Scientific publications
2024Journal articleEnglishOpen access
Dissolution of Volcanic Ash in Alkaline Environment for Cold Consolidation of Inorganic Binders (opens in a new tab)
Authors
University of Yaoundé I
Philippe Douwe
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Scientific publications
Philippe Douwe
Giovanni Dal Poggetto
Other affiliations: North Carolina State University · Ferrari (Italy)
Antonio Stroscio
Other affiliations: University of Catania · Ferrari (Italy)
Elie Kamseu
Other affiliations: National Radiation Protection Agency of Cameroon · Ferrari (Italy)
Isabella Lancellotti
Other affiliations: Ferrari (Italy)
Cristina Leonelli* (Corresponding author)
Other affiliations: Ferrari (Italy)
Materials
A systematic study on the dissolution in concentrated alkali of two volcanic ashes from Cameroon, denoted as DAR and VN, is presented here. One volcanic ash, DAR, was 2 wt% richer in Fe and Ca and 4 wt% lower in Si than the other, designated as VN. Such natural raw materials are complex mixtures of aluminosilicate minerals (kaersutite, plagioclase, magnetite, diopside, thenardite, forsterite, hematite, and goethite) with a good proportion of amorphous phase (52 and 74 wt% for DAR and VN, respectively), which is more reactive than the crystalline phase in alkaline environments. Dissolution in NaOH + sodium silicate solution is the first step in the geopolymerisation process, which, after hardening at room temperature, results in solid and resistant building blocks. According to XRD, the VN finer ash powders showed a higher reactivity of Al-bearing soluble amorphous phases, releasing Al cations in NaOH, as indicated by IPC-MS. In general, dissolution in a strong alkaline environment did not seem to be affected by the NaOH concentration, provided that it was kept higher than 8 M, or by the powder size, remaining below 75 µm, while it was affected by time. However, in the time range studied, 1-120 min, the maximum element release was reached at about 100 min, when an equilibrium was reached. The hardened alkali activated materials show a good reticulation, as indicated by the low weight loss in water (10 wt%) when a hardening temperature of 25 °C was assumed. The same advantage was found for of the room-temperature consolidated specimens' mechanical performance in terms of resistance to compression (4-6 MPa). The study of the alkaline dissolution of volcanic ash is, therefore, an interesting way of predicting and optimising the reactivity of the phases of which it is composed, especially the amorphous ones.