首页> 外文期刊>Continental Shelf Research: A Companion Journal to Deep-Sea Research and Progress in Oceanography >Processes affecting the distribution of dissolved trace metals in the North Aegean Sea (Eastern Mediterranean)
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Processes affecting the distribution of dissolved trace metals in the North Aegean Sea (Eastern Mediterranean)

机译:影响北爱琴海(地中海东部)中溶解的痕量金属分布的过程

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Dissolved Cd, Cu Ni and Mn were measured in the North Aegean Sea, during the MATER and INTERREG programmes, in order to evaluate the processes which control their distribution. The North Aegean receives the fresh waters from many of the rivers draining the Balkan Peninsula, as well as large amounts of brackish water from the Black Sea and the Sea of Marmara. Furthermore, the area consists of two shelf areas and discrete basins. Six sampling cruises were undertaken in the area, during three seasons (winter, spring, summer); a total of 402 samples were analysed. Trace metal levels in the area are comparable to those of other semi-closed Mediterranean regimes (Cd:0.018-0.278nM; Cu:0.56-6.85nM; Ni:2.22-18.6nM; Mn:0.068-44.0nM). The nutrient-like behaviour of Cd, Cu and Ni was not detectable. In contrast, surface enhancement of trace metals was apparent. The calculation of enrichment factors (E-f) showed that the two shelf areas were not enriched significantly in trace metals, relative to the deeper water parts of the system. Only Mn showed some degree of enrichment over the shelves. The transport of trace metals, towards the open waters, is controlled largely by the prevailing surface water circulation and mixing pattern of the two water masses-Black Sea Water and Levantine Intermediate Water. Occasionally, increases in Cu, Ni and Mn concentrations were observed at depth, near the slope or in the deep basins. (C) 2003 Elsevier Science Ltd. All rights reserved. [References: 55]
机译:在MATER和INTERREG计划期间,在北爱琴海对溶解的Cd,Cu Ni和Mn进行了测量,以评估控制其分布的过程。北爱琴海从流入巴尔干半岛的许多河流中获得淡水,并从黑海和马尔马拉海中获得大量咸淡水。此外,该区域由两个架子区域和不连续的盆地组成。在三个季节(冬季,春季,夏季)在该地区进行了六次采样巡游;总共分析了402个样品。该地区的痕量金属水平可与其他半封闭式地中海地区的金属水平相比(Cd:0.018-0.278nM; Cu:0.56-6.85nM; Ni:2.22-18.6nM; Mn:0.068-44.0nM)。 Cd,Cu和Ni的营养样行为无法检测到。相反,痕量金属的表面增强是明显的。富集因子(E-f)的计算表明,相对于系统中较深的水部分,两个架子区域未在痕量金属中大量富集。只有Mn在架子上显示出一定程度的富集。微量金属向开阔水域的运输在很大程度上受主要的地表水循环和两种水团(黑海水和黎凡特中间水)的混合方式控制。有时,在深处,斜坡附近或深盆地中观察到铜,镍和锰的浓度增加。 (C)2003 Elsevier ScienceLtd。保留所有权利。 [参考:55]

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