用于陶瓷工业的芬兰采矿尾矿的增值

IF 1.3 4区 地球科学 Q2 GEOLOGY
Soili Solismaa, A. Ismailov, Marjaana Karhu, Harisankar Sreenivasan, M. Lehtonen, P. Kinnunen, M. Illikainen, M. Räisänen
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引用次数: 21

摘要

本研究对芬兰尾矿废物进行了估价,以确定使用陶瓷技术的机会。根据其矿物学和化学含量,选择的五种尾矿废物分别代表富含石英和碱性长石的长英质尾矿(FMT)、以含镁和含铁矿物为主的尾矿(MgFeMT)和富含碳酸盐矿物的尾矿(CMT)。初步中试研究表明,FMT材料是制备莫来石类陶瓷的潜在次原料。由于所研究尾矿的Al2O3含量太低,无法进行毛拉石化,因此需要添加Al。此外,含Ca硅酸盐的碳酸盐尾矿可用于化学键合磷酸盐陶瓷(CBPC)的合成。根据文献综述,FMT是生产地质聚合物的可行原料,但高的初始Si:Al比(在富含石英的FMT中)可能导致部分地质聚合物化。预热的金云母与偏高岭土混合的地质聚合物的初步结果给出了有希望的发现,形成了具有良好抗压强度的地质聚合物。这些发现支持了富含金云母的MgFeMT材料用于生产碱活性陶瓷的可行性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Valorization of Finnish mining tailings for use in the ceramics industry
The present study valorized Finnish mining tailings waste to identify opportunities for the use of ceramics technologies. On the basis of their mineralogical and chemical contents, the five selected tailings wastes represented felsic mining tailings (FMT) rich in quartz and alkali feldspars, mining tailings dominated by Mgand Fe-bearing minerals (MgFeMT), and mining tailings rich in carbonate minerals (CMT). Preliminary pilot studies indicated that the FMT materials are potential secondary raw materials for mullite-type ceramics. An Al additive was needed, since the Al2O3 content of the studied tailings was too low for mullitization. In addition, carbonate-bearing tailings with Ca silicates can be applicable for chemically bonded phosphate ceramic (CBPC) synthesis. Based on a literature review, FMT are viable source materials for the production of geopolymers, but a high initial Si:Al ratio (in quartz-rich FMT) may lead to partial geopolymerization. Preliminary results from the geopolymerization of pre-heated phlogopite mica mixed with metakaolin gave promising findings, with the formation of a geopolymer having good compressive strength. The findings support the viability of MgFeMT materials rich in phlogopite mica for the production of alkali-activated ceramics.
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来源期刊
CiteScore
1.30
自引率
0.00%
发文量
5
审稿时长
>12 weeks
期刊介绍: Bulletin of the Geological Society of Finland (BGSF) publishes research articles and short communications in all branches of geosciences. Contributions from outside Finland are welcome, provided that they contain material relevant to Finnish geology or are of general interest.
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