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The effect of C:N ratio on heterotrophic nitrification in acidic soils

机译:C:N比对酸性土壤异养硝化的影响

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Generally, a high carbon to nitrogen (C:N) ratio is considered an important factor inducing heterotrophic nitrification in acidic soils; however, few studies have investigated the regulation of C:N ratio on heterotrophic nitrification. In the present study, a C:N ratio gradient (C:N 23, C:N 19, C:N 15, C:N 10) was regulated in acidic forest soil (SF) and acidic agricultural soil (SC) under 24 h and 30 days incubation, and N-15-labeling techniques combined with acetylene inhibition were used to distinguish between heterotrophic and autotrophic nitrification. Gene copy abundance and soil fungi and bacteria composition were also determined under 30 days C:N ratio regulation. The results showed that N input in C-abundant soils (e.g. SF in this investigation) and C input in N-abundant soil (e.g. SC in this investigation), instead of high C:N ratios, may stimulate soil heterotrophic nitrification. The stimulatory effect of acetic acid on heterotrophic nitrification in SC rather than SF further confirmed our conclusion. Soil fungal populations were significantly and positively correlated with gross heterotrophic nitrification rates and the ratio of heterotrophic nitrification rate to total nitrification rate, in addition to the contribution of heterotrophic NO3- production to total NO3- production in both the N-15-NH4+ and N-15-Glycine treatments, indicating soil fungi could play the key role in driving heterotrophic nitrification. In addition, our results suggested that Mortierella and Trichodenna were the potential fungal species driving heterotrophic nitrification in acidic forest soils, while Exophiala and Acidomelania seemed to be the fungal species driving heterotrophic nitrification in acidic agricultural soils according to their high abundance in C-abundant treatments. Consequently, initial soil C and soil N status should be taken into account when predicting the responses of soil heterotrophic nitrification to C or N soil inputs.
机译:通常,高碳对氮气(C:N)的比例被认为是在酸性土壤中诱导异养硝化的重要因素;然而,很少有研究研究了C:N比对异养硝化的调节。在本研究中,在酸性森林土壤(SF)和24岁以下的酸性农业土壤(SC)中调节C:N比梯度(C:N 23,C:N 19,C:N 15,C:N 10) H和30天孵育,并使用与乙炔抑制结合的N-15标记技术区分异养和自养硝化。基因复制丰度和土壤真菌和细菌组合物也在30天C:N比调控下测定。结果表明,N在C型土壤中的N输入(例如,本研究中的SF)和N丰土中的C输入(例如,本研究中的SC.SC),而不是高C:N比例,可以刺激土壤异养硝化。乙酸对SC中异养硝化而不是SF的刺激作用进一步证实了我们的结论。除了在N-15-NH4 +和N中的N-15-NH4 +和N中的总NO 3-生产的贡献之外,土壤真菌群显着且杂养硝化率与总硝化率与总硝化率的比例呈正相关。 -15-甘氨酸治疗,表明土壤真菌可以发挥促进异养硝化的关键作用。此外,我们的结果表明,Mortierella和Trichodenna是潜在的真菌物种,潜在的抗酸性森林土壤中硝化硝化,而Exoshiala和酸甲醇似乎是根据其在C-Auvery治疗中的高丰度促进酸性农业土壤中异养硝化的真菌物种。因此,当预测土壤异养硝化氢对C或氮土壤投入的反应时,应考虑初始土壤C和土壤N状况。

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