放射性废物贮存地点地下水放射性污染的40年演变(俄罗斯联邦圣彼得堡地区)

V. Rumynin, В Г Румынин, D. N. Zamaskin, Д Н Замаскин, K. Vladimirov, К В Владимиров, A. Plotnikov, А. В. Плотников, I. A. Lelyavin, И А Лелявин, A. M. Nikulenkov, А М Никуленков, E. Kaplan, Е М Каплан, V. A. Khodina, В А Ходина
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引用次数: 0

摘要

基于放射性废物贮存场40年的监测数据,研究了20世纪90年代放射性废物泄漏引起的氚和β污染羽流的演变。发现局部和区域尺度的水动力学是控制氚污染在含水层系统中扩散的主要特征,而β -活性羽流的空间分布受到90Sr / 137Cs同位素在岩石基质上的吸附的强烈限制。研究表明,该基地地下水系统实际上正处于从“历史”污染中恢复的阶段。专门的复杂调查方案旨在检查储存库建筑物中积累的水及其与地下水的相互联系,表明建筑物与周围含水层的隔离良好,目前没有RW向地下环境释放的证据。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Forty-year evolution of radioactive groundwater contamination at the site of radioactive waste storage (St. Petersburg region, Russian Federation)
Evolution of tritium and beta contamination plumes resulted from radioactive waste leakage in the 1990s has been studied based on 40-year-long monitoring data at the site of radioactive waste (RW) storage. Localand regional-scale hydrodynamics are found to be the main features controlling the spreading of tritium contamination in the aquifer system, while spatial distribution of beta-activity plume is strongly restricted by sorption of 90Sr и 137Cs isotopes onto rock matrix. The study performed proves that groundwater system at the site is actually in the stage of rehabilitation from the «historical» contamination. Special complex investigation program aimed on examination of water accumulated in repository buildings and its interconnection with groundwater, demonstrated good isolation of the buildings from the surrounding aquifers and no evidence of RW release to the subsurface environment nowadays.
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