The formation of the trace gases NO and N2O in soils by the coupled processes of nitrification and denitrification: results of kinetic 15N tracer investigations

R Russow, I Sich, H.-U Neue
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引用次数: 76

Abstract

Biogenic production in soils, especially when fertilized with high levels of nitrogen, is one of the main sources of nitrous oxide (N2O) and may be a significant source of nitric oxide (NO). NO and N2O are formed by the microbial processes of nitrification and denitrification but in soils these processes are not fully understood in detail. The kinetic 15N isotope method, is very useful for investigating the mechanism of such complex N transformation processes in soils. We used this method with 15NH4+, 15NO2, and 15NO3 as tracers to study the processes of NO and N2O formation in black earth soil (Haplic Phaeozem). The experiments were conducted using a special analytical set-up in which the incubation vessels were directly connected to a gas chromatograph quadrupole mass spectrometer system. This system allows simultaneous determination of the concentration of N2O, NO and N2 along with their 15N abundance in the gas phase. The results of these investigations are discussed and combined in a diagram, termed the model of coupled nitrification and denitrification, illustrating the formation of NO and N2O. Nitrification and denitrification proceed under both water-unsaturated (nearly aerobic) and water-saturated (nearly anaerobic) conditions. The two processes are linked by a “common” nitrate pool. In contrast the nitrite, an important intermediate of the two processes, evidently exists within two separate pools. NO is mainly produced by nitrification as a by-product of the oxidation of ammonium to nitrite or directly by nitrite decomposition. If NH4+ contents are high under aerobic conditions NO emission can markedly exceed that of N2O. Nitrous oxide is mainly formed by denitrification of nitrate. Therefore increasing water saturation promotes N2O emission. NO could not be confirmed as a free precursor of N2O formation via denitrification.

硝化和反硝化耦合过程中土壤中微量气体NO和N2O的形成:动力学15N示踪研究结果
土壤中的生物源性生产,特别是在高水平氮施肥时,是一氧化二氮(N2O)的主要来源之一,可能是一氧化二氮(NO)的重要来源。NO和N2O是由微生物的硝化和反硝化过程形成的,但在土壤中这些过程的细节尚未完全了解。动力学15N同位素方法对于研究土壤中这种复杂的N转化过程的机理是非常有用的。采用该方法,以15NH4+、15NO2−和15NO3−为示踪剂,研究了黑土(Haplic Phaeozem)中NO和N2O的形成过程。实验使用一种特殊的分析装置进行,其中孵育容器直接连接到气相色谱仪四极杆质谱仪系统。该系统可以同时测定N2O、NO和N2的浓度及其在气相中的15N丰度。这些研究的结果被讨论并结合在一个图表中,称为耦合硝化和反硝化模型,说明了NO和N2O的形成。硝化和反硝化在水不饱和(近好氧)和水饱和(近厌氧)条件下进行。这两个过程由一个“共同的”硝酸盐库连接起来。相反,这两个过程的重要中间体亚硝酸盐显然存在于两个不同的池中。NO主要由硝化作用产生,作为氨氧化生成亚硝酸盐的副产物或直接由亚硝酸盐分解产生。在好氧条件下,当NH4+含量较高时,NO的排放量会明显超过N2O。氧化亚氮主要由硝酸盐的反硝化作用形成。因此,水饱和度的增加促进了N2O的排放。不能证实NO是通过反硝化作用形成N2O的自由前体。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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