台风期海堤护面块体稳定性研究

RESEARCH ON THE STABILITY OF ARMOR BLOCKS ON SEAWALLS DURING TYPHOON CONDITIONS

  • 摘要: 通过收集台风后海堤护面块体失稳情况,分析了失稳护面块体分布特征,并利用实测波浪资料结合卫星照片分析了海堤建成后护面块体稳定状况,继而识别出作用海堤的典型台风过程。基于ERA5风场建立了风暴潮-台风浪耦合模型,反演了海堤前风暴潮和台风浪发展过程,利用护面块体稳定重量计算公式结合参数选取方法形成参数化方案,根据典型台风过程中护面块体实际稳定状态分析了各个参数化方案的适用性。研究结果表明:海堤护面块体失稳后,块体失稳概率沿横向基本成正态分布;ERA5风场驱动的风暴潮-台风浪耦合模型可以较好地反演出海堤前潮位和波浪情况;开敞海域海堤护面块体稳定性计算需要考虑周期影响,小波高、长周期海浪作用时护面块体也会发生失稳破坏;苏联规范公式组合H4%更适用于本海堤护面块体稳定重量计算,和台风期护面块体实际稳定状况吻合度达到了83%。

     

    Abstract: Field investigations are carried out to analyze armor block displacements caused by typhoon events, with a focus on characterizing the spatial distribution patterns of dislocated blocks. Utilizing measured wave data and satellite imagery, the stability of armor blocks is assessed, and representative typhoon cases are identified. A storm-wave coupled model, forced by the ERA5 wind field, is employed to simulate storm surge and wave evolution in the seawall foreshore. Furthermore, a parametric approach is developed by integrating the armor block stability weight formula with parameter optimization techniques. The feasibility of each parametric method is systematically evaluated against field-observed block stability conditions. The research results indicate that the instability probability of armor blocks along the transverse direction of the seawall follows a normal distribution. The storm-wave coupled model driven by the ERA5 wind field effectively reproduces the generation and the development of storm surges and waves in the foreshore zone. Notably, armor block damage can occur even under relatively low wave heights if wave periods are sufficiently long, suggesting that wave period effects should be incorporated into stability formulations for open-coast applications. The parametric method based on the Soviet standard formula, when combined with the H4% wave height parameter, achieves an agreement level of 83% with field observations, indicating its improved suitability for estimating the armor block stability weight under typhoon conditions.

     

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