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The effects of urine nitrogen application rate on nitrogen transformations in grassland soils
The Journal of Agricultural Science ( IF 2 ) Pub Date : 2019-11-14 , DOI: 10.1017/s0021859619000832 C. Somers , N. T. Girkin , B. Rippey , G. J. Lanigan , K. G. Richards
The Journal of Agricultural Science ( IF 2 ) Pub Date : 2019-11-14 , DOI: 10.1017/s0021859619000832 C. Somers , N. T. Girkin , B. Rippey , G. J. Lanigan , K. G. Richards
Urine is a critical nitrogen (N) input in temperate grazed grasslands and can drive substantial nitrous oxide (N2 O) production in soils. However, it remains unclear how differences in the N input rate affect N2 O fluxes and vary between different grassland soils. The effect of increasing urine N application on ammonium (NH4 + ), nitrite (NO2 − ) and nitrate (NO3 − ) concentrations and N2 O production was tested in two grassland soils, a free-draining loam and an imperfectly drained sandy-loam. It was hypothesized that high-urine N application rates would lead to ammonia/ammonium (NH3 /NH4 + ) accumulation influencing N transformation rates and N2 O production which differ between grassland soils. Fresh cattle urine was applied at rates equivalent to 300 and 1000 kg N/ha in an aerobic incubation experiment. Soils were destructively sampled over 80 days to measure changes in inorganic-N and pH. The higher N addition rate was associated with elevated NH3 concentrations up to day 35 in soils, probably inhibiting NO2 − to NO3 − reduction. In contrast, there was no inhibition of nitrification in the 300 kg N/ha treatment. Cumulative N2 O fluxes were greatest from the 300 kg N/ha treatment for the loam soil, but were greater for the sandy-loam under the 1000 kg N/ha treatment. The results also show that differences in soil properties, in particular carbon availability, can be important in regulating N transformation and N2 O production. Collectively, these results demonstrate the proposed mechanism of nitrification inhibition at high-N input rates, driven by either high NH3 /NH4 and/or increased levels of NH4 HCO3 from urea hydrolysis.
中文翻译:
尿氮施用量对草地土壤氮素转化的影响
尿液是温带放牧草原的关键氮 (N) 输入,可驱动大量一氧化二氮 (N2 O) 在土壤中生产。然而,目前尚不清楚 N 输入速率的差异如何影响 N2 O 通量和不同草地土壤之间的变化。增加尿氮施用量对铵(NH)的影响4 + ), 亚硝酸盐 (NO2 - ) 和硝酸盐 (NO3 - ) 浓度和 N2 O 产量在两种草地土壤中进行了测试,一种是排水良好的壤土,另一种是排水不完全的沙壤土。假设高尿氮施用率会导致氨/铵(NH3 /NH4 + ) 累积影响 N 转化率和 N2 草地土壤之间的 O 产量不同。在好氧孵化实验中,新鲜牛尿的施用量相当于 300 和 1000 kg N/ha。在 80 天内对土壤进行破坏性采样,以测量无机氮和 pH 值的变化。较高的 N 添加率与 NH 升高有关3 土壤中 35 天的浓度,可能抑制 NO2 - 到否3 - 减少。相反,在 300 kg N/ha 处理中没有抑制硝化作用。累积 N2 300 kg N/ha 处理的壤土 O 通量最大,但在 1000 kg N/ha 处理下的沙壤土更大。结果还表明,土壤性质的差异,特别是碳的有效性,对于调节 N 转化和 N2 Ø 生产。总的来说,这些结果证明了在高 N 输入速率下提出的硝化抑制机制,由高 NH 驱动3 /NH4 和/或 NH 水平升高4 碳酸氢钠3 尿素水解。
更新日期:2019-11-14
中文翻译:
尿氮施用量对草地土壤氮素转化的影响
尿液是温带放牧草原的关键氮 (N) 输入,可驱动大量一氧化二氮 (N