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Investigating morphological changes in treated vs. untreated stone building materials by x-ray micro-CT
Simone Bugani1, Mara Camaiti, Luciano Morselli
1Department of Industrial Chemistry and Materials, University of Bologna, Viale Risorgimento 4, 40136, Bologna, Italy.
Analytical and Bioanalytical Chemistry
|March 15, 2008
Summary
Conservation treatments for Lecce stone (biocalcarenite) were evaluated using micro-CT. Paraloid B72 (PB 72) showed homogenous distribution with minimal impact, while a fluoroelastomer (NH) reduced porosity but altered stone structure.
Area of Science:
- Geosciences
- Materials Science
- Conservation Science
Background:
- Calcareous stones, particularly calcarenites, are vital in historical architecture but susceptible to weathering due to high calcite content and porosity.
- Protective polymer treatments are essential for mitigating deterioration in historic stone structures.
Purpose of the Study:
- To investigate the morphological changes in biocalcarenite (Lecce stone) after conservation treatments using micro-X-ray computed tomography (micro-CT).
- To quantitatively assess the impact of Paraloid B72 (PB 72) and a fluoroelastomer (NH) on stone porosity and internal structure.
Main Methods:
- Micro-X-ray computed tomography (micro-CT) was employed to analyze the internal structure of Lecce stone samples.
- Porosity and morphological parameters were calculated before and after treatment.
- Student's t-test was used for statistical comparison of results.
Main Results:
- Paraloid B72 (PB 72) demonstrated homogenous distribution and caused minimal alterations to the stone's natural properties.
- The fluoroelastomer (NH) treatment resulted in a significant decrease in porosity.
- NH treatment led to variations in wall thickness distribution, likely due to inhomogeneous application.
Conclusions:
- Paraloid B72 (PB 72) is a suitable conservation agent for Lecce stone, preserving its natural characteristics.
- The fluoroelastomer (NH) effectively reduces porosity but may induce undesirable structural changes in the stone.

