模拟淹水条件下三峡库区消落带土壤重金属形态变化
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国家水体污染控制与治理科技重大专项(2009ZX07104-003)

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    摘要:

    采集三峡库区小江流域消落带土样,通过室内模拟试验和化学分析,考察土壤理化性质和消落带土壤淹水前后重金属(Fe、Mn、Cu、Zn)形态变化。结果表明:淹水导致Fe2+、Mn2+、有效铜等重金属含量增加,平均含量分别从58.88、35.26、0.96 mg/kg增加到1 383.8、782.7、1.73 mg/kg;淹水15 d后,部分样品有效锌含量增加10.15%~12.18%,部分样品有效锌含量减少3.69%~7.12%;淹水30 d后,有效锌的含量增加10.9%~46.6%。土壤基本理化性质对土壤重金属含量也有影响。

    Abstract:

    Soil samples on Xiaojiang watershed water-level fluctuation zone in the Three Gorges Reservoir Area were collected for the study.By simulation incubation and chemical analysis,the basic physical-chemical properties of soils and the changing forms of heavy metals (Fe2+,Mn2+,available Cu and Zn) were examined in continuous anoxic conditions.The results showed that flooding increased the contents of the Fe2+,Mn2+,available Cu.The contents increased on average from 58.88,35.26,0.96 mg/kg to 1 383.8,782.7,1.73 mg/kg,respectively.After 15 days’ flooding,the contents of available Zn in both Gaoyang and Yanglu increased at the rates of 12.18% and 10.15%,but the other forms decreased at the rates of 7.12% and 3.69%.After 30 days’ flooding,the contents of available Zn increased with the increment rate ranging from 10.9% to 46.6%.The changing form of heavy metals were influenced by the basic physical and chemical properties of soils.

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郭沛,朱强,王素梅,胡红青,胡莲,万成炎,张志永.模拟淹水条件下三峡库区消落带土壤重金属形态变化[J].华中农业大学学报,2013,32(6):70-74

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  • 收稿日期:2012-11-15
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