Evaluation of Marble Alteration Processes

I. Zăuleț, R. Ion, C. Rizescu
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Abstract

Abstract The aim of the paper consists in the study of three Romanian types of marble (Ruschita, Albesti, Carrara) with different compositions in different temperature conditions, for different periods of time. The three samples were exposed to two different types of treatments: 25 cycles of freeze-thaw (according to SR EN 12371) and 3 cycles of exposure to high temperatures (400 °C for 1 hour). Following the freeze-thaw cycles, small differences in chromatic parameters could be observed (∆E = 2.2 for Carrara Italia marble and ∆E = 7.2 for Rușchița pink marble). The freezing coefficient for all samples is low (0.016% - 0.029%). Following exposure to high temperature treatment, the samples show large differences in chromatic parameters (∆E = 43.47 for Albesti marble) and significant changes in gloss. The surface of the samples showed cracks and microcracks. Based on the results of this study, the following conclusions can be drawn: Thermal cycles can cause the mechanical disintegration of the outer part of the marble, starting from the discontinuities contained in the rock and between the faces between the different minerals that form the stone. Exposure to high temperatures will result in a loss of adhesion between the surface grains on the sample surface. The degradation processes have been investigated.
大理石改造过程的评价
本文的目的在于研究三种罗马尼亚类型的大理石(Ruschita, Albesti, Carrara)在不同的温度条件下,在不同的时间内具有不同的成分。三个样品暴露于两种不同类型的处理:25次冻融循环(根据SR EN 12371)和3次高温暴露(400°C 1小时)。在冻融循环之后,可以观察到颜色参数的微小差异(意大利卡拉大理石∆E = 2.2, Rușchița粉色大理石∆E = 7.2)。所有样品的冻结系数都很低(0.016% ~ 0.029%)。经过高温处理后,样品的颜色参数差异很大(Albesti大理石的∆E = 43.47),光泽度也发生了显著变化。试样表面出现裂纹和微裂纹。根据本研究的结果,可以得出以下结论:热循环可以引起大理石外部的机械解体,从岩石中所含的不连续以及形成岩石的不同矿物之间的面之间开始。暴露在高温下会导致样品表面颗粒之间的附着力丧失。对其降解过程进行了研究。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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4 weeks
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