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Geochemical survey of the occurrence of trace metals in thermal groundwaters from Sicily, (Southern Italy)

机译:地球化学调查,来自西西里岛(意大利南部)的热水中的微量金属

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The concentrations of 15 minor and trace elements were determined in 28 groundwater samples collected throughout Sicily. Thermal manifestations (T= 20-98°C) associated both with active volcanic areas (Etna, Pantelleria, Aeolian Islands) and with seismogenetic area (Belice area, Longi-Taormina fault zone) were selected for the present investigation. Trace metal concentrations range from a few tenths of μg/1 for ultra-trace elements (U, Y, Cs) up to 1-10 mg/1 for minor elements (Sr, Fe, Li, Rb). Due to the costal location of many sampling sites, seawater contribution is often important, at least for alkaline and earth-alkaline elements. However, the trace metal content is controlled by factors such as the master variables of the weathering solution (T, pH, Eh), the composition of the host rocks and the saturation state for primary and secondary mineral phases
机译:在整个西西里岛收集的28个地下水样品中确定了15种微量元素和痕量元素的浓度。选择与活动火山区(埃特纳火山,潘泰莱里亚,风神群岛)和地震成因区(贝利斯区,隆吉-塔尔米纳断裂带)相关的热力表现(T = 20-98°C)进行此次研究。痕量金属的浓度范围从超痕量元素(U,Y,Cs)的十分之一微克/ 1到次要元素(Sr,Fe,Li,Rb)的1-10 mg / 1。由于许多采样点的位置昂贵,至少对碱性和碱土金属元素而言,海水的贡献通常很重要。但是,痕量金属的含量受诸如风化溶液的主要变量(T,pH,Eh),基质岩石的组成以及主要和次要矿物相的饱和状态等因素控制。

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