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

机译:基于AMarkov模型的无di县盐碱地土壤微生物群落发展趋势预测

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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,在中国山东省无Shandong市沿海地区收集了不同的盐分土壤。研究了土壤微生物群落组成,土壤过氧化氢酶,脲酶活性和土壤理化性质。结果表明,硝化螺菌在 r n细菌群落中占主导地位,并且与总钾含量最相关。枝孢属和镰刀菌占主要的真菌群落,而脲酶,总氮和枝孢属最相关。同时,脲酶和镰刀菌最相关。每种盐碱土壤表层土壤中细菌和真菌群落的种类组成 r n最丰富,同质化程度较高。重度,中度和轻度盐分土壤中的过氧化氢酶活性分别为3.52至4.56、3.08至4.61和5.81至6.91mL•g-1。 r n过氧化氢酶的所有活性均具有逐渐变化的特征。随着土壤深度增加;土壤总钾与过氧化氢酶,pH,有机质,总氮和总磷直接相关,总钾与过氧化氢酶不直接相关。盐碱土壤的脲酶活性分别为0.04-0.52、0.08-1.07和0.27-8.21 mg•g-1,并且随着土壤深度的增加,脲酶活性逐渐降低。小趋势;土壤总氮与尿素酶直接相关, r npH,有机质和总钾与尿素酶通过总氮间接相关。 r nCCA排名显示,总磷对细菌群落的影响最大,而脲酶对真菌群落的影响最大。 。

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