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Characterization and microstructure observation of sintered red mud-fly ash mixtures at various elevated temperature

机译:不同温度下烧结红泥-粉煤灰混合物的表征和微观结构观察

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This study investigated the characterization and microstructure observation of sintered red mud fly ash mixtures at Various elevated temperature. The detailed analysis of the phase evolution during sintering process of red mud and fly ash as the function of sintering temperature were explored. Phase evolution and microstructure observation were carried out by X-ray diffraction method (XRD) and scanning electron microscope (SEM) method. Thermal analysis was carried out by thermogravimetric and differential thermal (TG-DTA) analysis. The mineralogical evolution revealed that quartz and goethite originates from the parent composition of red mud and fly ash. Microstructure observation revealed the transformation of globular grains towards elongated grains during the sintering process. Mass loss around 11% is observed in the thermal analysis patterns due to the dehydration, hydroxide-oxide phase transitions from iron (primary phase) and aluminum (secondary phase). The phase transition, evolution and dissolution as the function of sintering temperature were correlated as the function of temperature and the amount of fly ash content. The disappearance and appearance of the different phases confirms the decomposition and formation reaction suggested by thermal analysis. (C) 2015 Elsevier Ltd. All rights reserved.
机译:本研究研究了在各种高温下烧结赤泥粉煤灰混合物的表征和微观结构观察。深入研究了赤泥和粉煤灰烧结过程中的相变与烧结温度的关系。通过X射线衍射法(XRD)和扫描电子显微镜(SEM)进行相变和显微组织观察。通过热重分析和差热分析(​​TG-DTA)进行热分析。矿物学演化表明,石英和针铁矿起源于赤泥和粉煤灰的母体成分。显微组织观察表明,在烧结过程中球状晶粒向细长晶粒转变。在热分析模式中,由于脱水,铁(初级相)和铝(次级相)的氢氧化物-氧化物相变而在质量分析中观察到大约11%的质量损失。相变,析出和溶解与烧结温度有关,与温度和粉煤灰含量有关。不同相的消失和出现证实了热分析表明的分解和形成反应。 (C)2015 Elsevier Ltd.保留所有权利。

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