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Uranium in the Surrounding of San Marcos-Sacramento River Environment (Chihuahua Mexico)

机译:San Marcos-Sacramento河环境(墨西哥奇瓦瓦州)周围的铀

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摘要

The main interest of this study is to assess whether uranium deposits located in the San Marcos outcrops (NW of Chihuahua City, Mexico) could be considered as a source of U-isotopes in its surrounding environment. Uranium activity concentrations were determined in biota, ground, and surface water by either alpha or liquid scintillation spectrometries. Major ions were analyzed by ICP-OES in surface water and its suspended matter. For determining uranium activity in biota, samples were divided in parts. The results have shown a possible lixiviation and infiltration of uranium from geological substrate into the ground and surface water, and consequently, a transfer to biota. Calculated annual effective doses by ingestion suggest that U-isotopes in biota could not negligibly contribute to the neighboring population dose. By all these considerations, it is concluded that in this zone there is natural enhancement of uranium in all environmental samples analyzed in the present work.
机译:这项研究的主要目的是评估位于圣马科斯露头(墨西哥奇瓦瓦市西北部)的铀矿床是否可以被视为周围环境中的铀同位素来源。铀活度浓度通过α或液体闪烁光谱法确定了生物区,地下水和地表水中的铀。 ICP-OES分析了地表水及其悬浮物中的主要离子。为了确定生物区中的铀活性,将样品分成几部分。结果表明,铀可能从地质基质中浸出并渗入地下水和地表水,从而转移到生物区系。通过摄入计算得出的年度有效剂量表明,生物区系中的U同位素不能忽略地影响邻近人群的剂量。通过所有这些考虑,可以得出结论,在该区域中,本工作中分析的所有环境样品中的铀都有自然的增强。

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