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

机译:ZrDx阴极在真空电弧阴极点中氢同位素解吸的模拟

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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.
机译:已经开发了氢同位素对流扩散的二维轴对称流体力学模型,以描述它们在ZrDx阴极中解吸到真空电弧的阴极点等离子体中的过程。结果表明,限制因素主要是决定阴极点电池功能的流体动力学阶段中氘的脱附,是其在阴极中从体积到表面的转移。通过将几乎解吸的熔融金属表面层压向火山口周边区域,可保持表面附近氢同位素浓度的高梯度。气体完全从中解吸出来的阴极体积大约等于在形成火山口时被压出的熔融物质的体积。形成微弹坑时氘解吸的对流性质导致以下事实:氘离子的数量比带有ZrD0.67阴极的真空电弧CS等离子体中锆离子的数量大4-6倍。

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