Apart from one report of lightning that turned out to be an electrical flash, it was typical April weather for the region—light rain with a maximum wind speed of less than 50 mph, certainly nothing that would normally bring down utility poles. What, then, led to this disastrous utility pole failure?
A later report from an investigation into the event revealed that several consecutive poles in the middle of the 26 had a “significant amount of internal groundline decay” and were the first poles to fail. Rather than breaking due to extreme winds, these poles buckled in the face of moderate gusts because internal rot left them with just a thin remaining outer shell at the ground line – which is the pole section from 6 inches above ground to 18 inches below. With two circuits of large diameter electric lines attached to these poles, the failure of the first poles caused others on both sides to be pulled down by the conductors in a domino fashion.
Over the past decade, innovative inspection service providers have developed new techniques to detect these unseen risks in a scalable way. Now, after extensive usage, data analysis shows significant savings from this more precise method – not just from earlier identification of poles that were higher risk than initially believed but also by avoiding the premature removal of others that were in better shape than old inspection approaches suggested.
Any executive responsible for risk management at an electric utility or telecommunications provider with wood pole overhead lines should understand the distinction between decayed poles that fail in a bending mode versus those that are likely to fail due to localized buckling. The likelihood of buckling often is not fully appreciated or even detected and can cause the most dangerous and expensive surprises. It is essential to know the difference between these failure modes because it impacts how these conditions can be detected as well as properly and economically addressed.
When advanced internal decay occurs in a utility pole, the outer shell wall becomes thin – especially near the groundline of the pole – and localized buckling becomes a risk. It takes far less wind load to cause a thin-shelled pole – hiding hollow internal pockets created by decay – to buckle. With a moderate wind and a pole with advanced internal decay, the thin outer shell may collapse into itself causing the structure to fall. The key question to ask is, “Did our assessment of a pole’s remaining strength account for advanced internal decay at the groundline?”