Eddy F. Yusslee and Nur Hazwani Dahon and Mohd Azrul Abd Rajak and Sazmal E. Arshad (2022) Hydrothermal transformation of metakaolinite under basic solution.
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Abstract
An amorphous metakaolinite was treated hydrothermally with 1.25M KOH solution at 190 °C during different reaction times ranging from 0 to 48 h. The products obtained were characterised by X-ray diffraction in order to determine their mineralogical characteristics. Two distinct mechanisms can explain the change of the precursor material in KOH solutions: (1) precipitation and (2) dissolution. At the initial stage, only gibbsite and quartz can be identified from the major peaks of the diffractograms, while after 12 hours, zeolite F and kalsilite have been formed before the formation of leucite after 48 hours.
Item Type: | Proceedings |
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Keyword: | Kaolinite, Crystals, Diffraction |
Subjects: | Q Science > QE Geology > QE1-996.5 Geology > QE351-399.2 Mineralogy T Technology > TN Mining engineering. Metallurgy > TN1-997 Mining engineering. Metallurgy > TN799.5-948 Nonmetallic minerals |
Department: | CENTRE > Preparation Centre for Science and Technology |
Depositing User: | SITI AZIZAH BINTI IDRIS - |
Date Deposited: | 10 Oct 2024 16:07 |
Last Modified: | 10 Oct 2024 16:07 |
URI: | https://eprints.ums.edu.my/id/eprint/41259 |
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