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Validity of fully drained, fully undrained and u-p formulations for modeling a poroelastic half-space under a moving harmonic point load

机译:完全排水,完全不排水和u-p公式在运动谐波点载荷下对多孔弹性半空间建模的有效性

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摘要

Biot's theory has been widely employed to study responses of saturated soil under dynamic loads. To simplify the analysis, three simplified formulations based on Biot's theory have been proposed, including the u-p formulation, fully undrained formulation and fully drained formulation. The u-p formulation is established by neglecting the relative pore fluid acceleration. The fully undrained formulation founds on the assumption of no relative pore fluid displacement. The fully drained formulation supposes an infinite soil permeability. Nevertheless, the successful applications of these simplified formulations are hindered because of their indefinite application scopes. To overcome this, this paper carries out a comparative study of the simplified formulations for modeling a saturated poroelastic half-space subjected to a moving harmonic point load. The three simplified formulations are investigated by comparing with Biot's u-w formulation. A triple Fourier transform is first used to transform the four formulations into the frequency-wavenumber domain. Then an analytical inverse transform with respect to the frequency is performed to obtain the vertical soil displacement and pore pressure in the time-wavenumber domain. A parameter R_Ω defined in the wavenumber domain, which integrates effects of the soil permeability, load oscillating frequency and moving load velocity, is proposed to determine the validity ranges of the three simplified formulations. Some critical values of R_Ω are suggested and applied to a model in a previously published paper by Siddharthan et al.
机译:Biot理论已被广泛用于研究动荷载下饱和土的响应。为了简化分析,提出了三种基于Biot理论的简化配方,包括u-p配方,完全不排水的配方和完全排水的配方。通过忽略相对孔隙流体的加速度来建立u-p公式。完全不排水的配方建立在没有相对孔隙流体位移的假设下。完全沥干的配方需要无限的土壤渗透性。然而,由于其不确定的应用范围,阻碍了这些简化制剂的成功应用。为了克服这个问题,本文对简化公式进行了比较研究,该简化公式用于模拟承受运动谐波点载荷的饱和多孔弹性半空间。通过与Biot的u-w配方进行比较,研究了三种简化的配方。首先使用三重傅立叶变换将这四个公式变换为频率-波数域。然后对频率进行解析逆变换,以获得时波数域中的垂直土壤位移和孔隙压力。提出了在波数域中定义的参数R_Ω,该参数综合了土壤渗透性,载荷振荡频率和运动载荷速度的影响,以确定三种简化公式的有效范围。 Siddharthan等人在先前发表的论文中提出了一些R_Ω的临界值,并将其应用于模型。

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  • 来源
    《Soil Dynamics and Earthquake Engineering》 |2012年第2012期|p.292-301|共10页
  • 作者单位

    MOE Key Laboratory of Soft Soils and Ceoenvironmental Engineering Zhejiang University Hangzhou 310027 PR China;

    MOE Key Laboratory of Soft Soils and Ceoenvironmental Engineering Zhejiang University Hangzhou 310027 PR China College of Architecture and Civil Engineering Wenzhou University Wenzhou 325035 PR China;

    College of Architecture and Civil Engineering Wenzhou University Wenzhou 325035 PR China;

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