The kinetic friction of saline ice against itself at low sliding velocities

D. E. Jones, Francis E. Kennedy, E. M. Schulson

Annals of Glaciology · 1991 · 40 citations · 4 references

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Abstract

An experimental investigation was performed on the kinetic friction coefficient of laboratory-grown, columnar saline ice sliding against itself. Tests were performed on a dual-opposing load apparatus specially manufactured for attachment to an MTS testing system. The mean kinetic friction coefficient, μ , was measured for sliding velocities from 10 −6 to 5 × 10 −2 m s −1 at temperatures from —3° to —40°C under a contact pressure of about 20 kPa. The ice specimens were oriented with grain columns perpendicular to the sliding interface. At -3°C and at —10°C, three distinct regions were observed: from 10 −6 to about 10 −5 ms −1 , μ was nearly constant at 0.5; at velocities from 10 −5 to 10 −3 m s −1 , μ began to drop rapidly to about 0.1; and, above 10 −3 m s −1 , μ began to level off at ~0.05. The velocity at which μ began to decline increased with decreasing temperature. At temperatures below —10°C, μ increased from ~0.5 at v = 10 −6 ms −1 to a peak value of ~0.7 near a velocity of 5 × 10 −5 ms −1 and then fell rapidly to about 0.1 at 10 −2 ms −1 . In general, μ increased with decreasing temperature and sliding velocity.

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