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Non-Traditional Utilization of Uranium Deposits After Underground Mining Completion

机译:地下采矿完成后的铀矿床非传统利用

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摘要

In the course of the development and exploitation of particular uranium deposits, the chemism of mine waters changes depending upon the extent of infiltration area, the total volume of worked-out mineral, its mineralogical composition and also the achieved depth of mining. In the course of flooding the underground mine after its closure many important changes occur in the content of dissolved substances in waters that increases several times (uranium, radium, iron, and others). Mine waters of flooded former uranium mines thus represent, with reference to their considerable volumes, a significant source of uranium. The paper presents the partial results of running research project dealing with possibilities of the intensive utilisation of mine waters from flooded uranium mines as a source of uranium with an accompanying effect of shortening the time necessary for the purification of mine waters discharged into watercourses.
机译:在特定铀矿床的开发和开发过程中,矿山水的化学取决于渗透面积的程度,加工矿物的总体积,其矿物学组合物以及实现的深度。在填补地下矿井后,在封闭后淹没了许多重要变化,在水域中的溶解物质的含量上发生了几次(铀,镭,铁等)。因此,淹没的前铀矿的矿山是参考他们相当大的铀的重要来源。本文提出了运行研究项目的部分结果,处理矿水从洪水铀矿区密集利用的可能性,具有缩短挖掘进入水道的矿山水域所需的时间。

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