水面放电在水中传播所需的临界电场

M. Edirisinghe, A. Liyanage, V. Cooray
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引用次数: 2

摘要

本研究的核心目的是研究空气在水面上的放电行为,并研究闪电脉冲进入水体的方式。在实验中,从-550千伏到350千伏的标准闪电脉冲被引导到水面上,并使用两台相机拍摄了水面放电。水的电导率在41.5 μS/cm ~ 51.5 mS/cm之间变化。研究中进行的分析表明,当水的电导率较低时,电流更倾向于沿着水面而不是进入水中。计算得到的电场与电导率呈对数变化关系。对于这种变化,可以观察到饱和趋势,并且似乎存在一个电场临界值,低于该临界值,在任何导电性水平下都不会发生穿透。根据本研究的实验结果,可以估计出正极击穿小于1.5×105 V/m,负极击穿小于-5.0×105 V/m。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Critical electric field needed for the propagation of surface discharges on water
The core objective of this study was to investigate the behavior of electric discharge exited in air over water and to study the way in which the lightning impulse is conducted into a water body. During the experiments, standard lightning impulses from -550 kV to 350 kV have been directed on water surfaces and surface discharges has been photographed using two cameras. The conductivity of the water has been varied from 41.5 μS/cm to 51.5 mS/cm. Analysis carried out in the study revealed that the current rather travels along the water surface than into the water when the conductivity of the water is low. A logarithmic variation was observed between the calculated electric field and the conductivity. For this variation a saturating trend could be observed and it appeared as if there is a critical value for the electric field below which no penetration will occur at any level of conductivity. Based on the experimental results of this study it can be estimated that to be less than 1.5×105 V/m for the positive breakdown and -5.0×105 V/m for the negative breakdown.
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