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Study of REE concentrations and fractionation patterns in surface sediments in the Tinto and Odiel river estuary(SW Spain)

机译:Tinto和Odiel河口表层沉积物中稀土元素浓度和分馏模式研究 (sW西班牙)

摘要

Sc, Y, Th, Cu and rare earth elements (REE) concentrations have been analyzed in 14 samples of surfacesediments by means of ICP-MS. Mean concentrations of Sc, Y and Th in these sediments are lower thanthose presents in the Upper Continental Crust (UCC). Cu concentration is very high and is caused byinputs from the Odiel and Tinto rivers, affected by acid mine drainage. åREE mean concentration is lowerthan that observed in other rivers and estuaries. Plots of North American Shale Composite (NASC)-normalizedREE data of surface sediments show a slight depletion in REE concentrations. Most samples present withmiddle REE enrichment relative to light REE and heavy REE
机译:通过ICP-MS分析了14种表面沉积物样品中的Sc,Y,Th,Cu和稀土元素(REE)浓度。这些沉积物中Sc,Y和Th的平均浓度低于上地壳(UCC)中的浓度。铜的浓度非常高,是由奥迪尔河和廷托河的投入物造成的,并受到酸性矿山排水的影响。 •平均浓度低于其他河流和河口的平均浓度。北美页岩复合材料(NASC)归一化的REE地表数据显示REE浓度略有减少。相对于轻质稀土元素和重质稀土元素,大多数样品都具有中等稀土元素富集

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