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城市生活垃圾焚烧底灰的矿物学特征研究,重点关注重金属赋存相。

Mineralogical characterization of municipal solid waste incineration bottom ash with an emphasis on heavy metal-bearing phases.

机构信息

Graduate School of Engineering, Kyushu University, 744 Motooka, Nishi-ku, Fukuoka 819-0395, Japan.

出版信息

J Hazard Mater. 2011 Mar 15;187(1-3):534-43. doi: 10.1016/j.jhazmat.2011.01.070. Epub 2011 Jan 22.

Abstract

Municipal solid waste incineration (MSWI) bottom ash contains a considerable amount of heavy metals. The occurrence and uneven distribution of these heavy metals in bottom ash can increase the complexity of such residues in terms of long-term behavior upon landfilling or recycling. Bottom ashes sampled from three stoker-type incinerators in Japan were analyzed in this paper. This study presents detailed information on the mineralogical characterization of bottom ash constituents and the weathering behavior of these constituents by means of optical microscopy and scanning electron microscopy. It was revealed that bottom ash mainly consists of assorted silicate-based glass phases (48-54 wt% of ash) and mineral phases including melilites, pseudowollastonite, spinels, and metallic inclusions (Fe-P, Fe-S, Fe-Cu, Cu-Sn, Cu-Zn, Cu-S, and Cu-Pb dominated phases), as melt products formed during the incineration process. The compounds embedded in the glass matrix, e.g. spinels and metallic inclusions, played the most important role in concentration of heavy metals (Pb, Zn, Cu, Cr, Mn, Ni, etc.). Other phases such as refractory minerals and ceramics, frequently found in ash, were of less significance in terms of their influence on the involvement of heavy metals. Analysis of lab-scale artificially weathered and 10-year landfilled bottom ash samples revealed that secondary mineralization/alteration of the bottom ash constituents principally carbonation and glass evolution substantially decreased the potential risk of the heavy metals to the surrounding environment.

摘要

城市固体废物焚烧(MSWI)底灰含有相当数量的重金属。这些重金属在底灰中的存在和不均匀分布增加了这些残留物在填埋或回收利用时长期行为的复杂性。本文分析了来自日本三台炉排炉焚烧炉的底灰样本。该研究通过光学显微镜和扫描电子显微镜详细介绍了底灰成分的矿物学特征以及这些成分的风化行为。结果表明,底灰主要由各种硅酸盐基玻璃相(占灰分的 48-54wt%)和矿物相组成,包括辉沸石、假硅灰石、尖晶石和金属夹杂物(Fe-P、Fe-S、Fe-Cu、Cu-Sn、Cu-Zn、Cu-S 和 Cu-Pb 为主的相),这些是在焚烧过程中形成的熔融产物。嵌入玻璃基质中的化合物,如尖晶石和金属夹杂物,在重金属(Pb、Zn、Cu、Cr、Mn、Ni 等)的浓缩方面起着最重要的作用。其他相,如耐火矿物和陶瓷,在影响重金属参与方面的意义较小,经常在灰烬中发现。对实验室规模人工风化和 10 年填埋底灰样本的分析表明,底灰成分的次生矿化/蚀变主要是碳酸化和玻璃演化,大大降低了重金属对周围环境的潜在风险。

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