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An experimental study of the mechanical properties of granite after high temperature exposure based on mineral characteristics

机译:基于矿物特征的高温暴露后花岗岩力学性能的实验研究

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The macroscopic mechanical properties of granite collected from the Fujian Province, China were measured using uniaxial compression and three-point bending after the granite was exposed to high temperatures. The stress strain relationship was measured and mechanical properties including the Young's modulus, uniaxial compressive strength (UCS) and fracture toughness were calculated. In general, the uniaxial compressive strength (UCS), Young's modulus and fracture toughness of the granite specimens decrease with an increase in heat treatment temperature up to 800 degrees C, above which there is no obvious change. The microstructure of the failed specimens was explored using scanning electron microscopy (SEM) and stereomicroscopy. After heat treatment, the minerals within the granite were analysed using X-ray diffraction. The failure mechanisms and the mechanical characteristics of the granite are explained in terms of the microstructure and the minerals present. The results of the experiments indicate that the crystal structure of the phlogopite in granite transforms to a more stable structure between 400 degrees C and 600 degrees C with an associated increase in volume. A dehydroxylation reaction also occurs in the phlogopite at 400 degrees C, after which the uniaxial compressive strength (UCS) decreases and the ductility increases. Using SEM and stereomicroscopy, it was observed that the connection between the minerals within the granite becomes weaker with increasing heat treatment temperature. Intercrystalline cracking is the main failure mode for samples exposed to temperatures below 800 degrees C, whereas transcrystalline cracking can be observed in samples exposed to 1000 degrees C. (C) 2017 Elsevier B.V. All rights reserved.
机译:从福建省收集的花岗岩的宏观力学性能,通过单轴压缩测量,在花岗岩暴露于高温后三点弯曲测量。计算应力应变关系,并计算包括杨氏模量,单轴抗压强度(UCS)和断裂韧性的机械性能。通常,单轴抗压强度(UCS),花岗岩样品的缺口模量和断裂韧性随着热处理温度的增加而降低,高达800℃,上述没有明显的变化。使用扫描电子显微镜(SEM)和立体镜检查探索失败标本的微观结构。热处理后,使用X射线衍射分析花岗岩内的矿物质。根据存在的微观结构和矿物质来解释花岗岩的失效机制和机械特性。实验结果表明花岗岩中磷酸盐岩的晶体结构转化为400℃和600℃之间的更稳定的结构,其体积相关的增加。在400℃的絮络石中也发生脱羟基化反应,之后单轴抗压强度(UCS)降低并且延展性增加。使用SEM和立体镜检查,观察到花岗岩内矿物质之间的连接变弱,随着热处理温度的增加变弱。细胞裂解是暴露于800℃以下的温度的样品的主要故障模式,而可以在暴露于1000摄氏度的样品中观察到经晶裂解。(c)2017 Elsevier B.v.保留所有权利。

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