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首页> 外文期刊>Applied Geochemistry: Journal of the International Association of Geochemistry and Cosmochemistry >Mineralogical, geochemical, and leaching study of historical Cu-slags issued from processing of the Zechstein formation (Old Copper Basin, southwestern Poland)
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Mineralogical, geochemical, and leaching study of historical Cu-slags issued from processing of the Zechstein formation (Old Copper Basin, southwestern Poland)

机译:Zechstein地层加工历史Cu-Slags的矿物学,地球化学和浸出研究(旧铜盆,波兰西南部)

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摘要

Historical Cu-Slags located at former industrial sites in Poland are exposed to weathering that may trigger release of metallic contaminants to the surrounding soils. However, the extent to which different metals are leached depends on the mineral composition of the slags and the conditions of their deposition. Historical slags are often crystalline and composed of phases with a variable response to weathering. Also, weathering of crystalline slags (CS) is different from that of amorphous slags (AS). To understand how the slag phase composition triggers weathering and the ultimate release of metallic elements, we studied the leaching of historical crystalline and amorphous slag. A combined geochemical and mineralogical approach determined the weathering sequence(s) of slag components subjected to different conditions of specific slag disposal. In detail, experiments under: i) various pH conditions in the range of 2-13 in a batch mode simulated slag deposition within a deep soil profile, whereas ii) exposure to solutions of artificial root exudates (ARE) in a dynamic experimental system simulated slag deposition within topsoil. The results demonstrated that crystalline phases in the order Leucite Plagioclase Pyroxene are preferentially dissolved in inorganic conditions of a pH = 7, in contrast to glass, which is preferentially dissolved in alkaline conditions (pH 7). Also, inorganic conditions better promote the dissolution of metal-bearing phases (sulphides and metals) when compared to silicates. In contrast, artificial root exudates do not show preferential dissolution of any phase and cause the strongest leaching in all of the analyzed conditions. We show that reconstructing the susceptibility of complex crystalline slags to weathering requires a specific approach including analyses and interpretation of all major components such as Ca, Mg and K, not merely a focus on Si and metals.
机译:位于波兰前工业部位的历史Cu-Slags暴露于风化,可能会触发到周围土壤的金属污染物的释放。然而,浸出不同金属的程度取决于炉渣的矿物成分和它们的沉积条件。历史渣通常是晶体的,并且由具有可变对风化的阶段组成。而且,结晶渣(CS)的风化不同于非晶渣(AS)。要了解渣相成分如何触发风化和金属元素的最终释放,我们研究了历史结晶和无定形炉渣的浸出。组合的地球化学和矿物学方法确定了经受特定熔渣处理的不同条件的炉渣部件的耐候序列。详细的实验:i)在深土剖面内的批量模式下模拟渣沉积在2-13的各种pH条件,而ii)在模拟动态实验系统中暴露于人造根部渗出物(AS)的溶液。甲渣沉积在表土内。结果表明,顺序效果阶段的结晶相& Plagioclase&与玻璃形成对比的玻璃,优选溶解在pH& = 7的无机条件下。此外,与硅酸盐相比,无机条件更好地促进金属轴承阶段(硫化物和金属)的溶解。相反,人工根部渗出物不显示任何相的优先溶解,并导致所有分析的条件中最强的浸出。我们表明,重构复杂结晶炉渣对风化的易感性需要一种特定的方法,包括分析和解释所有主要组件,如Ca,Mg和K,而不仅仅是Si和金属。

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