Modeling impacts of N sources on N2O emissions in long-term crop rotation system in Brazil’s Cerrado using DNDCv.CAN

• DNDCv.CAN model fairly simulated the N 2 O emissions in 10-yr crop rotation in Brazil • N application increased N 2 O emissions, in which the model had similar pattern • DNDCv.CAN effectively predicted higher NH 3 losses from UR than other N sources • Soil NH 4 + and NO 3 - , WFPS and grain yield were acceptably simulated by DNDCvCAN • The WFPS dynamics for tropical soils may need further adjustments in the model Predicting N 2 O emissions can help identify crop production practices and environmental conditions for mitigation. The objectives were to calibrate and validate the DeNitrification-DeComposition (DNDCv.CAN) model to simulate N 2 O emission in crop rotation (CR) systems in Brazil’s Cerrado biome, using different N fertilizer sources. Field data were obtained from a CR experiment with maize and common beans cultivated under no-till for 10 years. Treatments were: Zero-N, calcium ammonium nitrate (CAN), urea (UR), and ammonium sulfate (AS), with 5 replicates. Measured data including N 2 O fluxes, NH 3 volatilization, soil NH 4 + and NO 3 - , water-filled pore space (WFPS), and grain yields were used to calibrate and validate the DNDCv.CAN. The model acceptably captured the daily N 2 O emissions associated with different N sources, although episodic peaks were over or under-predicted. Correlation coefficient was 0.62 during calibration, with a mean absolute error of 17 g N 2 O-N ha -1 day -1 , close to average measured (18 g ha -1 d -1 ), and simulated (17 g ha -1 day -1 ) emissions. Accumulated measured N 2 O-N emissions were 1.19, 4.38, 3.17, and 2.56 kg N 2 O-N ha -1 for Zero-N, CAN, UR, and AS, respectively, whereas the simulated were 1.13, 3.44, 2.24, and 3.32 kg N 2 O-N ha -1 . The NH 3 , NH 4 + , NO 3 - , WFPS, and yields were also fairly simulated. Soil hydrologic parameters were adjusted in the model using a built in pedotransfer function to improve the simulations, which should be further investigated. The DNDCv.CAN effectively simulated cumulative N 2 O emissions from different N sources applied to CR under tropical conditions, making it valuable for evaluating potential emissions and mitigation strategies.

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Publication Details

Journal
Ecological Modelling
Published
2026-02-04
DOI
https://doi.org/10.1016/j.ecolmodel.2026.111513
Primary Topic
Soil Carbon and Nitrogen Dynamics
Type
article
Field-Weighted Citation Impact
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article

Modeling impacts of N sources on N2O emissions in long-term crop rotation system in Brazil’s Cerrado using DNDCv.CAN

Bruno José Rodrígues Alves, Cláudia Pozzi Jantalia, B. E. Madari, Johnny Rodrigues Soares et al.
Ecological Modelling
Soil Carbon and Nitrogen Dynamics
article

Modeling impacts of N sources on N2O emissions in long-term crop rotation system in Brazil’s Cerrado using DNDCv.CAN

Bruno José Rodrígues Alves, Cláudia Pozzi Jantalia, B. E. Madari, Johnny Rodrigues Soares, C. F. Drury, Ward Smith, Maria da Conceição Santana Carvalho, Brian Grant, Antônio Carlos Reis de Freitas
article en

Abstract

• DNDCv.CAN model fairly simulated the N 2 O emissions in 10-yr crop rotation in Brazil • N application increased N 2 O emissions, in which the model had similar pattern • DNDCv.CAN effectively predicted higher NH 3 losses from UR than other N sources • Soil NH 4 + and NO 3 - , WFPS and grain yield were acceptably simulated by DNDCvCAN • The WFPS dynamics for tropical soils may need further adjustments in the model Predicting N 2 O emissions can help identify crop production practices and environmental conditions for mitigation. The objectives were to calibrate and validate the DeNitrification-DeComposition (DNDCv.CAN) model to simulate N 2 O emission in crop rotation (CR) systems in Brazil’s Cerrado biome, using different N fertilizer sources. Field data were obtained from a CR experiment with maize and common beans cultivated under no-till for 10 years. Treatments were: Zero-N, calcium ammonium nitrate (CAN), urea (UR), and ammonium sulfate (AS), with 5 replicates. Measured data including N 2 O fluxes, NH 3 volatilization, soil NH 4 + and NO 3 - , water-filled pore space (WFPS), and grain yields were used to calibrate and validate the DNDCv.CAN. The model acceptably captured the daily N 2 O emissions associated with different N sources, although episodic peaks were over or under-predicted. Correlation coefficient was 0.62 during calibration, with a mean absolute error of 17 g N 2 O-N ha -1 day -1 , close to average measured (18 g ha -1 d -1 ), and simulated (17 g ha -1 day -1 ) emissions. Accumulated measured N 2 O-N emissions were 1.19, 4.38, 3.17, and 2.56 kg N 2 O-N ha -1 for Zero-N, CAN, UR, and AS, respectively, whereas the simulated were 1.13, 3.44, 2.24, and 3.32 kg N 2 O-N ha -1 . The NH 3 , NH 4 + , NO 3 - , WFPS, and yields were also fairly simulated. Soil hydrologic parameters were adjusted in the model using a built in pedotransfer function to improve the simulations, which should be further investigated. The DNDCv.CAN effectively simulated cumulative N 2 O emissions from different N sources applied to CR under tropical conditions, making it valuable for evaluating potential emissions and mitigation strategies.

Ecological ModellingVol. 515
Agriculture and Agri-Food Canada (CA), Brazilian Agricultural Research Corporation (BR), Instituto Federal Goiano (BR)
Life in Land
Openalex Percentile: Top 67%
Soil Carbon and Nitrogen Dynamics
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