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Salt crystallization dynamics in indoor environments: Stone weathering in the Muñoz Chapel of the Cathedral of Santa María (Cuenca, central Spain)

Identifiers
URI: http://hdl.handle.net/20.500.12251/2649
View/Open: https://www.scopus.com/inward/record.uri?eid=2-s2.0-85092615278&doi=10.1016%2fj.culher.2020.09.011&partnerID=40&md5=b897a7700a130d74769e8c0006d5798a
ISSN: 12962074
DOI: 10.1016/j.culher.2020.09.011
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Author
Martínez Martínez, J.; Torrero Fuentes, Enrique; Sanz, D.; Navarro, V.
Date
2021
Subject/s

Sales - Materiales

Cristalización

Catedral de Santa María

Cuenca

Sillares

Patologías - Construcción

Patrimonio de la Humanidad

Degradación -materiales-

Mantenimiento preventivo

Obras de restauración

Unesco Subject/s

3305.26 Edificios Públicos

3313.04 Material de Construcción

3312.12 Ensayo de Materiales

3328.05 Cristalización

3308.04 Ingeniería de la Contaminación

Abstract

The cathedral of Santa María, where the Muñoz Chapel is located, is the most remarkable monument of the UNESCO Wold Heritage City of Cuenca (Spain). This emblematic chapel suffers an intense stone weathering by crystallization of a complex mixture of salts including epsomite, hexahydrite, gypsum, chlorides and phosphates. The salt dynamics is controlled by a variable indoor environment with daily and seasonal cyclicality. A methodology combining salt analysis, environmental monitoring and non-destructive stone inspection was adopted in order to understand the salt crystallization dynamics and finally, to design an adapted preventive conservation plan focused on the mitigation of the salt damages. Moreover, new parameters are designed in order to quantify the microenvironmental variability, establishing a new methodology for the analysis of indoor environments. Obtained results reveal that stone weathering is mainly due to: (1) the transformation of both CaSO4 and MgSO4·4H2O into CaSO4·2H2O and MgSO4·6H2O, respectively; and (2) the direct crystallization of MgSO4·6H2O in the porous system. These phases crystallize as efflorescences and as subflorescences, causing granular disintegration, peeling and scaling on the stone. Several preventive measures are finally proposed, being focused on two main objectives: (1) reducing the access of salts and moisture to the monument; and (2) establishing a nonaggressive environment, keeping temperature and relative humidity constants in the range of 15ˆ’20 °C and 40"“50%, respectively. This proposed climate range is defined in order to avoid both the crystallization of new salts in the porous system of the stone as well as volume changes of the present salts. This study constitutes a pilot project where to test the efficiency of these preventive measures that could be extensive to the whole cathedral complex. © 2020 Elsevier Masson SAS

The cathedral of Santa María, where the Muñoz Chapel is located, is the most remarkable monument of the UNESCO Wold Heritage City of Cuenca (Spain). This emblematic chapel suffers an intense stone weathering by crystallization of a complex mixture of salts including epsomite, hexahydrite, gypsum, chlorides and phosphates. The salt dynamics is controlled by a variable indoor environment with daily and seasonal cyclicality. A methodology combining salt analysis, environmental monitoring and non-destructive stone inspection was adopted in order to understand the salt crystallization dynamics and finally, to design an adapted preventive conservation plan focused on the mitigation of the salt damages. Moreover, new parameters are designed in order to quantify the microenvironmental variability, establishing a new methodology for the analysis of indoor environments. Obtained results reveal that stone weathering is mainly due to: (1) the transformation of both CaSO4 and MgSO4·4H2O into CaSO4·2H2O and MgSO4·6H2O, respectively; and (2) the direct crystallization of MgSO4·6H2O in the porous system. These phases crystallize as efflorescences and as subflorescences, causing granular disintegration, peeling and scaling on the stone. Several preventive measures are finally proposed, being focused on two main objectives: (1) reducing the access of salts and moisture to the monument; and (2) establishing a nonaggressive environment, keeping temperature and relative humidity constants in the range of 15ˆ’20 °C and 40"“50%, respectively. This proposed climate range is defined in order to avoid both the crystallization of new salts in the porous system of the stone as well as volume changes of the present salts. This study constitutes a pilot project where to test the efficiency of these preventive measures that could be extensive to the whole cathedral complex. © 2020 Elsevier Masson SAS

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