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Chemical characteristics of the waters of a uranium mineralized zone in NW Spain

机译:NW西班牙铀矿化区水的化学特征

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In Sageras-Mina Fe there are more than 100 boreholes drilled to investigate the mineral resources of the deposit. 35 boreholes were selected in order to analyze the chemical composition of groundwaters based on their depth and situation around the uranium ore. Groundwater samples come from 50 to 150 m depth. The waters are classified as calcium-bicarbonate type waters, with a redox potential that indicates they are slightly reduced (values vary between 50 to -350 mV). The TOC varies between <0.1 and 4.0 mgC/L and the dissolved uranium has a maximum value of 7.7 mg/L.The tritium contents in the groundwaters vary between 1.5 and 7.3 T.U. Considering that the mean value of tritium in rainwater from the studied area has a value of 4 T.U., the residence times of the groundwaters are relatively short, not longer than 50 years in the oldest case.
机译:在Sageras-Mina Fe中,钻了100多个钻孔,以调查矿床的矿产资源。选择了35个钻孔,以基于铀矿周围的深度和情况分析地下水的化学成分。地下水样本深度50至150米。水分为碳酸氢钙型水分,具有氧化还原电位,表示它们略微降低(值在50至-350 mV之间变化)。 TOC在<0.1和4.0mgc / L之间变化,溶解的铀的最大值为7.7mg / L.地下水中的氚含量在1.5和7.3 t.u之间变化。考虑到研究从研究区域的雨水中氚的平均值具有4℃。,地下水的停留时间相对较短,在最旧的情况下不超过50年。

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