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作 者:田海涛[1] 张振克[1] 丁海燕[1] 李彦明[1] 孟红明[1]
机构地区:[1]南京大学地理与海洋科学学院海岸与海岛开发教育部重点实验室
出 处:《湖泊科学》2008年第5期600-604,共5页Journal of Lake Sciences
基 金:国家自然科学基金项目(40471128)资助
摘 要:根据石梁河水库沉积物粒度和重金属元素(Cu,Cr,Zn,AS和Pb)含量的分析,结合137Cs放射性比活度精确定年,研究了石梁河水库沉积速率和重金属的污染变化特征,并利用地累积指数法评价了重金属的污染程度.结果表明:石梁河水库40年来平均淤积速率为3.85cm/a,Cu,Cr和Zn地累积指数一直小于1,处于轻微污染;As污染水平变化较大,现处于低水平的轻度污染;Pb污染水平自柱底始持续恶化,目前地累积指数大于1,且有污染加剧趋势.According to the analysis of the grain size, content of heavy metals (Cu, Cr, Zn, As and Pb) and ^137Cs dating in Shilianghe Reservoir, the sedimentary rate and pollution characteristic of heavy metals were investigated, The geo-accumulation index was used to assess the pollution degree of heavy metals. It showed that the averaged sedimentary rate was 3.85cm/a, and Cu, Cr and Zn were in the light polluted level with the geo-accumulation index less than I during the past 40 years. The geo-accumulation index of As fluctuated strongly, but now it was in the light polluted level. The geo-accumulation index of Pb was more than 1, and the pollution level increased gradually from the bottom of the core and trends to aggravate.
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