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Effect of long-term fertilization strategies on bacterial community composition in a 35-year field experiment of Chinese Mollisols

机译:长期施肥策略对中国软体动物35年田间试验的影响

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摘要

Bacteria play vital roles in soil biological fertility; however, it remains poorly understood about their response to long-term fertilization in Chinese Mollisols, especially when organic manure is substituted for inorganic nitrogen (N) fertilizer. To broaden our knowledge, high-throughput pyrosequencing and quantitative PCR were used to explore the impacts of inorganic fertilizer and manure on bacterial community composition in a 35-year field experiment of Chinese Mollisols. Soils were collected from four treatments: no fertilizer (CK), inorganic phosphorus (P) and potassium (K) fertilizer (PK), inorganic P, K, and N fertilizer (NPK), and inorganic P and K fertilizer plus manure (MPK). All fertilization differently changed soil properties. Compared with CK, the PK and NPK treatments acidified soil by significantly decreasing soil pH from 6.48 to 5.53 and 6.16, respectively, while MPK application showed no significant differences of soil pH, indicating alleviation of soil acidification. Moreover, all fertilization significantly increased soil organic matter (OM) and soybean yields, with the highest observed under MPK regime. In addition, the community composition at each taxonomic level varied considerably among the fertilization strategies. Bacterial taxa, associated with plant growth promotion, OM accumulation, disease suppression, and increased soil enzyme activity, were overrepresented in the MPK regime, while they were present at low abundant levels under NPK treatment, i.e. phyla Proteobacteria and Bacteroidetes, class Alphaproteobacteria, and genera Variovorax, Chthoniobacter, Massilia, Lysobacter, Catelliglobosispora and Steroidobacter. The application of MPK shifted soil bacterial community composition towards a better status, and such shifts were primarily derived from changes in soil pH and OM.
机译:细菌在土壤生物肥力中起着至关重要的作用。但是,关于它们对中国软体动物长期施肥的反应仍知之甚少,特别是当有机肥料代替无机氮肥时。为了拓宽我们的知识,在为期35年的中国Mollisols田间试验中,使用高通量焦磷酸测序和定量PCR来探讨无机肥料和肥料对细菌群落组成的影响。从以下四种处理中收集土壤:无肥料(CK),无机磷(P)和钾(K)肥料(PK),无机P,K和N肥料(NPK),无机P和K肥料加肥料(MPK) )。所有的施肥都会改变土壤的性质。与CK相比,PK和NPK处理使土壤pH值分别从6.48显着降低至5.53和6.16,从而酸化了土壤,而MPK的施用没有显示土壤pH的显着差异,表明减轻了土壤酸化。此外,所有施肥均显着提高了土壤有机质(OM)和大豆单产,在MPK制度下观察到最高。此外,每个分类学级别的群落组成在施肥策略之间也有很大差异。在MPK方案中,与植物生长促进,OM积累,病害抑制和土壤酶活性增加相关的细菌类群被过度代表,而在NPK处理下它们却以较低的丰富水平存在,即门菌属和拟杆菌属,丙型杆菌属和Variovorax,Chononiobacter,Massilia,Lysobacter,Catheloblobosispora和Steroidobacter属。 MPK的应用使土壤细菌群落组成向更好的状态转变,这种转变主要源自土壤pH和OM的变化。

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