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首页> 外文期刊>Plant and Soil >Soil nitrous oxide emissions from a typical semiarid temperate steppe in inner Mongolia: effects of mineral nitrogen fertilizer levels and forms
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Soil nitrous oxide emissions from a typical semiarid temperate steppe in inner Mongolia: effects of mineral nitrogen fertilizer levels and forms

机译:内蒙古典型半干旱温带草原土壤一氧化二氮排放量:矿物氮肥水平和形态的影响

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Nitrous oxide (N2O) emissions can be significantly affected by the amounts and forms of nitrogen (N) available in soils, but the effect is highly dependent on local climate and soil conditions in specific ecosystem. To improve our understanding of the response of N2O emissions to different N sources of fertilizer in a typical semiarid temperate steppe in Inner Mongolia, a 2-year field experiment was conducted to investigate the effects of high, medium and low N fertilizer levels (HN: 200 kg N ha(-1)y(-1), MN: 100 kg N ha(-1)y(-1), and LN: 50 kg N ha(-1)y(-1)) respectively and N fertilizer forms (CAN: calcium ammonium nitrate, AS: ammonium sulphate and NS: sodium nitrate) on N2O emissions using static closed chamber method. Our data showed that peak N2O fluxes induced by N treatments were concentrated in short periods (2 to 3 weeks) after fertilization in summer and in soil thawing periods in early spring; there were similarly low N2O fluxes from all treatments in the remaining seasons of the year. The three N levels increased annual N2O emissions significantly (P < 0.05) in the order of MN > HN > LN compared with the CK (control) treatment in year 1; in year 2, the elevation of annual N2O emissions was significant (P < 0.05) by HN and MN treatments but was insignificant by LN treatments (P > 0.05). The three N forms also had strong effects on N2O emissions. Significantly (P < 0.05) higher annual N2O emissions were observed in the soils of CAN and AS fertilizer treatments than in the soils of NS fertilizer treatments in both measured years, but the difference between CAN and AS was not significant (P > 0.05). Annual N2O emission factors (EF) ranged from 0.060 to 0.298% for different N fertilizer treatments in the two observed years, with an overall EF value of 0.125%. The EF values were by far less than the mean default EF proposed by the Intergovernmental Panel on Climate Change (IPCC).
机译:一氧化二氮(N2O)排放会受到土壤中可用氮(N)的数量和形式的显着影响,但其影响高度取决于特定生态系统中的当地气候和土壤条件。为了增进我们对内蒙古典型的半干旱温带草原中N2O排放对不同氮源肥料响应的理解,我们进行了为期2年的田间试验,研究了高,中和低氮肥水平(HN: 200 kg N ha(-1)y(-1),MN:100 kg N ha(-1)y(-1)和LN:50 kg N ha(-1)y(-1))和N使用静态密闭室法处理N2O排放中的肥料形态(CAN:硝酸铵钙,AS:硫酸铵和NS:硝酸钠)。我们的数据表明,在夏季施肥后的短时间内(2至3周),以及在早春的土壤解冻期,由N处理诱导的N2O通量峰值集中。在一年的其余季节中,所有处理产生的N2O通量同样较低。与第1年的CK(对照)处理相比,这3个N水平按MN> HN> LN的顺序显着增加了年度N2O排放(P <0.05)。在第2年,HN和MN处理的年N2O排放量升高显着(P <0.05),而LN处理的则无统计学意义(P> 0.05)。三种氮的形式也对一氧化二氮的排放产生强烈影响。在两个测量年中,CAN和AS肥料处理土壤的年N2O排放均显着高于NS肥料处理土壤,但CAN和AS之间的差异并不显着(P> 0.05)。在观察的两年中,不同氮肥处理的年N2O排放因子(EF)为0.060至0.298%,总EF值为0.125%。 EF值远远小于政府间气候变化专门委员会(IPCC)提出的平均默认EF。

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