机构地区:[1]State Key Laboratory of Urban and Regional Ecology, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences [2]Faculty of Veterinary and Agricultural Sciences, The University of Melbourne [3]National Soil Fertility and Fertilizer Effects Long-term Monitoring Network, Institute of Agricultural Resources and Regional Planning,Chinese Academy of Agricultural Sciences
出 处:《Journal of Environmental Sciences》2016年第1期155-164,共10页环境科学学报(英文版)
基 金:financially supported by the National Science Foundation of China (Nos. 51221892 and 41025004);the Strategic Priority Research Program of the Chinese Academy of Sciences (No. XDB15020200)
摘 要: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.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.
关 键 词:Copper stress Dry–rewetting disturbance Bacterial community Substrate induced respiration Resistance
分 类 号:X53[环境科学与工程—环境工程] X172
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