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Thorium accumulation in the sedimentary environment of the Vigo Ria (NW Iberian Peninsula)

机译:ium在维哥里亚(西北伊比利亚半岛)沉积环境中的积累

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摘要

Thorium levels and their association with Fe, Sc, Ca, and Particulate Organic Carbon (POC) were researched in sediments of the Vigo Ria in order to assess the influence of radioactive gneisses from the neighbouring continental Galineiro Complex. Sediment of 50 surface samples and 1 core was analysed by ICP-MS and the results were validated with certificate reference material from marine sediment. It was found that Th accumulates in the middle Ria zone (9-15 mg kg~(-1)) as a result of the terrestrial source. The thorium concentration in the Ria (average: 9.4 ±5.1 mg kg~(-1)) is not anthropogenically impacted in accordance with its own regional background level (11.4 ± 3.5 mg kg~(-1)), which is two times higher than the content in earth's crust. Throughout the relationship Th/Fe, Th may be associated with the iron cycle in the Ria, probably through iron oxy-hydroxide scavenging.
机译:在Vigo Ria的沉积物中研究了ium的含量及其与Fe,Sc,Ca和颗粒状有机碳(POC)的关系,以评估邻近大陆Galineiro Complex的放射性片麻岩的影响。用ICP-MS分析了50个表面样品和1个岩心的沉积物,并用海洋沉积物中的合格参考物质验证了结果。结果表明,由于陆源,Th积累在中部Ria区(9-15 mg kg〜(-1))。 Ria中的concentration浓度(平均值:9.4±5.1 mg kg〜(-1))不受其自身背景水平(11.4±3.5 mg kg〜(-1))的人为影响,是后者的两倍。比地壳中的含量高在整个Th / Fe关系中,Th可能与Ria中的铁循环有关,可能是通过羟基氧化铁清除。

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