Abstract
Back-scattered Scanning Electron Microscopy (BSEM) has been used to identify weathering mechanisms occurring in two oolitic limestones from urban areas in London and Cambridge, United Kingdom. From a petrographical point of view, the two stones can be described as oosparite and oomicrite, their main distinctive feature being the crystal size of the cement binding the limestone grains together. The sulphation mechanism, i.e. the replacement of calcium carbonate (calcite: CaCO3) by calcium sulphate dehydrate (gypsum: CaSO4 2H2O), at the surface and within the stone fabric is confirmed as the general decay process. Differences in macroporosity/permeability distribution in the two limestones lead to different weathering patterns. BSEM provides evidence that gypsum patinas still commonly found on limestone facades in polluted urban locations are advancing inside the diseased stone and that their removal is urgently needed to arrest the growth of the in-growing weathering front.
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Schiavon, N. et al. (2012). Applying the Techniques on Materials II. In: Varella, E. (eds) Conservation Science for the Cultural Heritage. Lecture Notes in Chemistry, vol 79. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-30985-4_6
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