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Development and application of a method for determination of net nitrification rates

机译:净硝化率测定方法的开发与应用

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A laboratory method was developed that allows determination of in situ net nitrification with high sensitivity and at high temporal resolution. Nitrate in soils is quantitatively converted into nitrous oxide under strictly anaerobic conditions in the presence of 10 kPa acetylene by the soil endogenous denitrifier population, with the N2O detected by a gas chromatograph equipped with a 63Ni electron capture detector. Thus, even low net nitrification rates, i.e. small net increases in soil nitrate concentrations can easily be detected. Comparison of results using this method with results obtained using the classical in situ incubation method (buried bag soil incubation) revealed excellent agreement. Application of the new method allowed both determination of the seasonal pattern of net nitrification as well as correlation analysis between in situ NO and N2O flux rates and in situ net nitrification rates of the forest soils studied. Regardless of the forest site studied (spruce, spruce limed, beech), and during each year of a 3 years period (1995–1997), net nitrification varied strongly with season and was least during winter and greatest during summer. The long-term annual, mean rate of net nitrification for the untreated spruce site, the limed spruce site and the beech site were 1.54 ± 0.27 mg N kg−1 sdw d−1, 1.92 ± 0.23 mg N kg−1 sdw d−1 and 1.31 ± 0.23 mg N kg−1 sdw d−1, respectively. In situ rates of nitrification and NO and N2O emission were strongly correlated for all sites suggesting that nitrification was the dominate source of NO as well as N2O.
机译:开发了一种实验室方法,该方法可以高灵敏度和高时间分辨率确定原位净硝化。在土壤内源性反硝化作用下,在严格的厌氧条件下,在存在10 kPa乙炔的条件下,土壤中的硝酸盐被定量转化为一氧化二氮,其中N2O由装有63Ni电子的气相色谱仪检测捕获检测器。因此,即使很低的净硝化率,即土壤硝酸盐浓度的净增加很小,也可以容易地检测到。使用这种方法的结果与使用经典原位孵育方法(埋袋式土壤孵育)获得的结果进行比较,显示出极好的一致性。新方法的应用既可以确定净硝化的季节模式,也可以分析森林土壤的原位NO和N2 通量率与原位净硝化率之间的相关性。不论所研究的森林地点(云杉,云杉,石灰,山毛榉)如何,并且在3年期间的每一年(1995-1997年)中,净硝化作用均随季节变化很大,并且在冬季最小,在夏季最大。未经处理的云杉部位,石灰云杉部位和山毛榉部位的长期年平均净硝化速率为1.54±0.27 mg N kg−1 sdw d-1 ,1.92±0.23 mg N kg-1 sdw d-1 和1.31±0.23 mg N kg-1 sdw d-1 。原位硝化速率与所有站点的NO和N2 O排放密切相关,这表明硝化作用是NO和N2 O的主要来源。

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