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首页> 外文期刊>Applied Ecology and Environmental Research >RESPONSE OF SOIL FUNGAL COMMUNITY STRUCTURE AND DIVERSITY TO SALINE WATER IRRIGATION IN ALLUVIAL GREY DESERT SOILS
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RESPONSE OF SOIL FUNGAL COMMUNITY STRUCTURE AND DIVERSITY TO SALINE WATER IRRIGATION IN ALLUVIAL GREY DESERT SOILS

机译:土壤真菌群落结构与盐水灌溉土壤真菌群落结构和多样性的反应

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Saline water irrigation can change the soil environment, thereby influencing soil microbial processes. In this study, a nine years saline water irrigation experiment had been conducted in Shihezi, Xinjiang Province, China, to investigate the composition and diversity of the soil fungal community. Our results showed that irrigation with either brackish or saline water significantly increased soil salinity and Available Phosphorus, but reduced soil pH, SOC, TN, and Available Kalium. Saline water irrigation significantly decreased operational taxonomic units (OTUs), ACE, Chao1, and Shannon indices but increased Simpson indices. The dominant fungal phyla were Ascomycota, Mortierellomycota, Basidiomycota, Glomeromycota, and Chytridiomycota. Irrigation with either brackish or saline water significantly reduced the abundance of Mortierellomycota but increased the abundance of Ascomycota and Basidiomycota. In addition, saline water irrigation significantly decreased the relative abundance of Glomeromycota compared with fresh water irrigation, but significantly increased the relative abundance of Chytridiomycota. Redundancy analysis (RDA) results showed that salinity (ECe) was the primary factors driving the changes in soil fungal community composition. LEfSe analysis demonstrated fungal potential biomarkers decreased by saline water irrigation. These results increase our understanding of soil ecological processes in soils that are increasingly salinized.
机译:盐水灌溉可以改变土壤环境,从而影响土壤微生物过程。在这项研究中,九年盐水灌溉实验已经在新疆,新疆省,探讨了土壤真菌群落的组成和多样性。我们的研究结果表明,咸水或盐水的灌溉显着增加了土壤盐度和可用磷,但减少了土壤pH,SOC,TN和可获得的千卡。盐水灌溉显着减少了运营分类单位(OTU),ACE,Chao1和Shannon指数,但辛普森索引增加。优势真菌phyla是ascomcota,mortierellomycota,碱霉菌,肾小球霉菌和chytridiomycota。灌溉或盐水的灌溉显着降低了大量的菌兵霉菌,但增加了ascomcota和盆西的丰富。此外,与淡水灌溉相比,盐水水灌溉显着降低了肾小球菌的相对丰富性,但显着增加了Chytridiomcota的相对丰度。冗余分析(RDA)结果表明,盐度(ECE)是推动土壤真菌群落组成的变化的主要因素。 lefse分析表明,盐水水灌溉的真菌潜在的生物标志物降低。这些结果提高了我们对越来越盐化的土壤中土壤生态过程的理解。

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