三峡库区消落区水体-沉积物重金属迁移转化特征

Movement and Transformation of Heavy Metals in Water-Sediment in Water-Level-Fluctuating Zone of Three Gorges Reservoir Area

结合三峡水库反季节调度模式,对消落区沉积物中Cu、Pb、Cd、Cr这4种重金属的存在形态及迁移转化特征进行研究.结果表明,不同重金属在消落区沉积物中形态分布各异,Cu主要以有机物及硫化物结合态和残渣态形式存在,Pb主要以碳酸盐结合态、Fe-Mn氧化物结合态及残渣态存在,Cd主要以碳酸盐结合态、Fe-Mn氧化物结合态存在,Cr主要以残渣态存在.伴随着消落过程的进行,汛期出露沉积物的有机质及AVS含量下降、ORP升高、pH值降低,沉积物中可提取态重金属的相对含量显著下降,重金属具有向水体迁移趋势,Cu、Pb、Cd、Cr平均迁移率分别为30.50%、26.10%、33.50%和11.77%,4种重金属的迁移性大小依次为Cd>Cu>Pb>Cr.可提取态Cu、Pb、Cd、Cr对重金属迁移贡献率分别为77.15%、86.09%、94.86%和32.34%,可提取态是重金属发生迁移的主要部分.研究结果表明,消落区重金属迁移呈"缓释"特征,三峡水库的反季节调度模式有利于缓解消落区重金属迁移诱导的生态风险,库区水体重金属含量处于较低水平.

According to the off-season regulation model for Three Gorges Reservoir, the characteristic of movement and transformation of Cu, Pb, Cd and Cr in sediment of water-level-fluctuating zone of Three Gorge Reservoir Area was investigated. The results indicated that the chemical fraction composition characteristics of heavy metals are different. Cu mainly existed in organic/sulphidic fraction and residual fraction; Pb mainly existed in carbonates, Fe-Mn oxides and residual fraction; Cd mainly existed in carbonates and Fe-Mn oxides fraction; Cr mainly existed in residual fraction. In flood season, the exposure of sediment from river bottom to atmosphere caused the decrease of TOC, AVS and pH and increase of ORP, and lowered the amount of extractable heavy metals. Heavy metals have the tendency to release to water body. The migration rates of Cu, Pb, Cd and Cr were 30.50%, 26.10%, 33.50%, and 11.77% respectively, the migration ability of heavy metals followed： Cd 〉 Cu 〉 Pb 〉 Cr. The contributions of extractable fractions of Cu, Pb, Cd and Cr to the migrated heavy metals were 77.15% , 86.09%, 94.86%, and 32.34% respectively, extractable fraction was the mainly part of the migrated heavy metals. The off-season regulation model for Three Gorges Reservoir lowered the ecological harm of heavy metals, the concentrations of Cu, Pb, Cr, Cd in the study areas were low.