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Community composition of ammonia-oxidizing bacteria and archaea in rice field soil as affected by nitrogen fertilization

机译:施氮对稻田土壤氨氧化细菌和古细菌群落组成的影响

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Little information is available on the ecology of ammonia-oxidizing bacteria (AOB) and archaea (AOA) in flooded rice soils. Consequently, a microcosm experiment was conducted to determine the effect of nitrogen fertilizer on the composition of AOB and AOA communities in rice soil by using molecular analyses of ammonia monooxygenase gene (amoA) fragments. Experimental treatments included three levels of N (urea) fertilizer, i.e. 50, 100 and 150mgNkg super(-) super(1) soil. Soil samples were operationally divided into four fractions: surface soil, bulk soil deep layer, rhizosphere and washed root material. NH sub(4) super(+)-N was the dominant form of N in soil porewater and increased with N fertilization. Cloning and sequencing of amoA gene fragments showed that the AOB community in the rice soil consisted of three major groups, i.e. Nitrosomonas communis cluster, Nitrosospira cluster 3a and cluster 3b. The sequences related to Nitrosomonas were predominant. There was a clear effect of N fertilizer and soil depth on AOB community composition based on terminal restriction fragment length polymorphism fingerprinting. Nitrosomonas appeared to be more abundant in the potentially oxic or micro-oxic fractions, including surface soil, rhizosphere and washed root material, than the deep layer of anoxic bulk soil. Furthermore, Nitrosomonas increased relatively in the partially oxic fractions and that of Nitrosospira decreased with the increasing application of N fertilizer. However, AOA community composition remained unchanged according to the denaturing gradient gel electrophoresis analyses.
机译:关于淹没的水稻土中氨氧化细菌(AOB)和古细菌(AOA)的生态学方面的信息很少。因此,通过使用氨单加氧酶基因(amoA)片段的分子分析,进行了微观实验,以确定氮肥对水稻土中AOB和AOA群落组成的影响。实验处理包括三种水平的N(尿素)肥料,即50、100和150mgNkg的super(-)super(1)土壤。将土壤样品在操作上分为四个部分:表层土壤,块状土壤深层,根际和洗过的根部材料。 NH sub(4)super(+)-N是土壤孔隙水中氮的主要形式,并随着施氮量的增加而增加。 amoA基因片段的克隆和测序表明,水稻土中的AOB群落由三个主要组组成,即亚硝化单胞菌簇,亚硝基螺菌簇3a和簇3b。与亚硝化单胞菌有关的序列占主导。基于末端限制性片段长度多态性指纹图谱,氮肥和土壤深度对AOB群落组成有明显影响。亚硝酸盐在潜在的含氧或微含氧成分中(包括表层土壤,根际和水洗的根部物质)似乎比缺氧的散装土壤深层更为丰富。此外,随着氮肥施用量的增加,亚硝化单胞菌在部分含氧部分中相对增加,而亚硝基螺菌的部分减少。然而,根据变性梯度凝胶电泳分析,AOA群落组成保持不变。

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