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

机译:用ZRDX阴极对真空弧的阴极点中的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:已经开发出氢同位素对流扩散的2D轴对称流体动力学模型,以用ZRDX阴极描述其对真空电弧的阴极点等离子体的解吸。结果表明,主要决定阴极点细胞的功能性的流体动力学阶段的氘解吸的限制因素,其在从体积到表面的阴极中转移。通过将熔融金属的几乎解吸的表面层压制到火山口外围区域,维持在表面附近的高梯度的表面浓度。阴极体积,气体完全解吸的,大致等于熔融质量的体积,在烧架形成时压出。氘解吸后的对流性质在形成微陆时导致氘离子的数量比具有Zrd0.67阴极的真空电弧中的Cs血浆中的锆离子量大4-6倍。

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