冷却水中盐迁移现象的机理及其对冰闪络的影响

K. Wang, Tianzheng Wang, Yu Deng, Z. Jia, Z. Guan
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引用次数: 2

摘要

华南地区的绝缘子在早春常发生积冰现象。2008年,南方城市遭受了严重的冰雪灾害,造成了巨大的经济损失,冰雪问题越来越受到人们的关注。本文讨论了盐在冰层中的迁移,给出了污染程度与冷却时间的关系,并对冰闪蒸最容易发生的时间进行了解释。冷却水从固液界面冻结到水膜顶部。由于低温下溶解度下降,出现了盐迁移现象。最后,根据110 kV全尺寸绝缘子试验,熔水电导率接近应用水电导率的6倍,得出冰层中盐迁移是引发冰闪络的关键原因。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The mechanism of salt migration phenomena in cooling water and its impact on ice flashover
Ice accumulation always happen to insulators in south China in early spring. In the year 2008, southern cities were suffered from serious icing disaster, leading to great economic loss, thus icing problems are paid more attentions. This paper is concerned with salt migration in ice layer, the relationship between pollution level and cooling time were presented, as well as interpretations on when the ice flashover is most likely to appear. Cooling water was freezing from the solid-liquid interface to the top of water film. Salt migration phenomenon appeared because of the decline of solubility under low temperature. Finally according to 110 kV full-size insulator test, melting water conductivity is nearly six times of the applied water conductivity and conclusions can be drawn that salt migration in ice layer was a critical reason to initiate ice flashover.
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