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首页> 外文期刊>Journal of structural geology >Effect of water on the strength and microstructure of Carrara marble axially compressed at high temperature
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Effect of water on the strength and microstructure of Carrara marble axially compressed at high temperature

机译:水分对高温轴向压缩的卡拉拉大理石强度和微观结构的影响

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摘要

In this study, we aimed to (ⅰ) answer the question if water affects the strength of marble deforming at high temperature and (ⅱ) establish criteria that allow assessment of the role of water in microstructure development in marble. Samples of Carrara marble were axially compressed at temperatures ranging 600-1000℃ and strain rate ~ 10~(-5) s~(-1), with or without addition of 0.4-2.1 wt% water. Water-added samples were found to be slightly weaker than dry samples. Microstructurally, all samples showed grain flattening and twinning at 600℃ and dynamic recrystallization dominated by grain boundary migration at higher temperature. Grain boundaries in wet samples showed isolated or semi-continuous remnants of fluid pockets. The average grain roundness R and fractal dimension D relating grain diameter d and grain perimeter P (P ∝ d~D) for wet recrystallized samples were systematically lower than for dry samples. At 600℃, high pore fluid pressure probably enhanced dilatation of wet samples and helped grain boundary sliding (GBS), thereby lowering the strength. At higher temperature, fluid-enhanced grain boundary migration served as a recovery process, reducing the contribution of GBS to creep. Overall, water has little effect on strength and microstructure of marble experimentally deformed at high temperature.
机译:在这项研究中,我们旨在(ⅰ)回答水是否会影响高温下大理石变形的强度的问题,以及(ⅱ)建立标准以评估水在大理石微结构发展中的作用。将卡拉拉大理石样品在600-1000℃的温度和应变速率〜10〜(-5)s〜(-1)的范围内进行轴向压缩,添加或不添加0.4-2.1 wt%的水。发现加水样品比干样品稍弱。显微组织表明,所有样品在600℃下均表现出晶粒扁平化和孪生,并且在较高温度下动态再结晶以晶界迁移为主。湿样品中的晶界显示出孤立或半连续的积液。湿重结晶样品的平均晶粒圆度R和与晶粒直径d和晶粒周长P有关的分形维数D(P∝d〜D)有系统地低于干燥样品。在600℃时,高孔隙流体压力可能会增强湿样品的膨胀并帮助晶界滑动(GBS),从而降低强度。在较高温度下,流体增强的晶界迁移充当了恢复过程,从而减少了GBS对蠕变的贡献。总体而言,水对高温下实验变形的大理石的强度和微观结构影响很小。

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