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Long term changes in the concentration of coal mines and Upper Silesian rivers of radium in discharge waters

机译:排放水中的煤矿和镭的上西里西亚河浓度长期变化

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摘要

According to the latest guidelines of the International Atomic Energy Agency (IAEA, 2016), coal mining is one of the most important contributors to occupational exposure. Coal mining contributes about 45% of the total annual collective dose obtained by workers due to the exposure at places of working. One of the sources of exposure in mining are formation brines with elevated concentrations of natural radionuclides, the most common are radium Ra-226 and Ra-228. Radium isotopes often occur in formation waters in underground collieries in the Upper Silesian region (USCB) in Poland. Significant amounts of radium remain underground in the form of radioactive deposits created as a result of spontaneous deposition or water treatment. This phenomenon leads to the increase of radiation hazard for miners. The remaining activities of 226Ra and 228Ra are released into the rivers with mine effluents, causing the contamination of bottom sediments and river banks.
机译:根据国际原子能机构(IAEA,2016)的最新指南,煤矿开采是造成职业暴露的最重要因素之一。由于工作地点的暴露,煤矿开采贡献了工人每年集体总剂量的约45%。采矿中的暴露源之一是天然放射性核素浓度升高的地层盐水,最常见的是镭Ra-226和Ra-228。波兰上西里西亚地区(USCB)的地下煤矿,地层水中经常发生镭同位素。大量镭以自发沉积或水处理产生的放射性沉积物形式残留在地下。这种现象导致矿工的辐射危害增加。 226Ra和228Ra的剩余活动随矿山废水释放到河流中,导致底部沉积物和河岸受到污染。

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