2003
DOI: 10.1081/sl-120026615
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Evaluation of Gypsum and Calcium Oxalates in Deteriorated Mural Paintings by Quantitative FTIR Spectroscopy

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Cited by 35 publications
(22 citation statements)
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“…Oxalate compounds are the main components of human kidney stones [5][6][7] and they are also produced during the degradation of ancient paintings, sculpture, and architectural works [31][32][33][34][35][36] due to both natural and anthropological phenomena, such as climatic conditions and exposure to pollutant agents. Several ancient monuments were found to be covered by a superficial film comprising several compounds such as calcium oxalate, which has protective effects against unfavorable environmental conditions.…”
Section: Introductionmentioning
confidence: 99%
“…Oxalate compounds are the main components of human kidney stones [5][6][7] and they are also produced during the degradation of ancient paintings, sculpture, and architectural works [31][32][33][34][35][36] due to both natural and anthropological phenomena, such as climatic conditions and exposure to pollutant agents. Several ancient monuments were found to be covered by a superficial film comprising several compounds such as calcium oxalate, which has protective effects against unfavorable environmental conditions.…”
Section: Introductionmentioning
confidence: 99%
“…Regarding the decaying compounds, because the formation of calcium oxalates (whewellite and weddellite) result from the bio-deterioration and/or deterioration of binders in ancient paintings [13,25,26], we tried to weigh up their presence by measuring the FT-IR peak area/μg of sample at 780 cm −1 ( Table 2). Interestingly, the ratio between organic material percentage and the corresponding oxalate area/μg resulted higher in sample S1 and S5 (1.69 and 1.28, respectively) compared to samples S2, S3, and S4 (0.56, 0.45, and 0.54, respectively), thus suggesting that samples S1 and S5 were probably less bio-deteriorated/deteriorated compared to samples S2, S3, and S4.…”
Section: Discussionmentioning
confidence: 99%
“…7 provides evidence of low concentrations of the minerals, gypsum (CaSO 4 •2H 2 O) and goethite (FeOOH) in the Hinder modelling clay. Bands at 603 and 675 cm −1 and at 3553 and 3406 cm −1 superimposed upon the broad O-H stretching band are characteristic of gypsum [19,20]. A small band at 766 cm −1 and a contribution to the broad O-H stretching region indicates goethite is present [21,22].…”
Section: Hinder Artworkmentioning
confidence: 96%