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Biochar and organic fertilizer changed the ammonia-oxidizing bacteria and archaea community structure of saline-alkali soil in the North China Plain

机译:生物炭和有机肥改变了华北平原盐碱土的氨氧化细菌和古细菌群落结构

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Purpose The application of a large amount of inorganic nitrogen (N) fertilizer resulted in an increasing N loss. It is an effective practice that biochar and organic fertilizer replace part of inorganic nitrogen fertilizer. Thus, it is necessary to identify and compare the effects of biochar and organic fertilizer on ammonia-oxidizing bacteria (AOB) and ammonia-oxidizing archaea (AOA) community structure in saline-alkali soil.Materials and methods Three treatments in triplicate were included in the field experiment: (1) CK (no biochar and organic fertilizer), (2) biochar at 10.0 t ha(-1) year(-1) (C), and (3) organic fertilizer at 7.5 t ha(-1) year(-1) (M). The community structures and diversities of AOB and AOA were investigated by Illumina sequencing analysis of gene encoding ammonia monooxygenase subunit A (amoA) and followed by principal component analysis, least discriminant analysis effect size, and redundancy analysis.Results and discussion Biochar and organic fertilizers did not change the diversity of AOA and reduced the relative abundance of Candidatus-Nitrosoarchaeum in maize season, while only biochar increased the relative abundance of Candidatus-Nitrosotenuis in wheat season. The diversity of AOB was significantly reduced in the M treatment, but was not changed in the C treatment in wheat season. Moreover, the relative abundances of Nitrosomonas (CK, 15.1%; C, 6.8%; M, 3.4%) were decreased in the maize season, and the relative abundances of Nitrosovibrio (CK, 9.8%; C, 16.8%; M, 14.5%) were increased in the wheat season in the C and M treatments, which probably related to the changes in soil pH, soil NH4+-N content, and soil salt content (SSC). The lower soil pH, higher NO3--N content, and SSC resulted in Nitrosospira (maize season: CK, 42.2%; C, 40.7%; M, 62.0%; wheat season: CK, 46.6%; C, 50.7%; M, 65.4%) becoming the dominant genus in the M treatment.Conclusions Our results indicated that AOB was more susceptible than AOA to biochar and organic fertilizer. Organic fertilizer has significant effects on the diversities and community structure of AOB than biochar associated with the changing in soil pH, salinity, and mineral N.
机译:目的大量施用无机氮(N)肥料会导致氮损失增加。生物炭和有机肥料代替无机氮肥是一种有效的做法。因此,有必要鉴定和比较生物炭和有机肥对盐碱土壤中氨氧化细菌(AOB)和氨氧化古细菌(AOA)群落结构的影响。材料和方法一式三份包括三种处理方法田间试验:(1)CK(无生物炭和有机肥料),(2)10.0 t ha(-1)年(-1)(C)的生物炭,(3)7.5 t ha(-1)的有机肥料)年(-1)(M)。通过Illumina对氨单加氧酶亚基A(amoA)编码基因的测序分析,对AOB和AOA的群落结构和多样性进行了研究,然后进行了主成分分析,最小判别分析效果大小和冗余分析。结果和讨论玉米季节没有改变AOA的多样性,降低了念珠菌-Nitrosotenae的相对丰度,而只有生物炭增加了小麦季节念珠菌-Nitrosotenuis的相对丰度。在M处理中,AOB的多样性显着降低,但在小麦季节中,在C处理中,AOB的多样性没有改变。此外,玉米季节亚硝化单胞菌的相对丰度(CK,15.1%; C,6.8%; M,3.4%)降低,而亚硝基梭菌的相对丰度(CK,9.8%; C,16.8%; M,14.5)。 C和M处理使小麦季节的碳含量增加(%),这可能与土壤pH,土壤NH4 + -N含量和土壤盐分(SSC)的变化有关。较低的土壤pH值,较高的NO3--N含量和SSC导致硝化螺菌(玉米季节:CK,42.2%; C,40.7%; M,62.0%;小麦季节:CK,46.6%; C,50.7%; M (65.4%)成为M处理的主要菌种。结论我们的结果表明,AOB比AOA对生物炭和有机肥更敏感。与土壤pH,盐分和矿质氮变化相关的生物炭相比,有机肥对AOB的多样性和群落结构具有重要影响。

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