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How Potholes Form

May 6th 2011 00:05
How potholes form. Water seeps through the cracks in pavement and softens the road’s base, collects then freezes. When the water freezes, it expands and forces the pavement up. Traffic further stresses the pavement. The sun dries up the water leaving a hole under the pavement. With no base, the pavement is weakened and collapses under the weight of traffic. A pothole is formed where the pavement collapsed. Wear from additional traffic expands the hole.
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Most potholes are formed due to fatigue of the road surface. As fatigue fractures develop they typically interlock in a pattern known as "alligator cracking". The chunks of pavement between fatigue cracks are worked loose and may eventually be picked out of the surface by continued wheel loads, thus forming a pothole.
The formation of potholes is exacerbated by low temperatures, as water expands when it freezes to form ice, and puts greater stress on an already cracked pavement or road. Once a pothole forms, it grows through continued removal of broken chunks of pavement. If a pothole fills with water the growth may be accelerated, as the water "washes away" loose particles of road surface as vehicles pass. In temperate climates, potholes tend to form most often during spring months when the subgrade is weak due to high moisture content. However, potholes are a frequent occurrence anywhere in the world, including in the tropics.

Potholes can grow to feet in width, though they usually only become a few inches deep, at most. If they become large enough, damage to tires and vehicle suspensions occurs. Serious road accidents can occur as a direct result, especially on motorways where vehicle speeds are greater. They are frequently almost invisible to road users.




*This article is licensed under the GNU Free Documentation License. It uses material from the Wikipedia article for Pothole.
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