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沿河口开垦 100 年时间序列中滨岸和沟渠湿地中重金属的分馏、迁移和生态风险。

Fractionation, transfer, and ecological risks of heavy metals in riparian and ditch wetlands across a 100-year chronosequence of reclamation in an estuary of China.

机构信息

State Key Laboratory of Water Environment Stimulation, School of Environment, Beijing Normal University, Beijing 100875, PR China; School of Nature Conservation, Beijing Forestry University, Beijing 100083, PR China.

State Key Laboratory of Water Environment Stimulation, School of Environment, Beijing Normal University, Beijing 100875, PR China.

出版信息

Sci Total Environ. 2015 Jun 1;517:66-75. doi: 10.1016/j.scitotenv.2015.02.052. Epub 2015 Feb 24.

Abstract

The effect of reclamation on heavy metal concentrations and the ecological risks in ditch wetlands (DWs) and riparian wetlands (RWs) across a 100-year chronosequence in the Pearl River Estuary of China was investigated. Concentrations of 4 heavy metals (Cd, Cu, Pb, and Zn) in soil and plant samples, and sequential extracts of soil samples were determined, using inductively coupled plasma atomic absorption spectrometry. Results showed that heavy metal concentrations were higher in older DW soils than in the younger ones, and that the younger RW soils contained higher heavy metal concentrations compared to the older ones. Although the increasing tendency of heavy metal concentrations in soil was obvious after wetland reclamation, the metals Cu, Pb, and Zn exhibited low or no risks to the environment based on the risk assessment code (RAC). Cd, on the other hand, posed a medium or high risk. Cd, Pb, and Zn were mainly bound to Fe-Mn oxide, whereas most of Cu remained in the residual phase in both ditch and riparian wetland soils, and the residual proportions generally increased with depth. Bioconcentration and translocation factors for most of these four heavy metals significantly decreased in the DWs with older age (p<0.05), whereas they increased in the RWs with younger age (p<0.05). The DW soils contained higher concentrations of heavy metals in the organic fractions, whereas there were more carbonate and residual fractions in the RW soils. The non-bioavailable fractions of Cu and Zn, and the organic-bound Cd and Pb significantly inhibited plant growth.

摘要

本研究调查了中国珠江口百年演替序列中围垦对沟渠湿地(DWs)和滨岸湿地(RWs)中重金属浓度及生态风险的影响。采用电感耦合等离子体原子吸收光谱法(ICP-AAS)测定了土壤和植物样品中 4 种重金属(Cd、Cu、Pb 和 Zn)的浓度及土壤样品的顺序提取。结果表明,较老的 DW 土壤中重金属浓度高于较年轻的 DW 土壤,而较年轻的 RW 土壤中重金属浓度高于较老的 RW 土壤。尽管湿地围垦后土壤中重金属浓度呈明显上升趋势,但根据风险评估代码(RAC),Cu、Pb 和 Zn 对环境的风险较低或没有。Cd 则表现出中到高风险。Cd、Pb 和 Zn 主要与铁锰氧化物结合,而 Cu 则主要以残余相存在于沟渠和滨岸湿地土壤中,且残余相比例通常随深度增加而增加。对于大多数这四种重金属,DWs 中年龄较大的土壤中的生物浓缩和转运系数显著降低(p<0.05),而 RW 中年龄较小的土壤中的生物浓缩和转运系数显著增加(p<0.05)。DW 土壤中重金属在有机相中浓度较高,而 RW 土壤中则有更多的碳酸盐和残余相。Cu 和 Zn 的非生物可利用部分,以及有机结合态的 Cd 和 Pb 显著抑制了植物的生长。

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