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首页> 外文期刊>Journal of the European Ceramic Society >In situ observation of the dissolution phenomena of SiC particle in CaO–SiO_2–MnO slag
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In situ observation of the dissolution phenomena of SiC particle in CaO–SiO_2–MnO slag

机译:SiC颗粒在CaO–SiO_2–MnO炉渣中的溶解现象的原位观察

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The dissolution of SiC particle at 1600 ℃ in the CaO–SiO_2–MnO slag was observed in situ by means of confocal scanning laser microscopy in order to make the determination of dissolution mechanism. The SiC particle is initially wetted by molten slag from the outer surface and the wetting between SiC and slag phase is more dominant in the composition of higher CaO/SiO_2 ratio. When the SiC particle is wetted by molten slag, the gas bubbles that are mainly CO gas is generated by the reaction between SiC and MnO in slag phase and are continuously evolved at the wetted area, which is pronounced as the CaO/SiO_2 ratio increases. The dissolution of SiC particle in the slag through the reaction with MnO is enhanced in the composition of higher CaO/SiO_2 ratio not only due to greater thermodynamic driving force but also due to accelerated mass transport kinetics.
机译:用共聚焦扫描激光显微镜原位观察了SiC颗粒在CaO-SiO_2-MnO熔渣中1600℃的溶解情况,从而确定了溶解机理。最初,SiC颗粒被外表面的熔融炉渣润湿,并且在较高的CaO / SiO_2比组成中,SiC和炉渣相之间的润湿更为明显。当SiC颗粒被熔融炉渣润湿时,主要是CO气体的气泡是通过炉渣相中的SiC和MnO之间的反应产生的,并且在润湿区域连续放出,这随着CaO / SiO_2比的增加而明显。通过与MnO的反应,SiC颗粒在炉渣中的溶解在较高的CaO / SiO_2比组成中得到增强,这不仅是由于更大的热力学驱动力,而且还因为加速了的物质传输动力学。

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