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Concentrations and Distribution Patterns of Rare Earth Elements in Various Factors of Water Body from Intertidal Flat of Tianjin

机译:天津市潮间带水体各要素中稀土元素的浓度分布格局

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摘要

Concentrations and distribution patterns of rare earth elements ( REEs) in the intertidal flat of Tianjin were studied using P 507 resin and ICP-MS analytical technology. The results show that average concentrations of REEs in the filtered(dissolved REEs) , unfiltered and interstitial water are 0. 461 mu g centre dot L~(-1), 4. 98 mu g centre dot L~(-1) and 0. 845 mu g centre dot L~(-1) , respectively. Their distribution patterns are similar to those in inland natural rivers, but quite different from those in oceans. The average concentrations of REEs in sediments and suspended matters are 161.2 mg centre dot L~(-1) and 168. 1 mg centre dot L~(-1) , respectively, which are much lower than those in sediments of natural rivers but higher than those in sediments of the continental shelf of East China Sea. It is suggested that REEs in sediments and suspended matters of intertidal flat can have mainly originated from terrestrial soils and thus their transportation and transformation processes are similar with those in rivers, and different from those in continental shelves. Pollutants discharged into the Bohai Bay do centre dot not cause significant effect on REEs in the intertidal flat of Tianjin yet.
机译:利用P 507树脂和ICP-MS分析技术研究了天津潮间带稀土元素的浓度和分布规律。结果表明,过滤后的(溶解的REEs),未过滤的和填隙水中的稀土元素平均浓度为0. 461μg中心点L〜(-1),4。98μg中心点L〜(-1)和0。分别为845μg中心点L〜(-1)。它们的分布方式与内陆天然河流中的分布方式相似,但与海洋中的分布方式完全不同。沉积物和悬浮物中稀土元素的平均浓度分别为161.2 mg中心点L〜(-1)和1 mg中心点L〜(-1),远低于天然河流沉积物中的REEs浓度,但较高比东海大陆架沉积物中的沉积物要多。建议潮间带沉积物和悬浮物中的稀土元素可能主要来源于陆地土壤,因此它们的迁移和转化过程与河流相似,与大陆架不同。排入环渤海湾的污染物的中心点对天津的潮间带的稀土元素尚未产生显着影响。

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