PAVEMENT CRACKING IN WEST TEXAS DUE TO FREEZE-THAW CYCLING.
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Samples from two compactive efforts were frozen in a biaxial closed system. Suction and temperature within the samples were monitored and volume changes after each freeze-thaw period were recorded. Coefficients of thermal activity were calculated from the dimension measurements. These coefficients showed a relationship with the as-compacted total soil moisture suction, which was similar for all materials. Finite element studies of the thermal strains that develop in a pavement showed that the thermally induced tensile stresses in the base course are far in excess of tensile strengths for initially intact pavements.