首页> 外文期刊>Radiocarbon >RADIOCARBON AND OTHER ENVIRONMENTAL ISOTOPES IN THE GROUNDWATER OF THE SITES FOR A PLANNED NEW NUCLEAR POWER PLANT IN LITHUANIA
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RADIOCARBON AND OTHER ENVIRONMENTAL ISOTOPES IN THE GROUNDWATER OF THE SITES FOR A PLANNED NEW NUCLEAR POWER PLANT IN LITHUANIA

机译:立陶宛计划中的新核电站厂区地下水中的放射性碳和其他环境同位素

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摘要

The assessment of construction sites for the new Visaginas Nuclear Power Plant (Visaginas NPP), including groundwater characterization, took place over the last few years. For a better understanding of the groundwater system, studies on radiocarbon; tritium; stable isotopes of hydrogen, oxygen, and carbon; and helium content were carried out at the location of the new NPP, at the Western and Eastern sites, as well as in the near-surface repository (NSR) site. Two critical depth zones in the Quaternary aquifer system were characterized by different groundwater residence times and having slightly different stable isotope features and helium content. The first shallow interval of the Quaternary multi-aquifer system consists of an unconfined aquifer and semiconfined aquifer. The second depth interval of the system is related to the lower Quaternary confined aquifer. Groundwater residence time in the first flow system was mainly based on tritium data and ranges from 6 to 60 yr. These aquifers are the most important in terms of safety assessment and are considered as a potential radionuclide transfer pathway in safety assessment. Groundwater residence time in the lower Quaternary aquifers based on ~(14)C data varies from modern to several thousand years and in some intervals up to 10,500 yr.
机译:最近几年,对新的维萨吉纳斯核电站(维萨吉纳斯核电厂)的建筑工地进行了评估,包括地下水特征分析。为了更好地了解地下水系统,进行了放射性碳研究;氚;氢,氧和碳的稳定同位素;氦含量是在新核电厂的地点,西部和东部地点以及近地表储存库(NSR)地点进行的。第四纪含水层系统中的两个临界深度带的特征是地下水停留时间不同,稳定同位素特征和氦含量也略有不同。四元多重含水层系统的第一个浅层间隔由一个非承压含水层和一个半承压含水层组成。该系统的第二深度间隔与下部第四纪承压含水层有关。第一流系统中的地下水停留时间主要基于tri数据,范围为6至60年。就安全性评估而言,这些含水层是最重要的,并被视为安全性评估中潜在的放射性核素转移途径。根据〜(14)C数据,较低的第四纪含水层中的地下水停留时间从现代到数千年不等,并且在某些时间间隔内长达10,500年。

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