Composition of soil recalcitrant C regulates nitrification rates in acidic soils

硝化作用 土壤水分 异养 环境化学 环境科学 温带气候 化学 土壤科学 植物 氮气 生物 细菌 遗传学 有机化学
作者
Yi Zhang,Siyi Liu,Yi Cheng,Zucong Cai,Christoph Müller,Jinbo Zhang
出处
期刊:Geoderma [Elsevier BV]
卷期号:337: 965-972 被引量:32
标识
DOI:10.1016/j.geoderma.2018.11.014
摘要

In acidic soils heterotrophic nitrification is considered to be an important NO3− production process. Previous studies have demonstrated that the content of soil C and soil C:N ratio was positively correlated with heterotrophic nitrification. However, relatively high heterotrophic nitrification rates also observed in cultivated black soils, with relatively low soil organic C content and soil C:N ratio compared to forest soils. To obtain a mechanistic understanding of heterotrophic nitrification the simultaneously occurring gross N transformations were quantified in five cultivated soils (SC) and six forest soils (SF) in subtropical region, ten cultivated soils (TC) and seven forest soils (TF) in temperate region subsequently analysed with respect to the soil physicochemical properties (pH, C:N ratio, SOC, TN), the chemical compositions of soil organic C (recalcitrant and labile organic C) and microbial communities (abundance of fungi, bacteria, amoA gene of AOB and AOA). The results showed that a significantly higher heterotrophic nitrification rate was observed in TC (0.52 mg N kg−1 d−1) compared to the other soils. The total content of soil C and soil C:N ratio could not explain the occurrence of heterotrophic nitrification but recalcitrant C fractions of carbonyl C and aromatic C, and the ratio of recalcitrant C to labile C (R:L ratio) was significantly positively correlated with heterotrophic nitrification rates (P < 0.01). This was further confirmed by structural equation modeling (SEM) that the R:L ratio was the most important indicator, suggesting that chemical composition of SOC is likely to be key to explain and predict heterotrophic nitrification rates across a large range of soils including soils high in black carbon such as chernozems, old grassland soils and/or anthropogenic soils such as anthrosols (Terra preta). In addition, heterotrophic nitrification rates were significantly positively correlated with fungal gene copy numbers (P < 0.05), providing a strong indication that fungi might be the predominant organisms carrying out heterotrophic nitrification.
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