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Metal concentrations and mobility in marine sediment and groundwater in coastal reclamation areas: A case study in Shenzhen, China

机译:沿海垦区海洋沉积物和地下水中金属的浓度和迁移率:以深圳为例

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摘要

The concentrations of metals in the buried marine sediment and groundwater were differently affected by land reclamation. Nine metals (V, Cr, Mn, Co, Ni, Cu, Zn, Cd and Pb) in sediment and coastal groundwater from reclamation areas in Shenzhen were examined. The gradually decreased concentrations (V, Cr, Mn, Ni, Cu, Zn) in sediment and relatively higher concentrations (V, Cr, Mn, Co, Ni, Cu and Cd) in ground-water within reclamation areas were observed. The increase of V, Cr, Mn, Ni, Cu and Cd concentrations in groundwater within reclamation areas subsequently after land reclamation should be resulted from the mobilization of these metals accumulated in the sediment. These metals appear to be easily mobilized from solid phase to solution phase after reclamation. The physico-chemical changes such as reduction in pH and salinity in water environment induced by land reclamation appear to be responsible for metal mobility in the sediment—groundwater system.
机译:土地开垦对海底沉积物和地下水中金属的浓度有不同的影响。考察了深圳垦区沉积物和沿海地下水中的九种金属(钒,铬,锰,钴,镍,铜,锌,镉和铅)。观察到填海区内地下水中的浓度(V,Cr,Mn,Ni,Cu,Zn)逐渐降低,而地下水中的较高浓度(V,Cr,Mn,Co,Ni,Cu和Cd)则相对较高。土地开垦后,开垦区随后地下水中V,Cr,Mn,Ni,Cu和Cd的浓度增加,应归因于这些沉积物中积累的这些金属的移动。在回收之后,这些金属似乎很容易从固相转移到固溶相。土地开垦引起的物理化学变化(例如pH值降低和水环境中的盐分降低)似乎是造成沉积物-地下水系统中金属迁移的原因。

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