Different ancient mortar samples were analyzed to characterize their binder
fraction, Thermal analyses (TG. DSC) proved to be very useful in the ident
ification 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 corres
ponding 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 character
istic of the hydromagnesite were often hidden by the wider peaks due to the
asymmetric stretching of the carbonate ion, observed for the calcite and m
agnesite. (C) 1998 Elsevier Science B.V.