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硬壳层和胶结层对矿山堆浸中氧气扩散系数的影响:扩散实验与模拟研究。

The impact of hardpans and cemented layers on oxygen diffusivity in mining waste heaps: diffusion experiments and modelling studies.

机构信息

Instituto Geológico y Minero de España, Plaza de España, Torre Norte, 41013 Sevilla, Spain.

出版信息

Sci Total Environ. 2011 Aug 1;409(17):3197-205. doi: 10.1016/j.scitotenv.2011.04.055. Epub 2011 May 31.

Abstract

This study reports column tests and modelling results to assess the impact of hardpans and cemented layers on oxygen supply in mine waste sediments. The analysed sediment samples were obtained from a low-sulphide and low-carbonate polymetallic mine waste tailings impoundment located in the Freiberg mining district in Germany. The three samples were characterised by different degrees and types of cementation. After physical and mineralogical properties of the samples had been determined, breakthrough curves of oxygen were measured in column studies at different degrees of water saturation, and the diffusivities were assessed using a numerical modelling approach. Results demonstrate that cemented layers and hardpans in undisturbed sediments associated with fine-grained material operate as preferential pathways for diffusive gas transport during rewetting, leading to higher oxygen diffusivities compared to disturbed sediments. Under air-dry conditions, the disturbed samples show higher diffusivities than the undisturbed sample, indicating clogging of the porosity by precipitation of secondary minerals such as trivalent Fe oxyhydroxides acting as a barrier and thereby decreasing the diffusivity of the undisturbed sample. In contrast to sediments without cementation, diffusion experiments of sediments with cemented layers used in this study yield similar tortuosities in spite of their different grain size distributions, pointing to the important role of these heterogeneities for gas diffusion.

摘要

本研究报告了柱试验和建模结果,以评估硬结层和胶结层对矿山废物沉积物中氧气供应的影响。所分析的沉积物样品取自德国弗赖贝格矿区的一个低硫化物和低碳碳酸盐多金属矿山废物尾矿坝。这三个样本的胶结程度和类型不同。在确定了样品的物理和矿物性质之后,在不同水饱和度的柱研究中测量了氧气的突破曲线,并使用数值建模方法评估了扩散系数。结果表明,与细粒物质相关的未扰动沉积物中的硬结层和硬底层在重新润湿时作为扩散气体传输的优先途径,与受扰沉积物相比,氧气扩散系数更高。在干燥空气条件下,受扰样品的扩散系数高于未受扰样品,这表明沉淀的三价铁氢氧化物等次生矿物堵塞了孔隙,形成了屏障,从而降低了未受扰样品的扩散系数。与没有胶结的沉积物相比,尽管本研究中使用的具有胶结层的沉积物的粒径分布不同,但扩散实验得到了相似的迂曲度,这表明这些非均质性对气体扩散起着重要作用。

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