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土壤硝化作用中亚硝酸盐积累的机制。

Mechanisms of nitrite accumulation occurring in soilnitrification.

作者信息

Shen Q R, Ran W, Cao Z H

机构信息

College of Natural Resources and Environmental Sciences, Nanjing Agricultural University, Nanjing 210095, China.

出版信息

Chemosphere. 2003 Feb;50(6):747-53. doi: 10.1016/s0045-6535(02)00215-1.

Abstract

Because low concentration of nitrite could be toxic to biological systems and high amounts of nitrite have been observed in a river of northern China since 1990, nitrite from agricultural soil sources should be investigated. In this paper, effects of levels of ammonium-N (NH4+-N), soil pH and nitrification inhibitors on NO2- accumulation, and duration of nitrite in soils were studied. Application of 11.2 mg of nitrapyrin kg(-1) soil or 11.2 mg of sodium azide kg(-1) soil dramatically suppressed nitrite occurrence. Within all incubation times and at all levels of ammonium-N input, we did not detect any measurable NO2-N accumulation in samples of Yellow-brown earth (pH 5.67), but observed huge accumulation in the 2 alkaline soils, Fluvo-aquic loam (pH 7.89) and Fluvo-aquic sand (pH 8.20). The concentrations of nitrite in both alkaline soils were related to ammonium-N levels. The effect of pH on nitrite accumulation was demonstrated by using slurries of Fluvo-aquic sand under continuous aeration and buffers of different pH. Data showed that nitrite concentration increased with the elevated pH, yet that ammonia oxidizers from the original soil (pH 8.2) could adapt to the new medium of low pH (pH 5.35). Dynamic changes of nitrite in soils amended with different rates of nitrite-N were also measured in 6 days. Thereby, we concluded that nitrite was unstable in acid soils, but durable in alkaline soils. The authors suggested that NO2- accumulation in field soils and its subsequent environmental impact should receive more attention.

摘要

由于低浓度亚硝酸盐可能对生物系统有毒,且自1990年以来在中国北方一条河流中观测到大量亚硝酸盐,因此应调查农业土壤来源的亚硝酸盐。本文研究了铵态氮(NH4+-N)水平、土壤pH值和硝化抑制剂对土壤中亚硝酸盐积累及亚硝酸盐持续时间的影响。施用11.2毫克/千克土壤的氯吡脲或11.2毫克/千克土壤的叠氮化钠可显著抑制亚硝酸盐的产生。在所有培养时间和所有铵态氮输入水平下,我们在黄棕壤(pH 5.67)样品中未检测到任何可测量的亚硝酸盐氮积累,但在两种碱性土壤,即潮土壤土(pH 7.89)和潮土砂土(pH 8.20)中观测到大量积累。两种碱性土壤中的亚硝酸盐浓度均与铵态氮水平有关。通过在连续曝气条件下使用潮土砂土泥浆和不同pH值的缓冲液,证明了pH值对亚硝酸盐积累的影响。数据表明,亚硝酸盐浓度随pH值升高而增加,然而来自原始土壤(pH 8.2)的氨氧化菌能够适应低pH值(pH 5.35)的新介质。还在6天内测定了用不同亚硝酸盐氮速率改良的土壤中亚硝酸盐的动态变化。由此,我们得出结论,亚硝酸盐在酸性土壤中不稳定,但在碱性土壤中持久存在。作者建议,田间土壤中亚硝酸盐的积累及其随后的环境影响应受到更多关注。

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