摘要
通过对太湖沉积物微量元素的测定,分析了沉积物的元素含量特征及变化趋势,指出了重金属元素的分布特点。沉积物和岩石微量元素的上地壳标准化值显示,它们的曲线存在明显的区别,反映了物质在风化和沉积过程中不同的性质差异。重金属在太湖北部地区较高,在南部地区较低,特别是As、Hg、Cu、Zn、Ni。对照背景值,探讨了重金属元素的富集程度,并运用地累积指数评估了沉积物的污染程度。根据1987年和2000年的数据,计算了重金属的累积速率。最后,讨论了自然作用和人类活动对微量元素的影响。
Trace elements of Taihu Lake are detected and their characteristics and variation trends are analyzed. The upper-crust standardized values of trace elements show that the pattern of the sediment is different from that of the rock. The concentrations of heavy metals, especially As, Hg, Cu, Zn and Ni, are relatively high in northern Taihu Lake, which is the major polluted source of heavy metals. We discuss the enrichment of heavy metals based on the background values and evaluate the pollution degree using the geoaccumulation index. The chart of element enrichment shows that Ni, Pb and Cu have larger enrichment levels than others. Based on the data of 1987 and 2000, we have calculated the accumulation rates of heavy metals in sediments. It is found that most of heavy metals are accumulated in the past decade. By comparison of elements between rock, soil and sediment, we also conclude that most of trace elements in sediments depend on weathering and natural processes, and only heavy metals as we know are affected by human activity.
出处
《地质论评》
CAS
CSCD
北大核心
2003年第5期552-560,共9页
Geological Review
基金
江苏省自然科学重点基金(编号 BK99204-1)
国土资源大调查项目(编号 0299203003)
