周期结构波阻板在层状横观各向同性土中的隔振性能与理论解答

    Vibration isolation performance and theoretical solution of periodic structure wave impeding block in layered transversely isotropic soil

    • 摘要: 相较于传统波阻板(WIB),周期结构波阻板(PSWIB)具有带隙特性,可根据振源特性设计参数实现对目标频率振动的隔离,然而既有研究忽略了PSWIB在土体中的性能表现。为此,将PSWIB置于更为复杂的层状横观各向同性(TI)土体环境中,基于声子晶体与等效介质理论,结合刚度矩阵法推导PSWIB在层状TI场地的动力响应基本解,评估在此复杂场地条件下PSWIB的隔振性能。结果表明,即使在考虑土体特性的情况下,与WIB相比,PSWIB 的隔振效率提高约43.3%。周期层数与每层周期数等几何参数对隔振效果均表现出正向调控,而埋深的影响在t=0.8B时达到峰值,加速度幅值减小1.17 m/s2。此外,研究揭示了土体TI特性对场地振动传播的影响规律,当Eh/Ev由 0.5 增至2.0时,位移峰值升高17.5%,对应主导频率降低。

       

      Abstract: Compared with traditional wave impeding block (WIB), periodic structure wave impeding block (PSWIB) exhibit inherent bandgap characteristics and can be tailored to isolate vibration waves at target frequencies; however, their performance in realistic soil environments has received limited attention. This study investigates the vibration isolation behavior of PSWIB embedded in layered transversely isotropic (TI) soils, aiming to clarify the underlying wave propagation mechanisms and evaluate their practical effectiveness. By integrating the theory of phononic crystals with the equivalent medium approach, a fundamental solution for the dynamic response of PSWIB in layered TI sites is derived using the stiffness matrix method. The proposed model is then employed to systematically examine the influence of geometric configuration and soil anisotropy on vibration isolation efficiency. The results indicate that PSWIB improves the isolation efficiency by approximately 43.3% compared with conventional WIBs, even under complex TI soil conditions. Increasing the number of periodic layers and cycles per layer enhances the bandgap-induced attenuation, while the optimal burial depth occurs at t = 0.8B, where the acceleration amplitude is reduced by 1.17 m/s2. Furthermore, soil transverse isotropy significantly affects wave propagation: as the horizontal-to-vertical stiffness ratio Eh/Ev increases from 0.5 to 2.0, the peak displacement increases by 17.5% accompanied by a downward shift of the dominant frequency.

       

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