄⁺) and nitrate (NO₃–), and NUE. The study included treatments that received deionized water only (control, CK) and two doses of ¹⁵N-enriched urea (65 (UR) and 129 mg N kg–¹ (UD)) without or with 350 g nitrapyrin for each 100 kg N (UR + NI and UD + NI). No significant differences were observed in soil NH+ content between the UR and UR + NI treatments, probably because of soil mineralization and immobilization (influenced by high soil organic matter content). Nitrapyrin application failed to maintain a stable pool of labeled NO₃⁻ due to the additional NO⁻ produced by heterotrophic nitrification, which is not effectively inhibited by nitrapyrin. After 56 d, N₂O emissions in UR (0.51 ± 0.12 mg N₂O-N kg–¹) and UR + NI (0.45 ± 0.13 mg N₂O-N kg–¹) were not significantly different; by contrast, emissions were 36.3% lower in UD + NI than in UD. It was concluded that the soil organic N mineralization and heterotrophic nitrification are the main processes of NH₄⁺ and NO₃– production. Additionally, it was found that N₂O emissions were partially a consequence of the direct oxidation of the soil's organic N via heterotrophic nitrification coupled to denitrification. Finally, the results suggest that nitrapyrin would likely exert significant mitigation on N2O emissions only if a substantial N surplus exists in soils with high organic matter content.
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