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Tidal salt marsh sediment in California, USA. Part 2: Occurrence and anthropogenic input of trace metals

机译:潮汐盐沼沉积物在加利福尼亚,美国。第2部分:痕量金属的发生和人为输入

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Surface sediment samples (0-5 cm) from 5 tidal salt marshes along the coast in California, USA were analyzed to investigate the occurrence and anthropogenic input of trace metals. Among study areas, Stege Marsh located in the central San Francisco Bay was the most contaminated marsh. Concentrations of metals in Stege Marsh sediments were higher than San Francisco Bay ambient levels. Zinc (55.3-744 μg g~(-1)) was the most abundant trace metal and was followed by lead (26.6-273 μg g~(-1)). Aluminum normalized enrichment factors revealed that lead was the most anthropogenically impacted metal in all marshes. Enrichment factors of lead in Stege Marsh ranged from 8 to 49 (median = 16). Sediments from reference marshes also had high enrichment factors (2-8) for lead, indicating that lead contamination is ubiquitous, possibly due to continuous input from atmospherically transported lead that was previously used as a gasoline additive. Copper, silver, and zinc in Stege Marsh were also enriched by anthropogenic input. Though nickel concentrations in Stege Marsh and reference marshes exceeded sediment quality guidelines, enrichment factors indicated nickel from anthropogenic input was negligible. Presence of nickel-rich source rock such as serpentinite in the San 'Francisco Bay watershed can explain high levels of nickel in this area. Coefficients of variation were significantly different between anthropogenically impacted and non-impacted metals and might be used as a less conservative indicator for anthropogenic input of metals when enrichment factors are not available.
机译:分析了美国加利福尼亚沿海5个潮汐盐沼的地表沉积物样本(0-5厘米),以调查痕量金属的发生和人为输入。在研究区域中,位于旧金山湾中部的Stege Marsh是受污染最严重的沼泽。 Stege Marsh沉积物中的金属浓度高于旧金山湾的环境水平。锌(55.3-744μgg〜(-1))是最丰富的微量金属,其次是铅(26.6-273μgg〜(-1))。铝归一化富集因子表明,铅是所有沼泽中受人为影响最大的金属。 Stege Marsh中铅的富集因子范围为8到49(中位数= 16)。参比沼泽的沉积物还具有较高的铅富集系数(2-8),这表明铅污染无处不在,这可能是由于先前用作汽油添加剂的大气运输铅的持续输入所致。 Stege Marsh的铜,银和锌也因人为投入而丰富。尽管Stege Marsh和参考沼中的镍浓度超过了沉积物质量指标,但是富集因子表明,人为输入的镍可以忽略不计。圣弗朗西斯科湾流域中富含蛇纹岩的富镍烃源岩可以解释该地区镍含量高的原因。人为影响的金属和非影响的金属之间的变异系数显着不同,并且在没有富集因子时,可以用作人类活动金属输入的较不保守的指标。

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