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dc.creatorMonge Muñoz, Mayela María
dc.creatorUrquiaga Caballero, Segundo Sacramento
dc.creatorMüller, Christoph
dc.creatorCambronero Heinrichs, Juan Carlos
dc.creatorZaman, Mohammad
dc.creatorChinchilla Soto, Isabel Cristina
dc.creatorBorzouei, Azam
dc.creatorDawar, Khadim
dc.creatorRodríguez Rodríguez, Carlos E.
dc.creatorPérez Castillo, Ana Gabriela
dc.date.accessioned2021-10-05T20:57:48Z
dc.date.available2021-10-05T20:57:48Z
dc.date.issued2021
dc.identifier.citationhttps://www.sciencedirect.com/science/article/pii/S1002016020600728?via%3Dihub
dc.identifier.issn1002-0160
dc.identifier.urihttps://hdl.handle.net/10669/84509
dc.description.abstractIn 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.es_ES
dc.description.sponsorshipUniversidad de Costa Rica/[802-B7-505]/UCR/Costa Ricaes_ES
dc.description.sponsorshipOrganismo Internacional de Energía Atómica/[No. CRP DI.50.16]/IAEA/Estados Unidoses_ES
dc.language.isoenges_ES
dc.sourcePedosphere, vol.31(2), pp.303-313es_ES
dc.subjectAndosoles_ES
dc.subjectNitrapyrines_ES
dc.subjectNitrous oxidees_ES
dc.subjectAutotrophic nitrificationes_ES
dc.subjectHeterotrophic nitrificationes_ES
dc.subjectMinerales_ES
dc.subjectMineral Nes_ES
dc.subjectNitrification inhibitores_ES
dc.subjectTropical grasses_ES
dc.titleNitrapyrin effectiveness in reducing nitrous oxide emissions decreases at low doses of urea in an Andosoles_ES
dc.typeartículo original
dc.identifier.doi10.1016/S1002-0160(20)60072-8
dc.description.procedenceUCR::Vicerrectoría de Investigación::Unidades de Investigación::Ciencias Básicas::Centro en Investigación en Contaminación Ambiental (CICA)es_ES
dc.identifier.codproyecto802-B7-505


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