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Influence of thermal damage on physical properties of a granite rock: Porosity, permeability and ultrasonic wave evolutions

机译:热损伤对花岗岩岩石物理性质的影响:孔隙率,渗透率和超声波演化

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In this paper, parameters for characterization of connected porosity and overall damage in the thermally-cracked rock of granite in order to assess, respectively, its transport properties and its mechanical strength are identified and quantified. Samples were heated to a range of peak temperatures up to 600 ℃ at ambient pressure. Characterizations were made by measurement of porosity, gas permeability, velocity and attenuation of ultrasonic waves. Our study confirms the strong influence of thermal damage on physical properties, and shows clearly the potential of the above techniques in connection with this type of damage. Typically, we show that the porosity measurement only informs about open porosity, which is distributed and available at rock surface, whereas the gas permeability measurement characterizes the connected porosity. As for the ultrasonic wave propagation, it is sensitive to overall damage in the material. Nevertheless, we observed that the three techniques are complementary and similarly describe the rock behavior in each stage of heat treatment; they show a good consistency between them.
机译:本文确定和量化了花岗岩热裂岩中连通孔隙度和整体损伤特征的参数,以便分别评估其输运性能和机械强度。在环境压力下将样品加热至最高峰值温度600℃。通过测量孔隙率,气体渗透率,超声波的速度和衰减进行表征。我们的研究证实了热损伤对物理性能的强烈影响,并清楚显示了上述技术与此类损伤相关的潜力。通常情况下,我们表明孔隙度测量仅能说明开放的孔隙度,该孔隙度分布在岩石表面并在岩石表面可用,而透气度测量则表征了连通的孔隙度。至于超声波的传播,它对材料的整体损坏很敏感。尽管如此,我们观察到这三种技术是互补的,并且相似地描述了热处理每个阶段的岩石行为。它们之间显示出良好的一致性。

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