首页> 外文期刊>Environmental Geochemistry and Health >HEAVY METALS IN THE BED AND SUSPENDED SEDIMENTS OF ANYANG RIVER, KOREA: IMPLICATIONS FOR WATER QUALITY
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HEAVY METALS IN THE BED AND SUSPENDED SEDIMENTS OF ANYANG RIVER, KOREA: IMPLICATIONS FOR WATER QUALITY

机译:韩国安养河床和悬浮沉积物中的重金属:对水质的影响

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The objective of this study is to compare Anyang River bed sediments with water chemical composition and to assess the anthropogenic chemical inputs into the river system. Eight sampling locations were chosen along the river channel. Bed and suspended river sediments and water samples were collected, and analyzed for their chemical and physical composition. Data revealed that trace element concentrations in the river water were generally below world average, except for As, Mn, Ni and Cr. Among the three phases: water, bed and suspended sediment, more than 99% of the trace elements was associated with the bed sediment. Concentrations of trace elements in the sediment were a function a particle size distribution and organic content. The calculated degrees of enrichment based on the least influenced sample (ASD 1) indicated the river sediments were enriched with respect to background. The enrichment factors for Pb, Zn and As were relatively lower than for Cr, Co, Ni and Zn. The difference in the enrichment seems to reflect the human activities influence in the basin, and specially for Cd. Speciation of the elements in the five different chemical forms in the sediment by sequential extraction indicated that the reducible fraction was predominant for Fe, Zinc and Cu showed an irregular variation among the different fractions; whereas, Cd and Pb were more regular. Zinc and Cu highly existed mostly in exchangeable forms. Acid soluble and reducible forms were also important for most metals. The speciation implies that the metals associated with the sediment are subject to release into water bodies as goechemical variables (pH and Eh) change. Currently, the introduced metals are deposited near the source area and are mostly associated with the sediment, implying that the river bed sediment acts mainly as a sink, rather than a pool. The accumulated and enriched toxic trace elements can pose a potential pollution of river water.
机译:这项研究的目的是比较安阳河床沉积物与水化学成分,并评估人为化学物质输入河系的情况。沿河道选择了八个采样点。收集河床和悬浮河沉积物和水样,并对其化学和物理组成进行分析。数据显示,除砷,锰,镍和铬外,河水中痕量元素的浓度一般都低于世界平均水平。在水,床层和悬浮沉积物这三个阶段中,超过99%的微量元素与床层沉积物有关。沉积物中微量元素的浓度是粒径分布和有机物含量的函数。根据影响最小的样本(ASD 1)计算的富集程度表明,河流沉积物相对于本底富集。铅,锌和砷的富集因子相对低于铬,钴,镍和锌的富集因子。富集的差异似乎反映了盆地中人类活动的影响,特别是对于镉。通过连续萃取对沉积物中五种不同化学形式的元素进行形态分析表明,铁,锌和铜的还原性组分居多,不同组分之间存在不规则变化。而Cd和Pb更规则。锌和铜主要以可交换形式存在。酸溶和可还原形式对大多数金属也很重要。这种形态意味着与沉积物相关的金属会随着Goechemical变量(pH和Eh)的变化而释放到水体中。目前,引入的金属沉积在源区附近,并且大多与沉积物有关,这意味着河床沉​​积物主要起着汇的作用,而不是水池的作用。积累并富集的有毒微量元素可能对河水构成潜在污染。

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