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豫中南烟区不同质地土壤理化性质、酶活性及微生物群落分析

Effects of soil texture on physicochemical properties, enzyme activities and microbial communities of soils in central and south Henan tobacco-planting areas

  • 摘要: 为明确土壤质地因素对土壤主要理化性质、酶活性和微生物群落的影响,采集并分析了豫中南烟区襄县、郏县和泌阳等三地的土壤样品。结果表明:① 三县烟区土壤质地以黏壤土为主,黏土与壤土所占比例较低。壤土的田间持水量高于黏土,而黏土的次表层硬度高于壤土和黏壤土。② 黏土的pH、有机质和速效钾含量较高,壤土的速效磷含量较高,而黏壤土的氯含量较高。③ 壤土磷酸酶活性高于黏土,而蔗糖酶和过氧化氢酶活性低于黏壤土和黏土,黏土脲酶活性高于壤土和黏壤土;黏土细菌数量和丰度指数高于壤土,黏壤土的细菌多样性指数高于壤土。④ 壤土、黏壤土和黏土在门水平的细菌群落组成相同,但相对丰度上有一定差异,壤土和黏土均以酸杆菌门相对丰度最高,而黏壤土的变形菌门所占比例最高;3种质地的真菌群落组成及相对丰度差异不明显。

     

    Abstract: To investigate the effects of soil texture on the physicochemical properties, enzyme activities and microbial communities of soil, soil samples collected from central and south Henan tobacco-planting areas, i.e. Xiangxian, Jiaxian and Biyang, were analyzed. The results showed that:1) Main soil texture in the three counties was clay loam soil, and the proportions of clay soil and loam soil were small. The field capacity of loam soil was higher than that of clay soil, however the subsurface hardness of clay soil was higher than that of loam soil and clay loam soil. 2) pH values and contents of organic matter and available K were higher in clay soil, while available P contents in loam soil and chlorine contents in clay loam soil were higher. 3) The phosphatase activity of loam soil was higher than that of clay soil, however its invertase and catalase activities were lower than those of clay loam soil and clay soil; among the three kinds of soils, the urease activity of clay soil was higher; while the quantity and abundance index of bacteria in clay soil and the diversity index of bacteria in clay loam soil was higher than those in loam soil. 4) The bacterial community compositions in loam, clay loam and clay soils were similar on phylum level, but there was some difference in relative abundance. The relative abundances of Acidobacteria were the highest both in loam soil and clay soil, and the proportion of Proteobacteria were the highest in clay loam soil. The fungal community compositions and relative abundances were not significantly different among the three kinds of soils.

     

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