3.9 Article

Deterioration Effects on Bricks Masonry in the Venice Lagoon Cultural Heritage: Study of the Main Facade of the Santa Maria dei Servi Church (14th Century)

期刊

HERITAGE
卷 6, 期 2, 页码 1277-1292

出版社

MDPI
DOI: 10.3390/heritage6020070

关键词

bricks; cultural heritage; decay; weathering process; damage; historical building; construction materials; firing process; salt crystallization; Venice lagoon

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Tidal exchange, capillary rise, water condensation-evaporation cycles, and salt crystallization are the main causes of damage in historic brick buildings in Venice. This study analyzed twenty-three brick samples from the Santa Maria dei Servi Church to understand the composition and deterioration processes. The presence of carbonates and newly formed silicate phases indicated firing temperatures and production inconsistencies. Sulfates were identified as the main weathering products, with secondary phases occurring in bricks with higher vitrification levels.
Tidal exchange, capillary rise, water condensation-evaporation cycles, and crystallization of salts are the main causes of damage in historic brick buildings in Venice. The present study addressed these issues by proposing a study of twenty-three brick samples collected on the main facade of the Santa Maria dei Servi Church (14th century). The color, mineralogical composition, and texture of these samples were studied using standard methods such as spectrophotometry, X-ray powder diffraction (XRPD), optical microscopy (OM), and field emission scanning electron microscopy (FESEM). The presence of carbonates (calcite and dolomite) and newly formed silicate phases, such as gehlenite and diopside, provided indications of the temperatures reached during firing and suggested the absence of a good standardization in the production process. Meanwhile, XRPD and hyperspectral analysis (HA) detected sulfates (e.g., gypsum and mirabilite) as the main weathering products due to the salt decay process that affects monuments in the Venice lagoon environment. Moreover, secondary phases, such as Mg- and Ca-zeolites, occurred in bricks where the groundmass observed by OM was more vitrificated, and the XRPD patterns displayed the highest amorphous content. On-site mapping of sulfates and chlorophyll by HA was also performed on the main facade of the Church, highlighting the large presence of salts and biodeterioration.

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