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2005
DOI: 10.1016/j.cemconres.2004.10.045
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Natural cement as the precursor of Portland cement: Methodology for its identification

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Cited by 77 publications
(41 citation statements)
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“…This band decreased in size as the curing time was extended in the spectra of FA10, SF10 and specifically in the FTIR spectrum of NS10 after 28 days reminding lesser extent of ettringite formation in NS10 [44,46,47] . The strong band observed at 949 cm -1 and the band observed at 719 cm -1 were associated with the bending-in-plane vibrations of the Si-O bonds in tricalcium silicates (C 3 S) and dicalcium silicates (C 2 S) [1,40,42,47] . The intensity of these bending-in-plane vibrations of the Si-O Figure 5.…”
Section: Characterization Of the Mortar Specimensmentioning
confidence: 99%
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“…This band decreased in size as the curing time was extended in the spectra of FA10, SF10 and specifically in the FTIR spectrum of NS10 after 28 days reminding lesser extent of ettringite formation in NS10 [44,46,47] . The strong band observed at 949 cm -1 and the band observed at 719 cm -1 were associated with the bending-in-plane vibrations of the Si-O bonds in tricalcium silicates (C 3 S) and dicalcium silicates (C 2 S) [1,40,42,47] . The intensity of these bending-in-plane vibrations of the Si-O Figure 5.…”
Section: Characterization Of the Mortar Specimensmentioning
confidence: 99%
“…The broad bands appearing at 3648-3650 cm -1 in the spectra of all mortar specimens including OPC (control) corresponded to the overlapping stretching vibrations of the structural -OH groups (ν 3 ) of Ca(OH) 2 formed during the hydration of C 3 S and C 2 S, and the free -OH groups (ν 1 ) of water molecules present in the mixture 41,42 . This band diminished for all samples as the hydration process proceeded, implying a decrease in free water due to C-S-H bond formation 43 .…”
Section: Characterization Of the Mortar Specimensmentioning
confidence: 99%
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“…Recent studies have been also focused on characterisation of some XIX and XX century mortars. Methodologies have been defined in order to identify the nature of binders and to distinguish between natural hydraulic mortars, natural cements and Portland cements [4,5]. FTIR, XRD analysis and SEM observation have been employed to identify gehlenite and C 3 S, as characteristic hydraulic phase respectively of natural hydraulic lime and cements.…”
Section: Introductionmentioning
confidence: 99%
“…The broad band detected at 3711 cm -1 in the infrared spectroscopy of OPC linked to overlap stretching vibrations of both the structural and free hydroxy groups of CH and water respectively. FTIR spectra of RC, CA, FA20CA which have been defined as fingerprint evidence for the degree of polymerization with the formation of calcium-silicate-hydroxide phase due to hydration [24] having strong band observed at 900 cm -1 and the band observed at 520 cm -1 were associated with the bending-in-plane vibrations of the Si-O bonds in C3S (tricalcium silicates) and C2S (dicalcium silicates) [25][26][27][28]. The intensity of these bending-in-plane vibrations of the Si-O bonds decreased as calcium-silicate-hydroxide crystals formed [24,29].…”
Section: Microstructural Analysismentioning
confidence: 99%