冻融荷载作用下砂岩损伤特性分析
[Abstract]:With the further development of the western part of China, a large number of geotechnical engineering will be carried out in the cold regions of the western part of China. In order to ensure the safety of the project, it is necessary to study the freeze-thaw mechanical properties of rocks. In this paper, the damage characteristics of sandstone under the action of freeze-thaw and load are studied systematically by the method of combining theory with test, starting from the actual rock mass engineering in cold area. The whole piece of fresh large sandstone was processed into standard cylindrical specimen, and the freezing and thawing cycle test was carried out after saturated. When the cycles of freezing and thawing were 0 times, 5 times, 10 times, 20 times and 40 times, the confining pressure was 0 MPA, 2 MPA, and 2 MPA, respectively, when the cycles of freezing and thawing were 0 times, 5 times, 10 times, 20 times and 40 times, respectively. Triaxial compression test of 4MPa and 6MPa. The main failure forms of sandstone are obtained by observing the experimental phenomena, and the mechanical parameters of sandstone under freeze-thaw cycle and load are obtained by analyzing and discussing the test results, as well as the variation of strength and deformation characteristics of sandstone with the times of freezing-thawing cycle and confining pressure. Based on the theory of continuous damage mechanics and the generalized strain equivalence principle, the damage model of sandstone is established by using the Weibull distribution and the Poisson distribution to describe the random characteristics of the strength of sandstone microelement, based on the Dp criterion of rock. The rationality of the model is verified by the experimental data. The analysis and comparison show that there is no significant difference between the two distributions in describing the process of sandstone compression failure, but the expression of parameters obtained by using Poisson distribution is rather complex, so the practicability is not strong. The damage constitutive model of sandstone is modified. The modified model can better reflect the change of the stress-strain curve of sandstone, and describe the residual strength of sandstone more accurately, and the physical significance of the model parameters is discussed, and the parameters of the model are analyzed and discussed, and the physical significance of the parameters of the model is analyzed and discussed. The damage model of sandstone is extended from the conventional triaxial stress state to the true triaxial stress state, so that the influence of intermediate principal stress on the strength and mechanical properties of sandstone can be described theoretically. The damage model of frozen-thawed sandstone under true triaxial stress is established and its damage mechanical characteristics are analyzed. The rationality of the damage model is verified by using the freezing-thawing cycle and triaxial compression test data of sandstone. When the confining pressure is constant, the total damage caused by freeze-thaw cycle and load to sandstone increases with the increase of freezing-thawing cycle times, meanwhile, the plasticity of sandstone is enhanced and the brittleness of sandstone is weakened by freezing-thawing cycle. When the number of freeze-thaw cycles is constant, the total damage of sandstone decreases with the increase of confining pressure, and the plastic properties are obviously enhanced.
【学位授予单位】:西安科技大学
【学位级别】:硕士
【学位授予年份】:2015
【分类号】:TU45
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