Abstract

Wet snow can create serious electrical and mechanical problems to power transmission networks due to its high adherence to materials. In this study, both adherence of wet snow to cables and wet snow shedding following the application of periodic loads were investigated in small-scale experiments. Wet snow was obtained from fresh dry snow collected from the top layer of snow accumulated outdoors. The collected dry snow was exposed to warm air for periods of time long enough to obtain the desired liquid water content (LWC) values. Wet snow sleeves were manually prepared after being compressed around the cable. The room temperature, snow sleeve length, cable diameter, and cable length were kept constant for each experiment. Dynamic load on the cable was simulated by a periodic excitation applied at one end of the cable, while the other end was fixed. Since fading adhesion is a condition for snow shedding, and since LWC is a critical factor influencing adhesion, the effects of excitation frequency and amplitude were investigated for different LWC values. LWC was examined for values from 10 to 40%. When free water began to increase, snow at this stage was wet and it adhered stronger to the cable than low LWC, where there is no enough water to stick on the cable or high LWC where snow is transparent. The LWC range was found experimentally between 20 to 30% (Hefny R. et al., 2009). Different snow shedding scenarios were studied, for which the shedding sequence and acceleration were observed at the excitation point, also cable tension at the fixed end and vertical displacement at the mid-point of the span were measured.

Highlights

  • Dry snow accretion occurs at sub-zero air temperature, and wind speed less than 2 m/s

  • The aims of the present study were undertaken to predict snow shedding from cables due to dynamic effects, such as those that may result from the effect of wind or other external loads or from load imbalances due to propagating snow shedding on an adjacent span

  • Procedure and Sample Preparation Wet snow sleeve molding: Fresh dry snow was used to prepare the wet snow in the climate room

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Summary

Introduction

Dry snow accretion occurs at sub-zero air temperature, and wind speed less than 2 m/s. Its density is too low; it does not exceed 0.1 g/cm. Dry snow adhesive force is small; it rarely gives rise to extreme loads. Dry snow cylindrical sleeve can form and shed spontaneously, giving dynamic vibration (Sakamoto, 2000). Whereas wet snow accretion occurs at temperature above freezing point, its density spans a range from 0.1 to 0.95 g/cm. Wet snow accretion can form a cylindrical sleeve which cannot shed by wind because of its greater adhesive strength (Sakamoto, 2000)

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