1995
DOI: 10.1016/0008-8846(95)00104-k
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Hydration of portland cement clinker in the presence of carbonaceous materials

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Cited by 17 publications
(9 citation statements)
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“…FTIR spectra of the powder form of the collected three different branded OPC cement of Patan city were taken to identify their functional groups and the results of the FTIR spectra are shown in Figs 1-3. The FTIR absorption peak at 3642 cm -1 is assigned to the O-H stretching of Ca (OH) 2 formed [11]; [12]; [13]; [14] and the intensity of this peak is generally increased with the hydration time. However, two different branded cement samples of the Brand-1 and Brand-3, except Brand-2 sample used in this study did not show a wide absorption peak in the region of 3000-3700 cm -1 which indicates that these two cement samples of the Brand-1 and Brand-3 analyzed here does not contain a large amount of water molecule, but the cement sample of Brand-2 sample has a very broad absorption band between this region as sown in Fig.…”
Section: Resultsmentioning
confidence: 99%
“…FTIR spectra of the powder form of the collected three different branded OPC cement of Patan city were taken to identify their functional groups and the results of the FTIR spectra are shown in Figs 1-3. The FTIR absorption peak at 3642 cm -1 is assigned to the O-H stretching of Ca (OH) 2 formed [11]; [12]; [13]; [14] and the intensity of this peak is generally increased with the hydration time. However, two different branded cement samples of the Brand-1 and Brand-3, except Brand-2 sample used in this study did not show a wide absorption peak in the region of 3000-3700 cm -1 which indicates that these two cement samples of the Brand-1 and Brand-3 analyzed here does not contain a large amount of water molecule, but the cement sample of Brand-2 sample has a very broad absorption band between this region as sown in Fig.…”
Section: Resultsmentioning
confidence: 99%
“…[27]. The presence of calcite is confirmed by the intensification of the band at 3652 cm -1 [28]. The intensity of the broad stretching vibration at around 3400 cm -1 increases This result suggests that the former band was due to the vibrations of the hydroxide of CSH [19,[27][28][29] and of the physisorbed water.…”
Section: Chemical and Mineralogical Characterizationmentioning
confidence: 85%
“…In the high zone, the C0 spectrum presents a very acute peak at 3645 cm -1 , whose intensity increases with the hydration time. This is assigned to the O-H stretching of Ca(OH) 2 formed [13][14][15][16] .…”
Section: Ir-analysismentioning
confidence: 99%