滇池典型湖区沉积物粒径与重金属分布特征

Sediment Particle Size and the Distribution of Heavy Metals in the Typical Districts of Dianchi Lake

  • 摘要: 对滇池3个代表性湖区(草海、湖心区、外海南部)表层(0~10cm)沉积物的粒径组成进行了分析,测试了不同粒径沉积物的主要理化性质和Cu、Cr、Ni、Zn、Pb、Fe、Mn、Cd等8种重金属的质量分数,并对滇池沉积物中重金属质量分数的粒径效应作了校正. 结果表明:滇池表层沉积物粒径主要分布在<250μm的范围内;粉砂(4~<63μm)所占比例最大,平均达到60%;黏土(<4μm)次之,平均占19%. 随着粒径的减小,大部分重金属质量分数在不同粒径的沉积物中呈增加趋势. 重金属在细粒径(<63μm) 沉积物中所占比例平均达79%,显著高于其他粒径(63~<125、125~<250μm). Cr、Cd、Cu、Pb、Zn和Ni具有相似的富集特性,其质量分数高值均出现在粒径为4~<63μm的沉积物中,该粒径沉积物中6种重金属的质量分数分别为土壤背景值的2.04、9.77、4.35、5.11、3.47和4.60倍;而w(Fe)和w(Mn)在各粒径沉积物中无明显差异. 黏土校正结果与不同粒径沉积物黏土校正的理论计算值相差不大. 黏土校正与参比元素校正都适合校正滇池不同粒径沉积物的重金属质量分数.

     

    Abstract: Composition of the surface sediments with particle sizes of 0-10cm were analyzed at three representative sites (Caohai, mid-lake, southern Waihai) from Dianchi Lake. Physiochemical properties and the concentrations of Cu, Cr, Ni, Zn, Pb, Fe, Mn and Cd in different particle-size fractions of the sediment were measured. The distributions in the surface sediment of different particle size were studied, as well as the normalization of metals concentrations was taken. The results showed that the surface sediments of the Dianchi Lake were dominated by the particles with sizes lower than 250μm. Silty (4-<63μm) made up of the biggest fraction among the four sizes with average of 60%. Besides, the clay (<4μm) was secondary, accounting for 19%. The overall most of heavy metal concentration increased with the particle size decreases. The average ratio of heavy metals in silts (<63μm) reached 79%, which was significantly higher than that in extremely fine sands (63-<125μm) and fine sands (125-<250μm). Cr, Cd, Cu, Pb, Zn and Ni have a peak concentration in the range of 4-<63μm with similar concentrations and enrichment properties. The six heavy metals concentrations mentioned above in <63μm fraction were 2.04,9.77,4.35,5.11,3.47and 4.60times of their local soil background values, respectively. Fe and Mn have no strong enrichment in these four particle sizes. No large difference was found between results calibrated by the clay concentration and calculated concentrations in initial sediments. Results of heavy metals in different size fractions were calibrated by the clay concentration in agreement with that of reference element calibration. In conclusion, both of these two methods were useful in calibration of heavy metals concentration in different size fractions of sediments from the Dianchi Lake.

     

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