Scholarly record
FORMATION AND EARLY DEVELOPMENT OF MAGNESIUM SILICATE HYDRATE UNDER CONTROLLED CURING CONDITIONS
Abstract
Magnesium silicate hydrate (M-S-H) is a promising binder phase for the development of low carbon cementitious materials. However, its formation mechanisms, phase evolution, and dependence on curing conditions remain poorly understood, particularly during the early and intermediate stages of hydration. This study investigates the formation and development of M S-H in model systems using reactive MgO and diatomite as the silica source, focusing on Mg/Si molar ratios of 0.75, 0.90, 1.05, and 1.20 under controlled curing at 40 degrees Celsius and relative humidity exceeding 95% for 30 and 60 days. Phase evolution was monitored by X-ray diffraction (XRD) and microstructural development by scanning electron microscopy (SEM) combined with energy dispersive spectroscopy (EDS). The results demonstrate that elevated temperature curing is essential for M-S-H gel formation within practically relevant timescales, with characteristic amorphous XRD humps appearing exclusively in thermally activated samples and intensifying with prolonged curing duration. Lower Mg/Si ratios (0.75–0.90) promoted more advanced M-S-H development, while higher ratios retained excess unreacted brucite. SEM-EDS confirmed progressive infilling of diatomite frustule pores by fibrous M-S-H gel, with Mg/Si ratios in gel-rich zones of 0.6–1.0, consistent with reported M S H stoichiometry. This study provides the first systematic characterisation of M-S-H formation in MgO–diatomite systems under controlled curing, demonstrating that diatomite is a viable reactive silica source provided sufficient thermal activation is applied.
Publication details
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