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Numerical simulation of rock-breaking under the impact load of self-excited oscillating pulsed waterjet

机译:自激振荡脉冲水射流冲击载荷作用下的岩石破碎数值模拟

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摘要

To investigate the rock-breaking performance of the self-excited oscillating pulsed waterjet (SOPW), the finite element method (FEM) combined with smoothed particle hydrodynamics (SPH) was utilized to simulate the rock-breaking process. First, the rock-breaking status of a continuous waterjet and SOPW impact were compared and the rock-breaking mechanism including the formation and propagation of cracks and the formation of the crushing zone were observed. Under the same conditions, the rock-breaking performance of SOPW was found to be superior to that of the continuous waterjet. In addition, the failure of the crack propagation and crushing zone formation results in brittle failure and plastic behavior, respectively. The hammer pressure generated at the initial stage is the major factor for rock-breaking using a continuous waterjet. In the case of the SOPW, the hammer pressure can be generated at a high frequency, which indicates that SOPW can more effectively exploit energy and hammer pressure than a continuous waterjet. In addition, the rock-breaking performance with different pulse amplitudes, pulse frequencies, and confining pressures was discussed. The results indicate that the greater the pulse amplitude, the more severe the rock damage. However, a regular trend was not observed for rock-breaking performance with increase in pulse frequency. In addition, with increase in confining pressure, the rock-breaking performance initially decreased and then increased and the main conical cracks gradually became vertical to the side surface.
机译:为了研究自激振荡脉冲水射流(SOPW)的破岩性能,利用有限元方法(FEM)结合平滑粒子流体动力学(SPH)来模拟破岩过程。首先,比较了连续喷水的破岩状态和SOPW冲击,并观察了包括裂缝的形成和扩展以及破碎区形成的破岩机理。在相同条件下,发现SOPW的破岩性能要优于连续喷水器。另外,裂纹扩展和破碎区形成的失败分别导致脆性破坏和塑性行为。初始阶段产生的锤击压力是使用连续水刀破碎岩石的主要因素。在SOPW的情况下,可以以较高的频率产生锤击压力,这表明SOPW可以比连续喷水更有效地利用能量和锤击压力。此外,还讨论了具有不同脉冲幅度,脉冲频率和围压的破岩性能。结果表明,脉冲幅度越大,岩石破坏越严重。然而,随着脉冲频率的增加,未观察到破碎性能的规律趋势。另外,随着围压的增加,破岩性能开始下降,然后上升,主要的圆锥形裂缝逐渐垂直于侧面。

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