Pozzolanic and Cementing Activity of Raw and Pyro-Processed Saudi Arabian Red Mud (RM) Waste

O. Alelweet, S. Pavia, Z. Lei
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引用次数: 6

Abstract

This paper investigates the composition, properties and reactivity of a red mud waste generated in Saudi Arabia with a view to find alternative materials to replace construction binders of high environmental impact. The phase transformation triggered by the sintering of the RM up to 1000°C is determined with thermal and X-Ray Diffraction analyses. Reactivity is investigated with chemical and physical methods including the Chapelle test, setting times, mechanical index and microscopy. The RM is clearly pozzolanic, and its activity is mainly due to the reaction of feldespathoids and the formation of zeolitic and feldspathoid-based hydrates. The positive effects of the thermal treatment are seen below 750°C, and include the loss of water in the zeolite/feldespathoids, and the destruction of the crystal structures of the clay minerals inherited form the parent bauxite. The negative effects of the thermal treatment are evidenced over 750°C, with a decrease in specific surface area, devitrification and crystal formation, whereby the active transition aluminas and the fedespathoids/zeolites (mainly cancrinite) transform into nepheline, tricalcium aluminate (C3A) and gehlenite. Despite the occurrence of nepheline, C3A and gehlenite in the RM sintered at 1000°C, the formation of pozzolanic hydrates that cause setting and strength development are greater at lower temperature. The optimum thermal treatment that enhances pozzolanic activity lies at c.400°C, as evidenced by the highest lime combination, the greatest mechanical index and the fastest set. The RM consists of gibbsite and boehmite, inherited from the bauxite, and cancrinite, chantalite and sodalite formed during the Bayer process. Feldespathoids have formed, instead of zeolites, due to the available silica and the high alkali content of the RM. The quick lime -CaO -, added twice during the refining process, has transformed the original goethite into hematite, and produced cancrinite. The Saudi RM has high SiO2 and high alkalinity, and an abundant specific surface area available for reaction. The chloride and carbon contents are low, and no environmental toxicity is inferred from its chemistry.
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生料和热处理沙特阿拉伯红泥(RM)废料的火山灰和固井活性
本文研究了沙特阿拉伯产生的一种红泥废物的组成、性质和反应性,以期找到替代材料来取代高环境影响的建筑粘合剂。通过热分析和x射线衍射分析确定了RM烧结到1000°C时引发的相变。用化学和物理方法考察反应性,包括夏贝尔试验、凝固时间、机械指数和显微镜。RM具有明显的火山灰性质,其活性主要是由于蛭石的反应以及沸石和长石基水合物的形成。在750°C以下的温度下,热处理的积极影响包括沸石/硬石中的水分损失,以及从母体铝土矿继承的粘土矿物的晶体结构的破坏。在750°C以上,热处理的负面影响表现为比表面积减小、脱硝和晶体形成,活性过渡氧化铝和原石/沸石(主要是癌质岩)转变为霞石、铝酸三钙(C3A)和辉长石。尽管在1000℃烧结的RM中存在霞石、C3A和辉长石,但在较低温度下形成的火山灰水合物更多,从而导致凝固和强度发展。提高火山灰活性的最佳热处理温度为C .400℃,石灰组合最高,力学指标最大,凝固速度最快。其中铝土矿由继承铝土矿的三水铝石和薄水铝石,以及拜耳过程形成的红灰岩、闪长石和钠长石组成。由于可用的二氧化硅和RM的高碱含量,形成了Feldespathoids,而不是沸石。在精炼过程中,两次加入生石灰- cao -,使原针铁矿转化为赤铁矿,生成癌辉石。沙特RM具有高SiO2和高碱度,具有丰富的反应比表面积。氯化物和碳的含量很低,从化学性质上看没有环境毒性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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