4.4 Article

Role of calcination on geopolymerization of lateritic clay by alkali treatment

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JOURNAL OF SAUDI CHEMICAL SOCIETY
卷 25, 期 3, 页码 -

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ELSEVIER
DOI: 10.1016/j.jscs.2021.101198

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Lateritic clay; Calcination; Metakaolin; Disorderness; Geopolymer

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The study investigated the role of calcination in synthesizing geopolymer using a low iron lateritic clay sample, analyzing the effects of different temperatures on the material's properties. Results showed that higher calcination temperatures led to improved quality of the geopolymer.
In the present study, the role of calcination of a low iron lateritic clay sample was investigated to synthesize the geopolymer. The analyses like X-ray fluorescence (XRF) spectroscopy for chemical composition, X-ray diffractometry (XRD) for mineral composition, and Fourier transform infrared (FT-IR) spectroscopy & scanning electron microscopy (SEM) for structural changes upon calcination at 500, 700 and, 900 degrees C were used to assess the suitability of selected lateritic clay sample for geopolymer. The drop in electrical conductivity and greater consumption of calcium hydroxide by CS-900 confirmed its potential reactivity than CS-700, CS-500, and CS-Control. The quality of geopolymer derived from un-calcined and calcined lateritic clay samples by alkali activation was evaluated by comparing results of compressive strength, water absorption test, and stability in the aggressive environment of chloride, FT-IR, XRD, and SEM analyses. The experimental results reveal that the quality of geopolymer enhances as the calcination temperature of the lateritic clay sample increases, However, calcination of the lateritic clay sample at 900 degrees C gives significant results and yield good quality geopolymer with 24.8 MPa of compressive strength, 7.07% of water absorption and 2.22% loss in mass in an aggressive environment. (c) 2021 Published by Elsevier B.V. on behalf of King Saud University. This is an open access article under the CC BY-NC-ND license (http://creativecommons.org/licenses/by-nc-nd/4.0/).

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