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2D semiempirical model of the formation of an elementary crater on the cathode of a vacuum arc

机译:2D真空电弧阴极上基本陨石坑形成的半透明模型

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A semiempirical hydrodynamic model based on the cellular structure of the cathode spot of a vacuum arc has been developed to describe the formation of a microcrater on the cathode and the initial stage of the formation of liquid-metal jets. The model includes experimentally obtained characteristics of the cathode spot plasma interacting with the cathode, such as the pressure exerted by the plasma on the cathode and the energy balance in the arc. In the context of a 2D axisymmetric statement of the problem of electric heat and mass transport in a cathode, the formation of a crater on a copper cathode has been simulated for a constant current carried by a elementary cathode spot cell. It has been shown that for the cell current ranging between 1.6 and 7 A and the time of current flow through the cell ranging between 15 and 60 ns, the crater diameter is 3÷7 μm. The crater depth is determined mainly by the current density in the cell. For all calculation variants where a micrometer-size crater was formed in several tens of nanoseconds, the maximum current density in a cell was (1÷3)·108 A/cm2.
机译:已经开发了基于真空弧的阴极斑点的细胞结构的半透镜流体动力学模型,以描述阴极对阴极的形成和液态金属喷射形成的初始阶段。该模型包括通过实验获得的与阴极相互作用的阴极点等离子体的特征,例如通过等离子体在阴极上施加的压力和电弧中的能量平衡。在阴极中电热和质量传输问题的2D轴对称陈述的上下文中,已经模拟了铜阴极上的陨石坑的形成,用于由基本阴极点细胞携带的恒定电流。已经表明,对于电池电流在1.6和7a之间,并且电流流过15至60ns之间的电池的时间,火山口直径为3‰7μm。火山口深度主要由电池中的电流密度决定。对于在几十纳秒中形成微米尺寸火山口的所有计算变型,电池中的最大电流密度是(1℃3)·108A / cm 2。

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