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首页> 外文期刊>Minerals Engineering >Secondary mineral phases associated with a historic arsenic calciner identified using automated scanning electron microscopy; a pilot study from Cornwall, UK
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Secondary mineral phases associated with a historic arsenic calciner identified using automated scanning electron microscopy; a pilot study from Cornwall, UK

机译:使用自动扫描电子显微镜鉴定与历史砷煅烧炉相关的次生矿物相;来自英国康沃尔郡的初步研究

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Historical polymetallic mining in Cornwall, UK has resulted in significant soil contamination. In particular the processing and refinement of arsenic in purpose built calciners has resulted in areas of localised, but extremely high contamination of soils with arsenic. Consequently, there is concern regarding the impact of this historic arsenic contamination on the local population. In this study automated scanning electron microscopy has been carried out to identify the phase distribution of arsenic within soil samples from: (a) adjacent to a calciner chimney, (b) adjacent to the calciner works and (c) for comparison, a sample of residue from the calciner dumps. Whilst the soil samples contain between 200 and 3325 ppm arsenic, the calciner residue contains approximately 12 percent arsenic. Although arsenopyrite is present in all the samples examined it is rare. Instead, the dominant arsenic mineral species present are As-Fe oxides which occur in a range of textural settings including: rims around coal, coke and fly ash particles; secondary phases infilling porosity with coal and coke particles; rims around silicate minerals and as a secondary phase cementing silicate grains and coal fragments together. In addition, in the sub 20 mu m size fraction from the calciner residue samples up to 15 percent of the grains present are As-Fe oxides, and of these many of the grains are less than 10 mu m in size and are potentially inhalable. These new data are significant in our understanding of the long-term dispersal of arsenic in the environment and its potential bioavailability.
机译:英国康沃尔郡的多金属开采历史悠久,造成了严重的土壤污染。特别是专用煅烧炉中砷的加工和精制导致局部地区的砷污染,但土壤污染极高。因此,人们担心这种历史性砷污染对当地居民的影响。在这项研究中,已经进行了自动扫描电子显微镜检查,以从以下位置确定土壤样品中砷的相分布:(a)靠近煅烧炉烟囱,(b)靠近煅烧炉工厂,以及(c)作为比较的样品煅烧炉垃圾堆中的残留物。虽然土壤样品中的砷含量为200至3325 ppm,但煅烧炉的残留物中砷含量约为12%。尽管毒气石存在于所有检查的样品中,但很少见。取而代之的是,存在的主要砷矿物物种是As-Fe氧化物,其存在于多种构造环境中,包括:煤,焦炭和粉煤灰颗粒周围的轮辋;第二阶段用煤和焦炭颗粒填充孔隙;在硅酸盐矿物周围形成轮缘,并作为第二相将硅酸盐颗粒和煤碎块粘合在一起。另外,在来自煅烧炉残余物样品的小于20微米的颗粒中,多达15%的颗粒是As-Fe氧化物,其中许多颗粒的尺寸小于10微米,并且可能被吸入。这些新数据对我们了解砷在环境中的长期扩散及其潜在的生物利用度具有重要意义。

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