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Physical dispersion of radioactive mine waste at the rehabilitated Radium Hill uranium mine site, South Australia

机译:南澳大利亚Radium Hill铀矿场经过修复的放射性矿山废料的物理扩散

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摘要

The Radium Hill uranium deposit, in semi-arid eastern South Australia, was discovered in 1906 and mined for radium between 1906 and 1931 and for uranium between 1954 and 1961 (production of 969 300 t of davidite ore averaging 0.12% U3O8). Rehabilitation was limited to removal of mine facilities, sealing of underground workings and capping of selected waste repositories. In 2002, gamma-ray data and samples of tailings, uncrushed and crushed waste rock, stream sediment, topsoil and vegetation were collected to assist in examination of the current environmental status of the mine site. The data indicate that capping of tailings storage facilities did not ensure the long-term containment of the low-level radioactive wastes due to the erosion of sides of the impoundments. Moreover, wind erosion of waste fines (phyllosilicates, ore minerals) from various, physically unstable waste repositories has caused increasing radiochemical (from a background dose of 35-70 nSv/hr to max. 0.94 Sv/hr) and geochemical (Ce, Cr, La, Lu, Rb, Sc, Th, U, V, Y, Yb) impacts on local soils. Plants (saltbush, pepper tree) growing on waste dumps display evidence of biological uptake of lithophile elements, with values being up to 1-2 orders of magnitude above values for plants of the same species at background sites. However, radiation doses associated with the mine and processing site average 0.67 Sv/hr; hence, visitors to the Radium Hill site will not be exposed to excessive radiation levels. Although rehabilitation procedures have been partly successful in reducing dispersion of U and related elements into the surrounding environment, it is apparent that 20 years after rehabilitation, there is significant physical and limited chemical mobility, including transfer into plants. Additional capping and landform design of the crushed waste and tailings repositories are required in order to minimise erosion and impacts on surrounding soils and sediments.
机译:位于南澳大利亚州半干旱东部的Radium Hill铀矿床于1906年被发现,并于1906年至1931年之间开采了镭,并于1954年至1961年之间开采了铀(生产了969300吨da石矿石,平均U3O8含量为0.12%)。修复仅限于拆除矿山设施,密封地下作业以及对选定的废物库进行封顶。 2002年,收集了伽马射线数据以及尾矿,未破碎和破碎的废石,河流沉积物,表土和植被的样品,以帮助检查矿区当前的环境状况。数据表明,由于蓄水池两边的侵蚀,尾矿存储设施的封顶不能确保对低放射性废物的长期控制。此外,来自各种物理上不稳定的废物库的废物细粉(页硅酸盐,矿石矿物)的风蚀已导致放射化学(从35-70 nSv / hr的本底剂量增加到最大0.94Sv/ hr)和地球化学(Ce Cr,La,Lu,Rb,Sc,Th,U,V,Y,Yb)对当地土壤的影响。在废物堆上生长的植物(盐灌木,胡椒树)显示出对嗜石生物元素的生物吸收的证据,其值比背景物种处相同物种的植物的值高1-2个数量级。但是,与矿山和加工场所相关的辐射剂量平均为0.67Sv/ hr;因此,访问Radium Hill网站的访客不会受到过多的辐射。尽管康复程序在减少U和相关元素向周围环境的扩散方面取得了部分成功,但是很明显,康复后20年,物理迁移和化学迁移受到限制,包括转移到植物中。需要对压碎的废物和尾矿库进行额外的封盖和地形设计,以最大程度地减少侵蚀和对周围土壤和沉积物的影响。

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