2009
DOI: 10.1155/2009/893528
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The Use of FTIR and Micro-FTIR Spectroscopy: An Example of Application to Cultural Heritage

Abstract: Recommended by Maher S. AmerMicro-FTIR and FTIR spectroscopy is useful for the study of degradation forms of cultural heritage. In particular it permits to identify the degradation phases and to establish the structural relationship between them and the substratum. In this paper, we report the results obtained on marble from a Roman sarcophagus, located in the medieval cloister of St. Cosimato Convent (Rome), and on oolitic limestone from the facade of St. Giuseppe Church in Syracuse (Sicily). The main compone… Show more

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Cited by 53 publications
(38 citation statements)
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“…4d) performed on CS-BG sample. In detail, an oxalate layer, originated from the degradation of a protective coating, is typically located at the crust-stone interface (La Russa et al, 2009), but in this case calcium oxalate is heterogeneously located within the whole crust.…”
Section: Discussionmentioning
confidence: 99%
“…4d) performed on CS-BG sample. In detail, an oxalate layer, originated from the degradation of a protective coating, is typically located at the crust-stone interface (La Russa et al, 2009), but in this case calcium oxalate is heterogeneously located within the whole crust.…”
Section: Discussionmentioning
confidence: 99%
“…The technique permits the identification of characteristic vibrations associated with functional groups in a given molecule [2]. Raman spectroscopy, being non-destructive, fast, sensitive, reproducible and less expensive than other techniques is being increasingly used for artwork analyses [3], in particular for pigment identification.…”
Section: Introductionmentioning
confidence: 99%
“…The thin film over the silvered surface was also characterized by DRIFT, which is well-known to generate high-quality IR spectra in reflectionabsorption configuration ( Figure 5A, spectrum c). Besides the presence of overlapping signals originating from the underlying gypsum layer (1680 and 1632 cm −1 ), a mixture of proteinaceous material (signals at 1650, 1576, and 1550 cm −1 ) and calcium oxalates (1636, 1320, and 780 cm −1 ) was identified [21][22][23]. The band presence at 1320-1325 cm −1 is typical of whewellite (Ca(C2O4) H2O) [24].…”
Section: Resultsmentioning
confidence: 96%