Abstract

ABSTRACT Novel fertilizer stabilization technologies are needed to decrease ammonia (NH3-N) losses and increase nitrogen use efficiency. Duromide + NBPT is a new technology that combines two molecules, Duromide and NBPT, whose propose is to increase the efficiency of the urease inhibitor NBPT in reducing NH3-N loss from urea. Preliminary results showed that Duromide + NBPT can be a more effective product than just NBPT, particularly under low soil pH and high-temperature conditions. This study aimed to compare the effects [...]

Highlights

  • Nitrogen (N) is the nutrient required in the greatest amounts and the most limiting factor for plant growth (Souza and Fernandes, 2018)

  • The maximum cumulative losses (α) of NH3-N, according to the adjusted model, were 11.2, 7.6, 5.1, 4.2, 3.6, and 2.7 kg ha-1 in plots treated with Ur90, Ur90-NBPT, Ur90-Duromide + NBPT, Ur45, Ur45-NBPT, and Ur45-Duromide + NBPT, respectively (Table 2)

  • Urea treated with the stabilizers NBPT and Duromide + NBPT reduced NH3-N losses by 14.8 and 35.3 %, respectively, compared with conventional urea at a dose of 45 kg ha-1 of N and by 31.9 and 54.2 %, respectively, compared with conventional urea at 90 kg ha-1 of N

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Summary

Introduction

Nitrogen (N) is the nutrient required in the greatest amounts and the most limiting factor for plant growth (Souza and Fernandes, 2018). Urea [CO(NH2)2] is the most used N fertilizer worldwide, with a total production of 183.2 Mt yr-1, supplying 53.3 % of the current N demand (IFA, 2019). When broadcast onto the soil surface, urea is highly susceptible to losses by leaching, denitrification, and ammonia (NH3-N) volatilization (Gillette et al, 2017). Urea is hydrolyzed by the action of ureases, resulting in the production of ammonium (NH4+) and carbon dioxide (CO2), as demonstrated by the reaction CO(NH2)2 + 2H+ + 2H2O → 2NH4+ + H2O + CO2 (Cantarella, 2007). Because urea hydrolysis consumes protons (H+), the reaction results in increased pH around fertilizer granules, shifting the equilibrium toward the formation of NH3-N, which is subsequently lost to the atmosphere in its gaseous form (NH3) (Rochette et al, 2009; Cantarella et al, 2018)

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