Simulation of the hydrogen isotope desorption in the cathode spot of a vacuum arc with a ZrDx cathode

I. Uimanov, D. Shmelev, S. Barengolts
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引用次数: 3

Abstract

2D axisymmetric hydrodynamic model of convective diffusion of hydrogen isotopes has been developed to describe their desorption into cathode spot plasma of the vacuum arc with a ZrDx cathode. It was shown that limiting factor, which mainly determines deuterium desorption in hydrodynamic stage of functioning of cathode spot cell, is its transfer in the cathode from the volume to the surface. High gradient of hydrogen isotope concentration near the surface is maintained by pressing of almost desorbed surface layers of molten metal to crater peripheral area. Cathode volume, from which the gas is completely desorbed, is approximately equal to the volume of molten mass, pressed out upon formation of crater. Convective nature of deuterium desorption upon formation of microcrater results in the fact that the number of deuterium ions is by 4-6 times larger than the quantity of zirconium ions in CS plasma of vacuum arc with ZrD0.67 cathode.
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用ZrDx阴极模拟真空电弧阴极点氢同位素解吸
建立了氢同位素对流扩散的二维轴对称流体动力学模型,描述了氢同位素在ZrDx阴极真空电弧阴极点等离子体中的解吸过程。结果表明,决定阴极点状电池水动力阶段氘脱附的主要限制因素是其在阴极内从体积向表面的转移。近地表氢同位素浓度的高梯度是通过将几乎解吸的金属熔液表层压向火山口周边区域来维持的。气体被完全解吸的阴极体积,大约等于在火山口形成时被压出的熔融质量的体积。由于形成微坑时氘的对流解吸特性,使得阴极为ZrD0.67的真空电弧CS等离子体中氘离子的数量比锆离子的数量多4-6倍。
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