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首页> 外文期刊>Journal of environmental sciences >Copper pollution decreases the resistance of soil microbial community to subsequent dry-rewetting disturbance
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Copper pollution decreases the resistance of soil microbial community to subsequent dry-rewetting disturbance

机译:铜污染降低了土壤微生物群落对随后的干湿重扰的抵抗力

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Dry-rewetting (DW) disturbance frequently occurs in soils due to rainfall and irrigation, and the frequency of DW cycles might exert significant influences on soil microbial communities and their mediated functions. However, how microorganisms respond to DW alternations in soils with a history of heavy metal pollution remains largely unknown. Here, soil laboratory microcosms were constructed to explore the impacts of ten DW cycles on the soil microbial communities in two contrasting soils (fluvo-aquic soil and red soil) under three copper concentrations (zero, medium and high). Results showed that the fluctuations of substrate induced respiration (SIR) decreased with repeated cycles of DW alternation. Furthermore, the resistance values of substrate induced respiration (RS-SIR) were highest in non-copper-stressed (zero) soils. Structural equation model (SEM) analysis ascertained that the shifts of bacterial communities determined the changes of RS-SIR in both soils. The rate of bacterial community variance was significantly lower in noncopper- stressed soil compared to the other two copper-stressed (medium and high) soils, which might lead to the higher RS-SIR in the fluvo-aquic soil. As for the red soil, the substantial increase of the dominant group WPS-2 after DW disturbance might result in the low RS-SIR in the high copper-stressed soil. Moreover, in both soils, the bacterial diversity was highest in non-copper-stressed soils. Our results revealed that initial copper stress could decrease the resistance of soil microbial community structure and function to subsequent DW disturbance. (C) 2015 The Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences. Published by Elsevier B.V.
机译:由于降雨和灌溉,土壤中的干重湿润(DW)干扰频繁发生,DW循环的频率可能会对土壤微生物群落及其介导的功能产生重大影响。然而,在重金属污染史上,微生物如何响应土壤中DW的变化仍然未知。在这里,构建了土壤实验室微观世界,以探索三个铜浓度(零,中和高)下两个对比土壤(潮土和红壤)中十个DW循环对土壤微生物群落的影响。结果表明,随着DW交替循环的进行,底物诱导的呼吸(SIR)的波动减小。此外,在非铜胁迫(零)土壤中,基质诱导呼吸(RS-SIR)的阻力值最高。结构方程模型(SEM)分析确定,细菌群落的变化决定了两种土壤中RS-SIR的变化。与其他两种铜胁迫(中等和高)土壤相比,非铜胁迫土壤的细菌群落变异率要低得多,这可能导致潮潮土壤中的RS-SIR较高。至于红壤,DW干扰后显着增加的WPS-2优势族可能导致高铜胁迫土壤中的低RS-SIR。此外,在两种土壤中,非铜胁迫土壤的细菌多样性最高。我们的研究结果表明,初始铜胁迫可以降低土壤微生物群落结构和对随后的DW干扰的抵抗力。 (C)2015年中国科学院生态环境研究中心。由Elsevier B.V.发布

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