铀
烧结
土壤水分
材料科学
土壤污染
冶金
矿物学
核化学
化学
环境科学
土壤科学
作者
Fen Luo,Hexi Tang,Xiaoyan Shu,Shunzhang Chen,Bingsheng Li,Keyou Shi,Yi Xie,Dadong Shao,Xirui Lu
标识
DOI:10.1016/j.jnoncrysol.2020.120551
摘要
To dispose of uranium-contaminated soil, the microwave sintering technology was used. A series of uranium-contaminated soils were successfully immobilized via microwave sintering for 30 min. When the amount of uranium ranges from 0 wt % to 1 wt %, glass phase occurred in saline-alkali soil, purple soil and red soil, while glass with presence of a crystalline phase occurred in yellow soil. The FT-IR analysis showed that the uranium-contaminated soils were mainly consist of [SiO4] units. The Qn distribution of Si-O tetrahedrons and network connectivity of 1 wt % uranium doped sintered soils were related to the composition of soils. The uranium ions were almost immobilized and evenly distributed in sintered soils. Theoretical results showed that the structures of uranium doped sintered soils were made of Si-O, Al-O and Fe-O tetrahedrons. The O-Si-O linkage was the most preferred one among all linkages and the network forming ability of Si was higher than Al.
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