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Modeling and simulation of melt flow during discharge crater formation in EDM

机译:EDM放电火山口熔体流动的建模与仿真

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To improve the accuracy of the discharge crater formation simulation in EDM,in this study a thermo-hydraulic coupling model based on finite element method was built,which comprehensively considered temperature-dependent material properties,buoyancy force,vaporization recoil pressure and Marangoni effect,to investigate the melt flow during the discharge crater formation.According to the simulation results,main conclusions can be drawn as follows.1.On the initial stage of discharge when arc plasma is expanding,vaporization recoil force acts on the melt pool surface is the main factor that drives the molten electrode material flow to the periphery of discharge crater.2.When the vaporization recoil force decreases to a small value due to the expansion of arc plasma,the thermo-capillary force caused by Marangoni effect becomes the main factor that drives the radial flow of the molten electrode material and that promote the formation of bulge.3.After the end of discharge,the crater radius will continue to increase and crater depth will experience fluctuations under the influence of surface tension,and bulge height continue to increase a little under the effect of thermo-capillary force.
机译:为了提高EDM中放电火山口形成模拟的准确性,在这研究中,建立了基于有限元方法的热液压耦合模型,其全面考虑了温度依赖性材料特性,浮力,汽化反冲压力和Marangoni效应调查在放电陨石坑期间的熔体流动。根据仿真结果,可以如下绘制主要结论.1。近弧等离子体膨胀时的初始阶段,蒸发反冲力作用在熔体池表面上是主要的驱动熔融电极材料的因素流到放电钻石船的周边。由于弧形等离子体膨胀导致蒸发反冲力降至较小的值时,由Marangoni效应引起的热毛细管力成为驱动的主要因素熔融电极材料的径向流动和促进凸起的形成。在放电结束时,火山口半径Wi LL继续增加,陨石坑深度将在表面张力的影响下体验波动,并且凸起高度在热毛细力的影响下继续增加一点。

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