针对深水斜坡堤堤脚块石的稳定性问题,通过二维物理模型试验进行研究。结果表明,深水斜坡堤堤脚块石的稳定性随相对水深h_t/h及破坏数N_(od)的变化规律同有限水深相比存在一些差异。为此,依据试验结果对可能影响深水斜坡堤堤脚块石稳定...针对深水斜坡堤堤脚块石的稳定性问题,通过二维物理模型试验进行研究。结果表明,深水斜坡堤堤脚块石的稳定性随相对水深h_t/h及破坏数N_(od)的变化规律同有限水深相比存在一些差异。为此,依据试验结果对可能影响深水斜坡堤堤脚块石稳定性的因素进行深入分析,然后将Van der Meer公式做了局部修正,该修正后的公式与试验结果的一致性较好,可供深水斜坡堤设计时参考。展开更多
For toe-shooting method, geomaterial constitutive models concerned are studied. Analysis shows that, although extensively applied in soil mechanics, due to its angular singularity of yielding surface, the Mohr-Coulomb...For toe-shooting method, geomaterial constitutive models concerned are studied. Analysis shows that, although extensively applied in soil mechanics, due to its angular singularity of yielding surface, the Mohr-Coulomb model is not suitable for numerical simulations in large deformation; in this case the rock-fills may be regarded as the Drucker-Prager model and the seaooze as the Prandtl-Reuss model. By comparing experimental data with numerical results, the constitutive model of the seaooze is numerically verified. It shows that, in high strain rate stage forming the blasting crater, the seaooze behaves as ideal non-compressible fluid, while in low strain rate stage during which the reck-fills flow to the blasting crater, the viscosity of the seaooze is negligible.展开更多
文摘针对深水斜坡堤堤脚块石的稳定性问题,通过二维物理模型试验进行研究。结果表明,深水斜坡堤堤脚块石的稳定性随相对水深h_t/h及破坏数N_(od)的变化规律同有限水深相比存在一些差异。为此,依据试验结果对可能影响深水斜坡堤堤脚块石稳定性的因素进行深入分析,然后将Van der Meer公式做了局部修正,该修正后的公式与试验结果的一致性较好,可供深水斜坡堤设计时参考。
基金Sponsored by the National Natural Science Foundation of China (10072070)
文摘For toe-shooting method, geomaterial constitutive models concerned are studied. Analysis shows that, although extensively applied in soil mechanics, due to its angular singularity of yielding surface, the Mohr-Coulomb model is not suitable for numerical simulations in large deformation; in this case the rock-fills may be regarded as the Drucker-Prager model and the seaooze as the Prandtl-Reuss model. By comparing experimental data with numerical results, the constitutive model of the seaooze is numerically verified. It shows that, in high strain rate stage forming the blasting crater, the seaooze behaves as ideal non-compressible fluid, while in low strain rate stage during which the reck-fills flow to the blasting crater, the viscosity of the seaooze is negligible.
