2003
DOI: 10.1016/s0008-8846(03)00227-8
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Micro-Raman spectroscopy applied to depth profiles of carbonates formed in lime mortar

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Cited by 140 publications
(92 citation statements)
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“…In contrast, under the fingerprint characterisation capacity of Raman spectroscopy [10,11], the reaction products of various deterioration mechanisms, such as calcium carbonate polymorphs (e.g., calcite, vaterite and aragonite) [12][13][14][15][16][17][18][19] from carbonation and sulphatebearing products (i.e., gypsum, ettringite and thaumasite) [20][21][22][23] from sulphate attack , can be clearly differentiated by their unique vibration bands (wavenumber in cm -1 ) and this can effectively overcome the limitations of ES. Moreover, as Raman spectroscopy works on the principle of intrinsic vibration of molecules, the chemical dyes as employed in the FOS is no longer needed which can totally eliminate the long-term instability and irreversibility issues facing FOS.…”
Section: Introductionmentioning
confidence: 99%
“…In contrast, under the fingerprint characterisation capacity of Raman spectroscopy [10,11], the reaction products of various deterioration mechanisms, such as calcium carbonate polymorphs (e.g., calcite, vaterite and aragonite) [12][13][14][15][16][17][18][19] from carbonation and sulphatebearing products (i.e., gypsum, ettringite and thaumasite) [20][21][22][23] from sulphate attack , can be clearly differentiated by their unique vibration bands (wavenumber in cm -1 ) and this can effectively overcome the limitations of ES. Moreover, as Raman spectroscopy works on the principle of intrinsic vibration of molecules, the chemical dyes as employed in the FOS is no longer needed which can totally eliminate the long-term instability and irreversibility issues facing FOS.…”
Section: Introductionmentioning
confidence: 99%
“…Bensted was the pioneer in using Raman spectroscopy (1976a) to characterize cement minerals, following by Conjeaud and Boyer (1980). Most of the papers devoted to the application of Raman spectroscopy in cement chemistry concerns the characterization of clinker anhydrous minerals (Bensted, 1976a-Conjeaud and Boyer, 1980-Newman et al, 2005, identification of the various calcium sulfate forms: gypsum CaSO 4 ·2H 2 O, bassanite CaSO 4 ·½H 2 O and anhydrite CaSO 4 (Bensted, 1976b-Prasad, 2001), study of cement hydration by recording the decrease in intensity of the signals from the anhydrous silicate phases (Tarrida et al, 1995) and the effects of carbonation (Bensted, 1977-Martinez-Ramirez, 2003. However some studies report the use of Raman spectroscopy to investigate cementitious hydrates: namely to distinguish thaumasite Ca 6 Si 2 (OH) 12 ·(CO 3 ) 2 ·(SO 4 ) 2 ·24H 2 O from ettringite Ca 6 Al 2 (OH) 12 ·(SO 4 ) 3 ·26H 2 O, (Brough and Atkinson, 2001-Jallad et al, 2001-Sahu et al, 2002 and to characterize the C-S-H, calcium silicate hydrate, phase (Kirkpatrick et al, 1997).…”
Section: Introductionmentioning
confidence: 99%
“…Martinez-Ramirez et al 18 the calcite, aragonite and vaterite mix generates a wide band that would combine the three chief vibration bands corresponding to carbonate groups in different environments, at 1076, 1085 and 1090 cm 1 .…”
Section: Resultsmentioning
confidence: 99%