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波兰南部地下水中镭-222和镭-226活度浓度:新数据及部分成因关系

Rn and Ra activity concentrations in groundwaters of southern Poland: new data and selected genetic relations.

作者信息

Przylibski Tadeusz A, Gorecka Joanna, Kula Agata, Fijałkowska-Lichwa Lidia, Zagożdżon Katarzyna, Zagożdżon Paweł, Miśta Wojciech, Nowakowski Robert

机构信息

Division of Geology and Mineral Waters, Institute of Mining Engineering, Faculty of Geoengineering, Mining and Geology, Wrocław University of Technology, Wybrzeże S. Wyspiańskiego 27, 50-370 Wrocław, Poland.

Faculty of Geoengineering, Mining and Geology, Graduated Master of Science of Wrocław University of Technology, Wybrzeże S. Wyspiańskiego 27, 50-370 Wrocław, Poland.

出版信息

J Radioanal Nucl Chem. 2014;301(3):757-764. doi: 10.1007/s10967-014-3215-x. Epub 2014 Jun 8.

Abstract

Since 2008, the authors have been conducting research into Rn and Ra activity concentrations in shallow circulation groundwaters in southern Poland. Measurements have been performed with a liquid-scintillation method and ultra low-level liquid-scintillation spectrometers α/β Quantulus 1220. The research carried out so far has demonstrated that in the Sudetes groundwaters with high activity concentrations of Rn and Ra are common. In other studied areas in southern Poland no shallow circulation groundwaters with high radon or radium concentrations have been found yet. The conducted research has demonstrated that the activity concentration of Rn dissolved in shallow circulation groundwaters in the Sudetes depends chiefly on the amount of radon, which after being released as gas from reservoir rocks is dissolved in waters flowing through these rocks. At the same time, the concentration of Rn dissolved in some shallow circulation groundwaters in the Carpathians is influenced significantly by the amount of radon produced from the decay of its parent ion Ra dissolved in these waters.

摘要

自2008年以来,作者一直在对波兰南部浅层循环地下水中的氡和镭活度浓度进行研究。测量采用液体闪烁法,使用超低本底液体闪烁光谱仪α/β Quantulus 1220进行。迄今为止开展的研究表明,在苏台德地区,地下水中氡和镭的活度浓度较高的情况很常见。在波兰南部的其他研究区域,尚未发现氡或镭浓度较高的浅层循环地下水。已开展的研究表明,苏台德地区浅层循环地下水中溶解的氡活度浓度主要取决于氡的含量,氡从储层岩石中以气体形式释放后溶解在流经这些岩石的水中。与此同时,喀尔巴阡山脉一些浅层循环地下水中溶解的氡浓度受到溶解在这些水中的母离子镭衰变产生的氡量的显著影响。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/3c6d/4514591/013626f3cf23/10967_2014_3215_Fig1_HTML.jpg

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