首页> 外文期刊>Aquatic ecosystem health & management >Trace metal speciation in marine sediments from Sulaibikhat Bay, Kuwait
【24h】

Trace metal speciation in marine sediments from Sulaibikhat Bay, Kuwait

机译:科威特苏莱比哈特湾海洋沉积物中的痕量金属形态

获取原文
获取原文并翻译 | 示例
获取外文期刊封面目录资料

摘要

The chemical speciation of trace metals (Cd, Co, Cr, Cu, Ni, Pb and Zn) in marine sediments from Sulaibikhat Bay, Kuwait was determined using a three-step sequential extraction procedure. To obtain a mass balance, a fourth step, i.e. digestion and analysis of the residue was undertaken using a microwave-assisted acid digestion procedure. The sum of the 4 steps (acid-soluble + reducible + oxidizable + residual) was in good agreement with the total content (71-116%), suggesting that the microwave extraction procedure is efficient. The results showed that all metals except for Pb and Zn were present at higher percentages in the residual fraction. The reducible fraction was the next followed by the oxidizable fraction. The exchangeable fraction was least important as a host for most metals. The mobility order of exchangeable fraction of the elements in surface sediments decreased in the order Cd > Zn > Cu > Co > Pb > Ni > Cr; the reducible fraction in the order Pb > Zn > Cu > Cd > Co > Ni > Cr; the oxidizable fraction in the order Pb > Cu > Cd > Ni > Co > Zn > Cr, and the residual fraction in the order Cr > Ni > Co > Cu > Cd > Zn > Pb. The data showed that the speciation of trace elements in sediments close to a sewage outfall was different from that of sediment from other parts of Sulaibikhat Bay. This suggests that the contribution of the sewage outfall to metal pollution in adjacent marine area is positive and is associated with fine-grained sediments with high level of organic content, which are major controlling factors for the distribution of trace metals in this part of the Bay.
机译:使用三步顺序萃取程序确定了来自科威特苏莱比哈特湾的海洋沉积物中痕量金属(镉,钴,铬,铜,镍,铅,锌和铅)的化学形态。为了获得质量平衡,第四步,即使用微波辅助酸消化程序进行残留物的消化和分析。这四个步骤的总和(酸溶+可还原+可氧化+残留)与总含量(71-116%)非常吻合,表明微波提取工艺是有效的。结果表明,除Pb和Zn以外的所有金属均以较高的百分比残留。接下来是可还原部分,接着是可氧化部分。作为大多数金属的主体,可交换部分最不重要。表层沉积物中元素交换分数的迁移率顺序依次为Cd> Zn> Cu> Co> Pb> Ni> Cr。可还原分数为Pb> Zn> Cu> Cd> Co> Ni> Cr;氧化分数为Pb> Cu> Cd> Ni> Co> Zn> Cr,剩余分数为Cr> Ni> Co> Cu> Cd> Zn> Pb。数据表明,靠近排污口的沉积物中微量元素的形态不同于苏莱比哈特湾其他地区的沉积物。这表明污水排污口对邻近海域金属污染的贡献是正的,并且与有机物含量高的细颗粒沉积物有关,这是该海湾该地区微量金属分布的主要控制因素。 。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号