火灾引起的当地建筑材料微结构变化:白色大理石和石灰石案例

Laila Akram
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摘要

摘要这项工作的目的是评估天然石材在遭受火灾后的退化状态。这些在建筑遗产中广泛使用的建筑和装饰材料在暴露于高温时会遭受不可逆转的破坏。因此,了解它们的残余耐久性对于确定火灾后的建筑结构是应该修复、加固还是拆除至关重要。为此,我们在马弗炉中对从当地采石场采集的石灰岩(钙钛矿)和白色大理石进行了加热-冷却循环,温度最高可达 1100°C。每次暴露后,在室温下使用 X 射线衍射 (XRD)、微拉曼和 ATR-FTIR 红外技术对所选样品进行表征。研究结果表明,钙质和大理石天然石材的矿物学性质是影响其在高温下热稳定性的关键因素。在 570°C 以上的不同温度范围内,天然石材都会发生方解石脱碳现象。大理石在矿物学上是单相的,在 800°C 时发生分解,与纯态方解石相似。方解石的分解温度要低得多,约为 700°C。这项研究认为大理石的热稳定性高于方解石。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Fire Induced Microstructural Changes in Local Building Materials: Cases of White Marble and Limestone
Abstract. The aim of this work is to evaluate the degradation state of natural stones after their exposure to fire. These building and decorative materials, widely used in the architectural heritage, suffer irreversible damage when exposed to high temperatures. Therefore, knowledge of their residual durability is crucial in order to determine whether the post-fire building structure should be restored, reinforced or demolished. For this purpose, limestones (calcarenites) and white marbles collected from local quarries were subjected to heating-cooling cycles in a muffle furnace at various temperatures up to 1100°C. After each exposure, the selected samples were characterized at room temperature using X-ray diffraction (XRD), micro-Raman and ATR-FTIR infrared techniques. The results obtained showed that the mineralogical nature of both calcareous and marble natural stones is a key factor in their thermal stability when exposed to high temperatures. Above 570°C, natural stones undergo calcite decarbonation at different temperature ranges. Marble, which is mineralogically monophasic, underwent decomposition at 800°C, similar to calcite in its pure state. Calcarenite was decomposed at a much lower temperature of about 700 °C. This study classifies marble as more thermally stable than calcarenite.
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