1996
DOI: 10.1366/0003702963905312
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Comparison of IR Techniques for the Characterization of Construction Cement Minerals and Hydrated Products

Abstract: /npsi/ctrl?lang=en http://nparc.cisti-icist.nrc-cnrc.gc.ca/npsi/ctrl?lang=fr Access and use of this website and the material on it are subject to the Terms and Conditions set forth at http://nparc.cisti-icist.nrc-cnrc.gc.ca/npsi/jsp/nparc_cp.jsp?lang=en NRC Publications Archive Archives des publications du CNRCThis publication could be one of several versions: author's original, accepted manuscript or the publisher's version. / La version de cette publication peut être l'une des suivantes : la version prépubli… Show more

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Cited by 79 publications
(27 citation statements)
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“…The spectrum shows a strong broad band in the 1200-800 cm -1 region. Maxima absorptions were checked at around 883, 908 and 940 cm -1 , typical for anhydrous tricalcium silicate [18,27]. Also strong absorption bands at ~ 850, 1000 and 1112 cm -1 (which is also due to the sulphates presence) are attributed to anhydrous dicalcium silicate [18].…”
Section: Influence Of Curing Timementioning
confidence: 91%
“…The spectrum shows a strong broad band in the 1200-800 cm -1 region. Maxima absorptions were checked at around 883, 908 and 940 cm -1 , typical for anhydrous tricalcium silicate [18,27]. Also strong absorption bands at ~ 850, 1000 and 1112 cm -1 (which is also due to the sulphates presence) are attributed to anhydrous dicalcium silicate [18].…”
Section: Influence Of Curing Timementioning
confidence: 91%
“…Their intensities increase and their widths decrease with NS%, due to the pozzolanic action of NS, which accelerates the formation of more hydrated silicates. Also, the appeared band at 950-980 cm -1 is due to the formation of CSH [50]. The band at 1480 cm -1 is due to C-O bond stretching of CO 3 , which result from the carbonation of hydrated silicates as well as the residual Ca(OH) 2 .…”
Section: Ir Spectroscopymentioning
confidence: 97%
“…Therefore, the rate of lime consumption becomes more than that of its production. The appeared band in the range 950-985cm -1 is assigned to the formation of Tobermorite like phase (CSH) [50]. The broad band centered at about 3400 cm -1 and that at 1640-1650 cm -1 are due to stretching and bending vibration of water bound in the hydrated silicates.…”
Section: Ir Spectroscopymentioning
confidence: 98%
“…It also absorbs this radiation in the range 3,000-3,700 cm -1 as this corresponds to the O-H stretching region. The hydroxide containing compounds also absorb in this range, such as Ca(OH) 2 at 3,643 cm -1 (Björnström 2005;Delgado et al 1996;Yu et al 1999).…”
Section: Introductionmentioning
confidence: 99%