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Experimental study on rock indentation using infrared thermography and acoustic emission techniques

机译:红外热成像和声发射技术岩体压痕的实验研究

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摘要

For better understanding of rock fragmentation mechanism and correlative influence factors under the cutter penetration, a set of two-dimensional wedge indentation tests was conducted. Nondestructive detection techniques, including infrared thermography and acoustic emission, were employed to capture rock damage evolution information. Combined with experimental observations, the cavity expansion model (CEM) theory was adopted to interpret the temperature rise differences for different rock damage zones, and the sizes of these zones were quantitatively determined based on the thermal distribution. It was thought that different thermomechanical coupling mechanisms in different damage zones cause their differences in temperature rise degrees. The quantitative estimation for damage zone sizes indicates the plastic zone and core zone initiate and develop sequentially rather than simultaneously. The main influence factors on rock indentation and damage evolution characteristics were also considered, including rock type, wedge indenter geometry and confining stress. Furthermore, some shortcomings of the classical CEM were discussed through the comparison of indentation pressure and damage zone size between the experimental value and theoretical estimation.
机译:为了更好地理解在刀具渗透下的岩石碎片机制和相关影响因素,进行了一组二维楔形压痕试验。非破坏性检测技术,包括红外热成像和声学发射,用于捕获岩石损伤演化信息。结合实验观察,采用腔膨胀模型(CEM)理论来解释不同岩石损伤区的升温差异,并且基于热分布定量地确定这些区域的尺寸。据认为,不同损伤区中的不同热机械耦合机制导致它们在温度上升度的差异。损伤区域尺寸的定量估计表示塑料区和核心区顺序引发和发展而不是同时发育。还考虑了岩石压痕和损伤演化特性的主要影响因素,包括岩型,楔形压痕几何形状和限制应力。此外,通过比较实验值与理论估计之间的压痕压力和损伤区大小来讨论经典CEM的一些缺点。

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