论文信息 - On the nature of the minimum creep rate – time correlation for soil, ice, and frozen soil

On the nature of the minimum creep rate – time correlation for soil, ice, and frozen soil

This technical note examines the nature and consequences of the linear correlation observed between the logarithm of the minimum creep rate, and the logarithm of the time to reach this minimum creep rate, tm, in soil, ice, and frozen soil. Simple mathematical creep models show that this correlation is due to the existence of an approximately constant strain at the minimum strain rate, and the relative insensitivity of the double logarithmic plot to small deviations from this approximately constant strain. Keywords: creep, failure, frozen soil, ice, unfrozen soil.

John M. Ting | J. Ting

[1] Branko Ladanyi,et al. An Engineering Theory of Creep of Frozen Soils , 1972 .

[2] John M. Ting,et al. Tertiary creep model for frozen sands , 1983 .

[3] John M. Ting,et al. Application of the Andrade equation to creep data for ice and frozen soil , 1979 .

[4] S. Leroueil,et al. CREEP AND FAILURE OF SLOPES IN CLAYS , 1981 .

[5] R. G. Campanella,et al. Triaxial and Plane Strain Creep Rupture of an Undisturbed Clay , 1974 .

[6] Frank Garofalo,et al. Fundamentals of creep and creep-rupture in metals , 1965 .

[7] J. Ting. The creep of frozen sands: Qualitative and quantitative models, part 2 , 1981 .

[8] Malcolm Mellor,et al. Mechanical Properties of Polycrystalline Ice , 1980 .

[9] J. W. Glen,et al. The creep of polycrystalline ice , 1955, Proceedings of the Royal Society of London. Series A. Mathematical and Physical Sciences.