Abstract

The research on snow-accreted insulators have been performed in an artificial climate chamber. However, the differences in the distribution, density and compactness of snow accretion under natural and artificial simulation environments cause differences in the flashover performance of snow-covered insulators. In the present work, a series of flashover tests were conducted on snow-coated glass and silicone rubber insulators in the climate chamber and at Xuefeng Mountain Natural Icing Test Base. The discrepancies in the electrical characteristics and flashover process of snow-covered insulators under two test environments were compared and analyzed. Results show that the arc flashover gradient of snow accreted insulator at high altitude site is higher than that in the laboratory because of the differences of the environmental parameters. Affected by the adiabatic effect and capillary action of snow layer, within the range of the study the flashover gradient of insulators covered with snow increases with the increasing in the snow thickness. The calculation of various forces applied on arcs during its propagation demonstrates that when the arc current is less than 0.2 A, the local arcs develop along the snow surface of the insulators under the action of an electrostatic force. As the current increases beyond 0.2 A, the thermal buoyancy is predominant, thereby causing arcs to levitate from the insulator surface.

Highlights

  • Insulator is an important facility of transmission lines, so its electrical performance plays a decisive role in the satisfactory reliability of power systems

  • Ice and snow accretion on outdoor insulators considerably degrades their electric strength in cold climate regions, which leads to numerous flashover accidents in China and abroad [1]–[4]

  • Hu et al [13] researched the effect of snow accretion on the various type of the insulators in an artificial climate chamber, and arrived at the conclusion that the relationship between the snow flashover gradient of the insulators and equivalent salt deposit density is a power function with a negative exponent

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Summary

Introduction

Insulator is an important facility of transmission lines, so its electrical performance plays a decisive role in the satisfactory reliability of power systems. Ice and snow accretion on outdoor insulators considerably degrades their electric strength in cold climate regions, which leads to numerous flashover accidents in China and abroad [1]–[4]. To the effect of snow accretion on the external insulation of transmission lines. Hu et al [13] researched the effect of snow accretion on the various type of the insulators in an artificial climate chamber, and arrived at the conclusion that the relationship between the snow flashover gradient of the insulators and equivalent salt deposit density is a power function with a negative exponent. For the insulators covered with an uneven snowpack distribution, the discharge developed along the leeward side [15]. Zhang et al [17] pointed out that the water melted from snow wets the pollution on post insulator surface to form a highly conductivity water film, which is a key factor

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