首页> 外文期刊>Arabian Journal for Science and Engineering >Distribution and Environmental Risk Evaluation of Metals in Sediment Cores from Marmara Ere ˘ glisi Shelf, Marmara Sea, Turkey
【24h】

Distribution and Environmental Risk Evaluation of Metals in Sediment Cores from Marmara Ere ˘ glisi Shelf, Marmara Sea, Turkey

机译:土耳其马尔马拉海马尔马拉海峡沉积层中沉积物芯中金属的分布和环境风险评估

获取原文
获取原文并翻译 | 示例
       

摘要

This paper studies trace element contents in core sediments from Marmara Ereglisi on the northern shelf of the Marmara Sea.The main objective is to detect the concentrations of the selected elements (Al, As, Cr, Cu, Fe, Mn, Ni, Pb, V and Zn) andhistorical evolution of sediment quality. The average concentrations of elements in mg/kg are 17,500 for Al, 5 for As, 70 forCr, 12 for Cu, 10,742 for Fe, 137 for Mn, 44 for Ni, 20 for Pb, 43 for V and 44 for Zn. The average percentages of the sand,silt and clay fractions are 17%, 36% and 47%, respectively. Based on contamination factor, enrichment factor and pollutionload index, computed from carbonate-free metal values, the core sediments are unpolluted for Al, Cr, Cu, Fe, Mn, Ni and Vfor the entire length of the cores and moderately polluted for As, Pb and Zn in the upper parts of the cores. The relative metalenrichment in cores starts at core depths of 13 to 39 cm depending on sedimentation rates, which commonly increase fromthe outer shelf toward the coast. Considering the sedimentation rates, the metal pollution on outer and inner shelf areas startedabout 400–500 years ago. Contamination of the northern shelf sediments is insignificant compared to those of the southernshelf, the semi-enclosed bays and gulf areas of the Marmara Sea with large catchment areas having a high population densityand agricultural activities, as well as with similar marine shelf areas elsewhere in the world. This is mainly due to the smallcatchment area and the dynamic circulation system of the Marmara Ereglisi Shelf area.
机译:本文研究了马尔马拉海北部陆架Marmara Ereglisi核心沉积物中的微量元素含量,主要目的是检测选定元素(Al,As,Cr,Cu,Fe,Mn,Ni,Pb, V和Zn)与沉积物质量的历史演变。元素的平均浓度(mg / kg)为:Al为17,500,As为5,Cr为12,Cu为10,742,Mn为137,Mn为44,Ni为20,Pb为20,V为V,Zn为44。沙,粉砂和粘土部分的平均百分比分别为17%,36%和47%。根据污染因子,富集因子和污染负荷指数(由不含碳酸盐的金属值计算得出),在整个核芯中,芯沉积物未受到Al,Cr,Cu,Fe,Mn,Ni和V的污染,而对As受到中度污染,芯上部为Pb和Zn。岩心中相对的金属富集起始于岩心深度13到39 cm(取决于沉积速率),沉积速率通常从外层到海岸增加。考虑到沉积速度,外架子和内架子区域的金属污染始于大约400-500年前。与南部大陆架,马尔马拉海的半封闭海湾和海湾地区相比,北部大陆架沉积物的污染微不足道,马尔玛拉海的集水区面积大,人口密度高,农业活动活跃,在马尔他海其他地方也有类似的海洋大陆架区域世界。这主要是由于小集水区和Marmara Ereglisi货架区的动态循环系统。

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