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Ion Migration in the Process of Water Freezing under Alternating Electric Field and Its Impact on Insulator Flashover

机译:交变电场下水冻结过程中的离子迁移及其对绝缘子闪络的影响

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摘要

Ice flashover threatens the security and reliability of power transmission. However, the ice flashover mechanism of insulators remains poorly understood. This study analyses water droplet freezing and ion distribution in ice layer under alternating electric field. It also investigates ion migration during icing process of insulator string under alternating electric field and its effects on insulator flashover. Results showed that the average freezing time of water droplets was related to electric field strength. The extent of ion migration during freezing decreased with increasing electric field strength. The maximal melting water conductivity of the ice layer and icicle of the insulator formed under energized condition was higher than the corresponding freezing water conductivity but lower than that under non-energized condition. Furthermore, the hanging location of each insulator significantly affected the melting water conductivity of the ice layer. The surface conductivity of the ice layer increased because of the conductive ion migration in freezing water during freezing, which was an important factor that decreased the flashover voltage of the ice-covered insulator. The existence of alternating electric field would impact the extent of ion migration. This study may serve as a reference for updating prediction flashover model of ice-covered insulators during the melting period.
机译:冰闪络威胁着输电的安全性和可靠性。但是,对绝缘子的冰闪机理仍知之甚少。本研究分析了交变电场下冰层中的水滴冻结和离子分布。它还研究了在交变电场下绝缘子串结冰过程中的离子迁移及其对绝缘子闪络的影响。结果表明,水滴的平均凝固时间与电场强度有关。冷冻过程中离子迁移的程度随电场强度的增加而降低。通电条件下形成的绝缘子的冰层和冰柱的最大融水电导率高于相应的冻结水电导率,但低于非通电条件下的冰水融化率。此外,每个绝缘子的悬挂位置显着影响了冰层的融水电导率。冰层的表面电导率由于在冷冻过程中在冷冻水中的导电离子迁移而增加,这是降低覆冰绝缘子的闪络电压的重要因素。交变电场的存在会影响离子迁移的程度。该研究可为冰期融化过程中更新冰覆绝缘子的预测闪络模型提供参考。

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