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Trace metals in porewater of surface sediments and their bioavailability in Jiaozhou Bay, Qingdao, China

机译:青岛胶州湾表层沉积物孔隙水中的痕量金属及其生物利用度

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Samples of porewater and the edible tissue of mottled clams, Ruditapes variegatus, were collected simultaneously at each of 12 stations from Jiaozhou Bay near Qingdao, China, in June of 2003. Chemical analysis focused on trace metals and major elements. Porewater concentrations of Cd, Cr, Pb, and Zn were distributed in a bimodal fashion among the 12 stations, with mean concentrations at six of the stations being 8–32 times mean values at the other six stations. The concentrations of the same metals in clams were remarkably similar among stations, the coefficients of variation being only 12–37%. Calculations performed with the computer program PHREEQC indicated that Pb and Cr in porewater were present only in the +2 and +3 states, respectively, and because dissolved Cd and Zn exist only in the +2 state, the bimodal distribution of these four metals likely reflects secondary effects associated with their scavenging by Fe and/or Mn under oxidizing conditions and subsequent dissolution in the reducing environment of the porewaters. Consistent with this hypothesis is the fact that the distribution of high and low metal concentrations was closely correlated with the granularity of the sediment, with lower metal concentrations associated with relatively coarse sediment. Comparison of published biological concentration factors with the ratios of metal concentrations in the clams to porewater metal concentrations indicated that the porewaters were not the primary sources of the metals in the clams. Mixing processes in the bay likely account for the rather uniform concentrations of metals in clam tissue.
机译:2003年6月,从中国青岛附近的胶州湾的12个站点中的每一个站点同时采集了斑驳的蛤Ru(Ruditapes variegatus)的孔隙水和可食组织样品。化学分析的重点是痕量金属和主要元素。 Cd,Cr,Pb和Zn的孔隙水浓度以双峰方式分布在12个站点中,其中六个站点的平均浓度是其他六个站点平均值的8–32倍。蛤stations中相同金属的浓度在各个站点之间非常相似,变异系数仅为12-37%。用计算机程序PHREEQC进行的计算表明,孔隙水中的Pb和Cr分别仅以+2和+3状态存在,并且由于溶解的Cd和Zn仅以+2状态存在,因此这四种金属的双峰分布很可能反映了与它们在氧化条件下被铁和/或锰清除以及随后在孔隙水的还原环境中溶解有关的次级影响。与这一假设相一致的事实是,高和低金属浓度的分布与沉积物的粒度密切相关,而较低的金属浓度则与相对较粗的沉积物有关。将已发表的生物浓度因子与蛤中金属浓度与孔隙水中金属浓度之比进行比较,结果表明,孔隙水不是蛤中金属的主要来源。海湾中的混合过程可能是蛤tissue组织中金属浓度相当均匀的原因。

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