堆石料颗粒强度时变劣化特征测算方法与初步应用

    Measurement method of time-varying degradation characteristics of rockfill particle strength and its preliminary application

    • 摘要: 使用离散元法模拟堆石料在荷载作用下的流变行为时,通常假定颗粒的强度随时间发生劣化。量化实际颗粒的强度时变劣化特征是进行定量分析的前提,但目前缺乏有效的手段来测量这一特征。为此,本文提出了一种结合试验与理论解析的测算方法。该方法通过分级恒载压缩试验来测定颗粒的蠕变柔量,并利用理论解析给出颗粒在单级恒载作用下的应变场时空演化过程。结合最大拉应变理论,进一步推导出颗粒破坏时间的计算公式。最后,通过荷载水平与破坏时间之间的定量关系来表征颗粒强度的时变劣化过程。通过对10 – 50 mm灰岩颗粒的初步应用验证了该方法的有效性。应用结果表明,荷载水平与破坏时间之间满足指数型方程,衰减参数的离散性服从lognormal分布,而长期强度所对应荷载水平的离散性则服从beta分布。本文提出的方法为定量测算堆石料颗粒强度的时变劣化特征提供了一个可行的解决方案。

       

      Abstract: It is usually assumed that the strength of individual particles deteriorates with time when using the discrete element method to model the creep behaviour of rockfill materials under load. Quantifying the time-varying degradation characteristics of the actual particle strength is essential for a quantitative analysis. However, effective means to measure these characteristics are currently lacking. To address this issue, a measurement method that integrates experimental testing with theoretical analysis is proposed in this paper. In this method, the creep compliance of individual particles is determined by a uniaxial compression test with a multiple-stage constant loading history. Moreover, theoretical analysis is employed to obtain the spatiotemporal evolution of the strain field in individual particles under a single-stage constant loading history. The calculation equation for the particle failure time is then derived based on the maximum tensile strain theory. Finally, the time-varying degradation process of the particle strength is characterized by a quantitative relationship between the load level and the failure time. Preliminary applications on limestone particles (10 − 50 mm) demonstrate the effectiveness of this method. The results also exhibit that the relationship between the load level and the failure time follows an exponential function. Meanwhile, the decay parameter shows a lognormal distributional randomness, and the randomness of the load level corresponding to the long-term strength obeys a beta distribution. The proposed method provides a viable solution to quantitatively measure the time-varying degradation characteristics of rockfill particle strength.

       

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