Mineralogy Division, Mintek, South Africa.
Mineralogy Division, Mintek, South Africa.
J Hazard Mater. 2022 May 5;429:127588. doi: 10.1016/j.jhazmat.2021.127588. Epub 2021 Oct 23.
Prior to its termination, asbestos mining in South Africa was centred on the large crocidolite fields of the present day Northern Cape, the amosite (grunerite)-crocidolite fields of Limpopo, and chrysotile fields of Mpumalanga provinces. The legacy of these activities continues to affect surrounding communities in contemporary South Africa. The asbestos fields of Limpopo host two important former mining areas at Penge and at the Bewaarkloof near Chuenespoort. A large abandoned site is located southeast of Penge at Weltevreden, where there is no evidence of any rehabilitation. Two former mines, Lagerdraai and Uitkyk, are rehabilitated sites in an extensive string of closed mines that operated in the southern Bewaarkloof. Samples from the abandoned and rehabilitated mine sites were studied using semi-quantitative X-ray powder diffraction (XRD) to determine asbestos contamination levels in soils, and to assess distribution patterns of asbestos mineral species in the surrounding soils. Only where below detection (typically 1-3 mass%) from XRD, samples were assessed optically. The Weltevreden site, with no observable rehabilitation efforts, contrasts with the rehabilitated sites at Lagerdraai and Uitkyk. The predominant asbestiform mineral species at each site were successfully identified, with underlying geological asbestos mineral distribution trends recognised in the soils at the Bewaarkloof. Trace amounts of asbestiform minerals were identified in soils downstream of the Weltevreden mine, as well as in surrounding hillsides. The results indicate that XRD is a potentially useful tool for benchmarking sites yet to be rehabilitated as well as monitoring the effectiveness of previous rehabilitation efforts. The method is also a suitable first-pass for target areas that may require more detailed, time-consuming, and costly analysis.
在南非的石棉开采终止之前,主要集中在当今北开普省的大型蓝石棉矿区、林波波省的铁石棉(格里诺石)-蓝石棉矿区和姆普马兰加省的温石棉矿区。这些活动的遗留问题继续影响着当代南非的周边社区。林波波省的石棉矿区拥有两个重要的前矿区,一个是彭格(Penge),另一个是恰尼斯波尔特(Chuenespoort)附近的贝瓦阿克洛夫(Bewaarkloof)。彭格东南方向有一个大型废弃矿区,位于韦尔特弗伦丹(Weltevreden),那里没有任何恢复的迹象。拉格德拉伊(Lagerdraai)和乌特基克(Uitkyk)两个前矿是在贝瓦阿克洛夫南部广泛的一系列关闭矿中进行修复的矿区。使用半定量 X 射线粉末衍射(XRD)对废弃和修复的矿场样品进行研究,以确定土壤中的石棉污染水平,并评估周围土壤中石棉矿物种类的分布模式。只有在 XRD 检测不到(通常为 1-3%质量)的情况下,才会通过光学方法进行评估。韦尔特弗伦丹(Weltevreden)矿区没有观察到任何恢复工作,与拉格德拉伊(Lagerdraai)和乌特基克(Uitkyk)的修复矿区形成对比。每个矿区都成功地识别出主要的石棉矿物种类,并在贝瓦阿克洛夫(Bewaarkloof)的土壤中识别出潜在的地质石棉矿物分布趋势。在韦尔特弗伦丹(Weltevreden)矿区下游以及周围的山坡上,也发现了土壤中存在痕量的石棉矿物。结果表明,XRD 是一种用于基准化尚未修复的场地以及监测以前恢复工作效果的潜在有用工具。该方法也是针对可能需要更详细、耗时和昂贵分析的目标区域的合适初步方法。