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镉污染稻田耕层与犁底层土壤镉形态分布对土壤性质及土壤微生物的响应

Cadmium Speciation Distribution Responses to Soil Properties and Soil Microbes of Plow Layer and Plow Pan Soils in Cadmium-Contaminated Paddy Fields.

作者信息

Hao Xiaodong, Bai Lianyang, Liu Xueduan, Zhu Ping, Liu Hongwei, Xiao Yunhua, Geng Jibiao, Liu Qianjin, Huang Lihua, Jiang Huidan

机构信息

Shandong Provincial Key Laboratory of Water and Soil Conservation and Environmental Protection, College of Resources and Environment, Linyi University, Linyi, China.

Biotechnology Research Institute, Hunan Academy of Agricultural Sciences, Changsha, China.

出版信息

Front Microbiol. 2021 Dec 3;12:774301. doi: 10.3389/fmicb.2021.774301. eCollection 2021.

Abstract

Cadmium (Cd) speciation ratio in arable land determines the Cd exposure risk and Cd uptake in crops. However, the driving mechanisms of Cd speciation change on the vertical scale of paddy fields remain poorly understood. In this study, the effects of plow layer and plow pan on Cd speciation distribution were investigated in a long-term Cd-contaminated rice ecosystem. The Cd accumulative effect within rice grain was enhanced with high levels of activated Cd speciation ratios in soils. Activated Cd speciation ratios were higher in plow layer soils, while stabilized Cd speciation ratios were elevated in plow pan soils. Soil physicochemical properties and soil microbes synergistically affected the Cd speciation changes in different ways between the two soil layers. Soil pH and organic elements in plow layer environment directly hindered the transformation of stabilized Cd speciation, while in plow pan environment, soil pH and organic elements indirectly decreased activated Cd speciation ratios and resulted in the accumulation of stabilized Cd speciation regulating the predominant bacterial taxa. This study will improve our understanding of how soil environments regulate Cd speciation distributions in rice ecosystems and help to seek effective remediation methods of Cd-contaminated paddy fields to reduce the Cd accumulation in rice.

摘要

耕地中镉(Cd)的形态比例决定了作物的镉暴露风险和镉吸收量。然而,稻田垂直尺度上镉形态变化的驱动机制仍不清楚。本研究在长期受镉污染的水稻生态系统中,研究了犁底层和犁底层对镉形态分布的影响。土壤中高含量的活性镉形态比例会增强水稻籽粒中的镉积累效应。犁底层土壤中活性镉形态比例较高,而犁底层土壤中稳定镉形态比例升高。土壤理化性质和土壤微生物以不同方式协同影响两层土壤中镉形态的变化。犁底层环境中的土壤pH值和有机元素直接阻碍了稳定镉形态的转化,而在犁底层环境中,土壤pH值和有机元素间接降低了活性镉形态比例,导致稳定镉形态的积累,从而调节主要细菌类群。本研究将增进我们对土壤环境如何调节水稻生态系统中镉形态分布的理解,并有助于寻求镉污染稻田的有效修复方法,以减少水稻中的镉积累。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/7718/8679784/564ce0236dfd/fmicb-12-774301-g001.jpg

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