高压电脉冲与单向静应力联合作用下花岗岩破裂机制

Fracture mechanism of granite under the combined action of high voltage electric pulse and high stress

  • 摘要: 采用实验与数值模拟相结合的方法系统研究了单向静应力与高压电脉冲联合作用下花岗岩破裂机制。利用自主研发的实验平台开展了多组单向静应力下的高压电脉冲破裂花岗岩实验,获取岩石破裂形态、块度分布特征;通过罗氏线圈监测电脉冲破岩过程中的电流波形,并反演获得等离子通道冲击波时程曲线;利用LS-DYNA软件开展了数值模拟研究,分析了高压电脉冲与单向静应力联合作用下,花岗岩内部裂纹扩展及损伤演化过程。结果表明:静应力及边界约束条件对高压电脉冲破裂岩石具有显著影响。无静应力加载情况下,花岗岩试件四边均为自由面,裂纹呈现无序随机多向扩展状态。在单向静应力加载情况下,试件加载面成为无反射边界,另一对平面仍然为自由面并能够反射应力波。在自由面冲击波反射拉伸和静应力联合作用下,岩石试件内平行于静载方向的裂纹得到充分发展,形成优势扩展方向,而垂直于静载方向的裂纹受到抑制。随着静应力增加,其对平行载荷裂纹的导向与促进作用增强,逐渐成为主导,冲击波的自由边界反射拉伸效应被削弱,裂纹向试件中部汇聚;特别是在等离子通道附近出现明显压损伤区,消耗了大量冲击波能量,是冲击波自由面反射拉伸效应减弱的主要原因。研究成果为高压电脉冲破岩技术在深部单向主应力环境下的应用提供了基础理论依据。

     

    Abstract: The fracture mechanism of granite under the combined action of unidirectional static stress and high voltage electric pulse is systematically studied by means of experiment and numerical simulation. The self-developed experimental platform was used to carry out multiple sets of high-voltage electrical pulse fracture granite experiments under unidirectional static stress, and the rock fracture morphology and block distribution characteristics were obtained. The current waveform in the process of electric pulse breaking rock is monitored by Rogowski coil and the time history curve of plasma channel shock wave is obtained by inversion. The numerical simulation was carried out by using LS-DYNA software, and the crack propagation and damage evolution process in granite under the combined action of high voltage electric pulse and unidirectional static stress were analyzed. The results show that the static stress and boundary constraint conditions have a significant effect on the fracture of rock by high voltage electric pulse. In the absence of static stress loading, the four sides of the granite specimen are free surfaces, and the cracks show a disordered random multi-directional expansion state. In the case of unidirectional static stress loading, the loading surface of the specimen becomes a non-reflective boundary, and the other pair of planes is still a free surface, which can reflect the stress wave. Under the combined action of shock wave reflection tension and static stress on the free surface, the cracks parallel to the static load in the rock specimen are fully developed, forming a dominant propagation direction, while the cracks perpendicular to the static load direction are suppressed. With the increase of static stress, the guiding and promoting effect of static stress on parallel load cracks is enhanced, and gradually becomes dominant. The free boundary reflection tensile effect of shock wave is weakened, and the cracks converge to the middle of the specimen. In particular, there is an obvious compressive damage zone near the plasma channel, which increases with the increase of static load and consumes a large amount of shock wave energy, which is the main reason for the weakening of the free surface reflection tensile effect of the shock wave. The research results provide basic theoretical basis and technical support for the application of high-voltage electric pulse rock breaking technology in deep unidirectional principal stress engineering.

     

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