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Entrapment of pollutants in Mediterranean sediments and biogeochemical indicators of their impact

机译:地中海沉积物中污染物的截留及其影响的生物地球化学指标

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The transit and fate of certain pollutants (Cd, Pb, Zn and P) transported to the western Mediterranean sea-floor and a method to assess their impact are described. The spatial distribution of pollutant concentrations in the Rhone prodelta shows that their decline with distance from their source is due both to mixing with unpolluted sediments, release from contaminated particles during transit and release from sediments after deposition. Beyond the continental shelf, metals of anthropogenic origin, mainly incorporated in faecal pellets, sink and become entrapped in deep sea sediments. Because subsaturating concentrations of trace metals are often found in surface pore waters and storage, therefore, still occurs, co-precipitation with other metal ions existing in slightly supersaturated states has also to be considered. Although phosphate tends to precipitate as apatite after entering sea water, its 'definitive' storage in sediments is hindered by certain forms of pollution. Low pH and reducing conditions in sediments enhance phosphate release to the overlying water. Eutrophication may then occur in localized areas. The effects of urban waste water contamination on biogeochemical processes in sediments are examined, in particular processes responsible for the transformation of organic nitrogen. Sediment quality appears to the better defined by the effectiveness of diagenetic processes than by pollutant concentration per se. In general, polluted sediments possess weak capacities to transform organic nitrogen relative to the quantities of organic matter that are available. Such sediment characteristics are indicated by the preferential growth of Caulerpa taxifolia over that of Posidonia oceanica.
机译:描述了某些污染物(Cd,Pb,Zn和P)运到地中海西部海底的过境和归宿,以及评估其影响的方法。罗纳河三角洲中污染物浓度的空间分布表明,污染物浓度随着距污染源的距离而下降,这是由于与未污染的沉积物混合,在运输过程中从受污染的颗粒中释放以及在沉积后从沉积物中释放而造成的。除大陆架之外,主要掺入粪便颗粒中的人为来源的金属下沉并陷于深海沉积物中。由于在地表孔隙水和储存中经常会发现痕量金属的过饱和浓度,因此仍然会发生,因此还必须考虑与存在于过饱和状态的其他金属离子共沉淀。尽管磷酸盐在进入海水后往往会以磷灰石的形式沉淀,但某些形式的污染会阻碍其在沉淀物中的“确定性”储存。较低的pH值和沉积物中的还原条件会增加磷酸盐向上方水的释放。富营养化然后可能会发生在局部区域。研究了城市废水污染对沉积物中生物地球化学过程的影响,特别是负责有机氮转化的过程。成岩过程的有效性似乎比污染物本身的浓度更好地定义了沉积物质量。通常,相对于可用有机物的数量,受污染的沉积物转换有机氮的能力较弱。这种沉积物特征由Caulerpataxifolia优先生长于Posidonia oceanica的特征表明。

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