Different ancient mortar samples were analyzed to characterize their binder fraction. Thermal analyses (TG, DSC) proved to be very useful in the identification of three different species of lime composed of: (a) only calcite; (b) calcite and magnesite; (c) calcite, hydromagnesite and magnesite. The hydromagnesite is well identified in the DSC curve showing the peaks corresponding to the three-step thermal decomposition. Also the same mineral was detected by FTIR and/or micro-FTIR analyses, depending on its amount in the binder fraction of the mortar. Actually, the two absorption peaks characteristic of the hydromagnesite were often hidden by the wider peaks due to the asymmetric stretching of the carbonate ion, observed for the calcite and magnesite.

Characterization of Ancient Magnesian Mortars coming from Northern Italy / S. Bruni, F. Cariati, P. Fermo, A. Pozzi, L. Toniolo. - In: THERMOCHIMICA ACTA. - ISSN 0040-6031. - 321:1-2(1998), pp. 161-165.

Characterization of Ancient Magnesian Mortars coming from Northern Italy

S. Bruni
Primo
;
F. Cariati
Secondo
;
P. Fermo;
1998

Abstract

Different ancient mortar samples were analyzed to characterize their binder fraction. Thermal analyses (TG, DSC) proved to be very useful in the identification of three different species of lime composed of: (a) only calcite; (b) calcite and magnesite; (c) calcite, hydromagnesite and magnesite. The hydromagnesite is well identified in the DSC curve showing the peaks corresponding to the three-step thermal decomposition. Also the same mineral was detected by FTIR and/or micro-FTIR analyses, depending on its amount in the binder fraction of the mortar. Actually, the two absorption peaks characteristic of the hydromagnesite were often hidden by the wider peaks due to the asymmetric stretching of the carbonate ion, observed for the calcite and magnesite.
Ancient mortars; Hydromagnesite; IR spectroscopy; Thermal analyses
Settore CHIM/01 - Chimica Analitica
Settore CHIM/12 - Chimica dell'Ambiente e dei Beni Culturali
1998
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/2434/188258
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