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The study investigates the slipperiness of ice by simulating ice-glass friction at the nanoscale using first-principles calculations and upscaling to the macroscale with a frictional heating model. Nanoscale simulations alone overestimate the coefficient of friction, but incorporating frictional heating reveals a significant temperature increase at the contact point, approaching the melting point even at modest speeds. This frictional heating mechanism explains ice's slipperiness and aligns well with experimental friction data across various velocities.
Ice's slipperiness isn't just about a lubricating film, but hinges on frictional heating that drives contact temperatures close to melting, even at modest speeds.
The origin of ice's slipperiness has long puzzled scientists. To resolve this question, we simulate ice- glass (amorphous silica) friction at the nanoscale from first principles and upscale to the macroscale using a frictional heating model. We find that nanoscale simulations alone cannot capture the correct velocity dependence of ice friction, resulting in an overestimated coefficient of friction. By properly accounting for frictional heating, we find a strong increase in contact temperature toward the melting point, even under modest motion of 1 millimeter with velocities above 0.1 m/s, yielding excellent agreement with experimental friction data across a wide range of velocities. While the initial formation of a lubricating film on ice may occur without heating, the ultimate slipperiness of ice hinges on frictional heating, as proposed by Bowden and Hughes in 1939, but without incorporating melting.
