Chałupnik Stanisław, Wysocka Małgorzata, Janson Ewa, Chmielewska Izabela, Wiesner Marta
Central Mining Institute, 40-166 Katowice, Pl. Gwarkow 1, Poland.
Central Mining Institute, 40-166 Katowice, Pl. Gwarkow 1, Poland.
J Environ Radioact. 2017 May;171:117-123. doi: 10.1016/j.jenvrad.2017.02.007. Epub 2017 Feb 22.
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 and Ra. 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 Ra and Ra are released into the rivers with mine effluents, causing the contamination of bottom sediments and river banks. The results of radioactivity monitoring of effluents and river waters are presented here to illustrate a trend of long-term changes in environmental contamination, caused by mining industry in the Upper Silesian Region.
根据国际原子能机构(IAEA,2016年)的最新指南,煤矿开采是职业暴露的最重要贡献因素之一。煤矿开采导致的职业暴露占工人每年集体剂量总量的约45%。采矿过程中的一个暴露源是天然放射性核素浓度升高的地层卤水,最常见的是镭(Ra)和镭(Ra)。镭同位素经常出现在波兰上西里西亚地区(USCB)地下煤矿的地层水中。大量镭以自发沉淀或水处理产生的放射性沉积物的形式留在地下。这种现象导致矿工面临的辐射危害增加。镭(Ra)和镭(Ra)的剩余活度随矿井废水排放到河流中,导致底部沉积物和河岸受到污染。本文展示了废水和河水放射性监测结果,以说明上西里西亚地区采矿业造成的环境污染长期变化趋势。