Ammonium-based fertilizers (urea, anhydrous NH 3 , (NH 4 ) 2 SO 4 and NH 4 NO 3 ) comprise the most commonly used forms of N applied in agriculture. While many soils can retain an abundance of cations such as NH + 4 , due to the typically negative charges on soil particle surfaces, large amounts of N are lost via the nitrification of NH 3 to NO − 3 , followed by leaching and runoff of this poorly soil-bound anion. For this reason, several strategies have been put forward to curb agricultural N losses, including the use of synthetic nitrification inhibitors (Coskun et al., 2017;Kawakami et al., 2013). The nitrification inhibitors contribute to increasing the supply of N in the form of NH + 4 , one of the forms of N absorbed by plants, in addition to NO − 3 . For example, three days after soil fertilization with urea (225 kg/ha of N), the NH + 4 in the soil solution was 0.44 and 1.74 mmol/L, without and with nitrification inhibitor, respectively (Kirschke et al., 2019).In relation to NO − 3 , NH + 4 has the advantage of a lower energy cost necessary to be incorporated into organic compounds, which can lead to increased crop yields. However, NH + 4 has the disadvantage of being toxic depending on its concentration in the culture medium and the tolerance of the plant (Salsac et al., 1987). Among the consequences of NH + 4 toxicity, the decrease in the accumulation of cations such as K, Ca and