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Restricted nitrous oxide emissions by ammonia oxidizers in two agricultural soils following excessive urea fertilization

机译:尿素过量施肥限制了两种农业土壤中氨氧化剂的一氧化二氮排放

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Purpose Nitrogen (N) fertilizer placement in bands is a widely accepted agricultural practice to increase N use efficiency. An excessive ammonium concentration in a fertilizer band can increase osmotic stress on ammonia oxidizers and potentially affect nitrification and resultant nitrous oxide (N2O) emissions, which is of great significance for soil function and climate change. The objectivity of this study was to identify the effects of excessive ammonium concentration on N2O emissions and ammonia oxidizers in two agricultural soils. Materials and methods In this study, we established a 56-day soil microcosm receiving a series of high concentrations of urea at 600, 900, and 1200 mg N kg(-1) (termed as N600, N900, and N1200, respectively), which simulated high ammonium levels in the center or proximity of a fertilizer band in two types of agricultural soils (fluvo-aquic soil and anthrosol). The mineral N concentrations, net nitrification rate, and N2O emissions were measured during the incubation. In addition, the abundances of bacterial and archaeal amoA were determined by using real-time quantitative PCR. Results and discussion Urea fertilization simultaneously increased the net nitrification rate and N2O emission at the early stage of incubation in both soils, suggesting N2O production was mainly from ammonia oxidation. Ammonia oxidizing bacteria (AOB) but not archaea (AOA) abundance was stimulated following urea fertilization and was positively correlated with N2O emission, indicating the dominant role of AOB in ammonia oxidation and N2O production in fertilized soils. The cumulative N2O emission was significantly higher in N1200 and N900 than N600 in both soils, but no further increase was observed in N1200 in the anthrosol. This implies restricted N2O production of ammonia oxidizers at excessive ammonium concentrations in the anthrosol. In the two soils treated with no N addition, the abundances of AOA amoA increased along the incubation time. Conclusions The present study collectively suggested that excessive urea-N addition was more effective in inhibiting N2O emission in the anthrosol than in the fluvo-aquci soil. AOB rather than AOA dominated the soil nitrification and N2O emissions under high N addition in both soils. The band fertilization regime may reduce the loss of N fertilizer from nitrification without necessarily increasing N2O emissions.
机译:目的在条带中放置氮肥是提高N利用率的一种广泛接受的农业实践。化肥带中铵盐浓度过高会增加氨气氧化剂的渗透压力,并可能影响硝化作用和产生的一氧化二氮(N2O)排放,这对于土壤功能和气候变化具有重要意义。这项研究的目的是确定铵盐浓度过高对两种农业土壤中N2O排放和氨氧化剂的影响。材料和方法在这项研究中,我们建立了一个为期56天的土壤缩影,在600、900和1200 mg N kg(-1)下分别接受一系列高浓度的尿素(分别称为N600,N900和N1200),该模型模拟了两种类型的农业土壤(潮土和人为土壤)中肥料带中心或附近的高铵含量。在培养过程中测量了矿物质氮的浓度,净硝化率和N2O排放。另外,通过使用实时定量PCR确定细菌和古细菌amoA的丰度。结果与讨论两种土壤在孵化初期,尿素施肥会同时增加净硝化速率和N2O排放,这表明N2O的产生主要来自氨氧化。尿素施肥后,氨氧化细菌(AOB)的丰度得到提高,但古细菌(AOA)却未得到刺激,并且与N2O排放呈正相关,表明AOB在施肥土壤中氨氧化和N2O产生中起主要作用。在两种土壤中,N1200和N900的累积N2O排放均显着高于N600,但在人为土壤中,N1200中未观察到进一步的增加。这意味着在人烟溶胶中铵盐浓度过高时,氨氧化剂的N2O产量会受到限制。在没有添加氮的两种土壤中,AOA amoA的丰度随着孵育时间的增加而增加。结论本研究共同表明,过量添加尿素-N比在潮水土壤中更能有效地抑制人为土壤中N2O的排放。在两种土壤中高氮添加下,AOB而非AOA主导了土壤硝化和N2O排放。波段施肥制度可以减少硝化过程中氮肥的损失,而不必增加N2O的排放。

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