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AMarkov-basedmodel for predicting the development trend of soil microbial communities in saline-alkali land in Wudi County

机译:Amarkov-基于Wudi县盐碱土地土壤微生物群落的发展趋势

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In October 2015, different salinity soils were collected in the coastal area of Wudi, Shandong,China. The soil microbial community composition, soil catalase, urease activity, and soil physicochemicalproperties were studied. The results showed that Nitrospira was dominant in thebacterial community, and it was the most related to total potassium. Cladosporium and Fusariumaccounted for thedominant fungal community, andurease, totalnitrogen,andCladosporiumwerethemost relevant. At the same time, urease and Fusarium are the most relevant. The species compositionof bacterial and fungal communities in the top soil of each saline-alkali soil is the mostabundant, and the degree of homogeneity is high. The activities of catalase in soils with heavy,moderate, and light salinity were 3.52 to 4.56, 3.08 to 4.61, and 5.81 to 6.91mL•g-1, respectively.Catalase activity all of them are characterized by gradual increase with soil depth; soil total potassiumis directly related to catalase, pH, organic matter, total nitrogen, and total phosphorus areindirectly related to catalase by total potassium. The urease activities of the saline-alkalinity soilswere 0.04-0.52, 0.08-1.07, and 0.27-8.21 mg•g-1, respectively, and the urease activity graduallydecreased as the soil depth increased. Small trend; soil total nitrogen is directly related to urease,pH, organic matter and total potassium are indirectly related to urease through total nitrogen.TheCCAranking showedthat totalphosphorushadthegreatest impactonbacterial communities,while urease had the greatest impact on the fungal community.
机译:2015年10月,在山东武都沿海地区收集了不同的盐度土壤,中国。土壤微生物群落成分,土壤过敏酶,脲酶活性和土壤物理化学研究了性质。结果表明,Nitrospira在占主导地位细菌群落,与总钾最有关。囊孢子和镰刀菌占患有的真菌群落,andurease,rovernitrogen,andcladosporiumwere相关的主题。与此同时,脲酶和镰刀菌是最相关的。物种组成每种盐碱土壤顶部土壤中的细菌和真菌社区最多丰富,均匀程度高。沉重的土壤中的过氧化氢酶的活性,温和,轻盈盐度分别为3.52至4.56,3.08至4.61,分别为5.81至6.91ml,而G-1。过氧化氢酶活性所有它们的特征在于土壤深度逐渐增加;土壤总钾与过氧化度,pH,有机物,总氮和总磷直接相关与总钾的过氧化氢酶间接相关。盐水碱度土壤的脲酶活性分别为0.04-0.52,0.08-1.07和0.27-8.21mg,逐渐释放脲酶活性随着土壤深度增加而下降。小趋势;土壤总氮与脲酶直接相关,pH,有机物质和总钾间接相关,与通过总氮的释放物无关。Charanking展示血症磷属植物症间肺结气社区,尿素对真菌群落产生了最大的影响。

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