2018
DOI: 10.1016/j.jcou.2018.08.025
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Characterization of Mg components in reactive MgO – Portland cement blends during hydration and carbonation

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Cited by 51 publications
(32 citation statements)
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“…Compared to the 20%‐0.55 and 20%‐0.50 mortars, the XRD pattern of the 20%‐0.45 mortar exhibits lower intensities corresponding to portlandite and greater intensities corresponding to Mg‐calcite, which agrees with the greatest carbonation front of the 20%‐0.45 mortar among the three mortars in Figure . The reaction mainly involves the carbonation of Mg 2+ and Ca 2+ forming Mg‐calcite . In terms of the thermal decomposition, M–S–H experiences a similar process as calcium silicate hydrate (C–S–H), which continues to a major mass loss at the temperature range of 50°C‐300°C .…”
Section: Resultsmentioning
confidence: 99%
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“…Compared to the 20%‐0.55 and 20%‐0.50 mortars, the XRD pattern of the 20%‐0.45 mortar exhibits lower intensities corresponding to portlandite and greater intensities corresponding to Mg‐calcite, which agrees with the greatest carbonation front of the 20%‐0.45 mortar among the three mortars in Figure . The reaction mainly involves the carbonation of Mg 2+ and Ca 2+ forming Mg‐calcite . In terms of the thermal decomposition, M–S–H experiences a similar process as calcium silicate hydrate (C–S–H), which continues to a major mass loss at the temperature range of 50°C‐300°C .…”
Section: Resultsmentioning
confidence: 99%
“…Nevertheless, the thermal decomposition of the residual M–S–H and C–S–H mainly contributes to the mass loss at the temperature range of 50°C‐300°C, corresponding to their dehydration process. Other than that, the character of TGA curves in Figure includes: (a) the mass loss and DTG peak at the temperature range of 50°C‐300°C are due to the dehydration of nesquehonite and the hydrated amorphous Mg carbonate; (b) the mass loss and DTG peak at the temperature range of 300°C‐480°C are due to the composition of brucite, nesquehonite, and the hydrated amorphous Mg carbonate; (c) the mass loss and DTG peak at the temperature range of 480°C‐650°C are due to the second step decarbonization of nesquehonite; and (d) the mass loss and DTG peak at the temperature range of 650°C‐950°C are due to the decomposition of Mg‐calcite. The TG curves of the 60%‐0.70 and 60%‐0.65 mortars yield similar mass losses at the aforementioned four temperature ranges, which manifests a comparable degree of carbonation.…”
Section: Resultsmentioning
confidence: 99%
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