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垃圾流化床焚烧炉灰渣的矿物学和孔隙水化学

Mineralogy and pore water chemistry of a boiler ash from a MSW fluidized-bed incinerator.

机构信息

BRGM (French Geological Survey), Environment and Processes Division, 3 Avenue C. Guillemin, Orléans Cedex, France.

出版信息

Waste Manag. 2010 Jul;30(7):1280-9. doi: 10.1016/j.wasman.2010.01.020. Epub 2010 Feb 11.

Abstract

This paper presents an investigation of the mineralogy and pore water chemistry of a boiler ash sampled from a municipal solid waste fluidized-bed incinerator, subject to 18 months of dynamic leaching in a large percolation column experiment. A particular focus is on the redox behaviour of Cr(VI) in relation to metal aluminium Al(0), as chromium may represent an environmental or health hazard. The leaching behaviour and interaction between Cr(VI) and Al(0) are interpreted on the basis of mineralogical evolutions observed over the 18-month period and of saturation indices calculated with the geochemical code PhreeqC and reviewed thermodynamic data. Results of mineralogical analyses show in particular the alteration of mineral phases during leaching (e.g. quartz and metal aluminium grains), while geochemical calculations suggest equilibria of percolating fluids with respect to specific mineral phases (e.g. monohydrocalcite and aluminium hydroxide). The combination of leaching data on a large scale and mineralogical analyses document the coupled leaching behaviour of aluminium and chromium, with chromium appearing in the pore fluids in its hexavalent and mobile state once metal aluminium is no longer available for chromium reduction.

摘要

本文研究了从城市固体废物流化床焚烧炉中采集的锅炉灰渣的矿物学和孔隙水化学,该灰渣在大型渗滤柱实验中经过 18 个月的动态浸出。特别关注的是 Cr(VI)的氧化还原行为与金属铝 Al(0)之间的关系,因为铬可能对环境或健康构成危害。浸出行为和 Cr(VI)与 Al(0)之间的相互作用是根据 18 个月期间观察到的矿物演化以及使用地球化学代码 PhreeqC 计算的饱和度指数和审查的热力学数据来解释的。矿物分析的结果特别显示了浸出过程中矿物相的变化(例如石英和金属铝颗粒),而地球化学计算表明渗滤流体与特定矿物相之间的平衡(例如一水碳酸钙和氢氧化铝)。大规模浸出数据和矿物分析的结合证明了铝和铬的耦合浸出行为,一旦金属铝不再可用于铬还原,铬就会以六价态和可移动态出现在孔隙流体中。

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