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Study of the effects of salt crystallization on degradation of limestone rocks

机译:盐结晶对石灰岩降解的影响研究

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Salt crystallization is widely recognized as a cause of deterioration of porous building materials. In particular, the crystallization pressure of salt crystals growing in confined pores is found to be the main cause for damage. The aim of this study is to better understand the degradation of porous rocks induced by salt crystallization and correlate such processes with the intrinsic characteristics of materials. With this intent, an experimental salt weathering simulation was carried out on two limestones widely used in the Baroque architecture of eastern Sicily. A systematic approach, including petrographic, porosimetric and colorimetric analyses, was used to evaluate the correlation among salt crystallization, microstructural and chromatic variations of limestones. Results showed a quite different resistance of the two limestones to salt damage, and this was found to be strongly dependent on their pore structure and textural characteristics.
机译:盐的结晶被广泛认为是导致多孔建筑材料劣化的原因。特别地,发现在狭窄的孔中生长的盐晶体的结晶压力是损坏的主要原因。这项研究的目的是更好地理解盐结晶引起的多孔岩石的降解,并将这些过程与材料的固有特性联系起来。为此,在两个西西里岛东部的巴洛克式建筑中广泛使用的两个石灰石上进行了盐分风化实验。一种系统的方法,包括岩相,孔隙度和比色分析,被用来评估盐结晶,石灰岩微结构和颜色变化之间的相关性。结果显示两种石灰石对盐害的抵抗力完全不同,这被发现很大程度上取决于它们的孔结构和质地特征。

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