¹⁵N isotope tracing of nitrogen runoff loss on red soil sloping uplands under simulated rainfall conditions

Abstract

Stable isotope 15 N tracer technique was used in combination with artificial rainfall simulation to study the influence of interflow and surface-flow on nitrogen (N) migration loss of soil-plant systems on typical red soil sloping uplands. This study also investigated the utilization efficiency of fertilizer N during different peanut plant growth stages. The results indicated that soil N loss was predominantly via interflow and erosive sediment. Fertilizer N loss during the initial growth stage was mainly through surface runoff, while that occurred as interflow increased from less than 5% to around 16% during the middle and late growth stages. The loss of fertilizer N through surface runoff, erosive sediment and interflow accounted for over 18% of the total N application. The utilization rate of fertilizer N by peanut plants was around 45% through its life cycle, and that 70% of N absorbed by this plant derived from the soil. This highlighted the importance of adopting effective methods to reduce nutrient loss through interflow and surface-flow, the need to increase the utilization rate of fertilizers, and the importance to maintain soil fertility at a relatively high level.

Nitrogen transformations from nitrogen fertilizers in soils of central and eastern Europe in changing climatic conditions

“…In extremely adverse weather conditions (high rainfall) , the loss can reach much higher values, of up to even 60-120 kg N ha -1 . In the model studies using red clay soils and 15 N isotopic techniques, it was demonstrated that, under heavy rainfalls, high nitrogen losses may occur with surface runoff, especially during the initial plant growth period, amounting even up to 18% of the nitrogen dose applied (Zheng et al, 2016). That is why, efforts are being made to reduce the intensity of this process, and to reduce the amount of nitrates in the soil environment, in view of the hazards for the ground-and surface waters.…”