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Natural iron-aluminosilicate as potential solid precursor for supplementary cementitious materials: A comparative
Joelle Nadia Nouping Fekoua1,2,3,4, Paul Venyite1,2, Seunkole Bila5
1Laboratory of Applied Inorganic Chemistry, University of Yaounde I, P.O. Box 812, Yaoundé, Cameroon.
Geographic and climatic conditions influence laterite properties. These laterites, rich in aluminosilicates, show high reactivity and potential as supplementary cementitious materials.
Area of Science:
- Geochemistry and Materials Science
- Exploration of laterite deposits and their geopolymerization potential.
Background:
- Laterite properties are significantly influenced by geographic and climatic factors.
- Understanding these influences is crucial for utilizing laterites in geopolymer applications.
Purpose of the Study:
- To investigate the impact of geographic and climatic conditions on laterite properties.
- To evaluate the geopolymerization potential of laterites from different regions of Cameroon.
Main Methods:
- Analysis of four laterite deposits from diverse geographical zones in Cameroon.
- Characterization using Infrared (IR) spectroscopy and Brunauer-Emmett-Teller (BET) analysis.
- Assessment of particle size and microstructure.
Main Results:
- Laterites from high rainfall areas (center, south) exhibited higher iron content compared to arid regions (north, west).
- All studied laterites showed characteristic aluminosilicate IR absorption bands and high BET surface areas, especially after calcination.
- Despite variations in laterization, all laterites demonstrated near-complete conversion to geopolymers, with iron content affecting microstructure.
Conclusions:
- Laterite properties are demonstrably linked to their geographic origin and associated climate.
- The particle size, high BET surface area, and reactivity of these laterites position them as viable alternatives to metakaolin and other supplementary cementitious materials.
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