2018
DOI: 10.1016/j.compgeo.2018.04.012
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Vertical vibrations of rigid foundations of arbitrary shape in a multi-layered poroelastic medium

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Cited by 29 publications
(9 citation statements)
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“…For the plane strain problem in a Cartesian coordinate system, the constitutive equations for the transversely isotropic poroelastic medium can be listed as bellow 13 σxbadbreak=c11uxxgoodbreak+c13uzzgoodbreak−αhp\begin{equation}{\sigma }_x = {c}_{11}\frac{{\partial {u}_x}}{{\partial x}} + {c}_{13}\frac{{\partial {u}_z}}{{\partial z}} - {\alpha }_hp\end{equation} σzbadbreak=c13uxxgoodbreak+c33uzzgoodbreak−αvp\begin{equation}{\sigma }_z = {c}_{13}\frac{{\partial {u}_x}}{{\partial x}} + {c}_{33}\frac{{\partial {u}_z}}{{\partial z}} - {\alpha }_vp\end{equation} τxzbadbreak=c44()uxz+uzx\begin{equation} {\tau}_{\textit{xz}}={c}_{44}\left(\frac{\partial {u}_{x}}{\partial z}+\frac{\partial {u}_{z}}{\partial x}\right) \end{equation} pbadbreak=Mf()αhuxx+αvuzz+wxx+wzz\begin{equation}p = - {M}_f \left({\alpha }_h\frac{{\partial {u}_x}}{{\partial x}} + {\alpha }_v\frac{{\partial {u}_z}}{{\partial z}} + \frac{{\partial {w}_x}}{{\partial x}} + \frac{{\partial {w}_z}}{{\partial z}}\right)\end{equation}Where cij(i,j=1,2,3,4...…”
Section: Fundamental Solutions For Layered Poroelastic Mediamentioning
confidence: 99%
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“…For the plane strain problem in a Cartesian coordinate system, the constitutive equations for the transversely isotropic poroelastic medium can be listed as bellow 13 σxbadbreak=c11uxxgoodbreak+c13uzzgoodbreak−αhp\begin{equation}{\sigma }_x = {c}_{11}\frac{{\partial {u}_x}}{{\partial x}} + {c}_{13}\frac{{\partial {u}_z}}{{\partial z}} - {\alpha }_hp\end{equation} σzbadbreak=c13uxxgoodbreak+c33uzzgoodbreak−αvp\begin{equation}{\sigma }_z = {c}_{13}\frac{{\partial {u}_x}}{{\partial x}} + {c}_{33}\frac{{\partial {u}_z}}{{\partial z}} - {\alpha }_vp\end{equation} τxzbadbreak=c44()uxz+uzx\begin{equation} {\tau}_{\textit{xz}}={c}_{44}\left(\frac{\partial {u}_{x}}{\partial z}+\frac{\partial {u}_{z}}{\partial x}\right) \end{equation} pbadbreak=Mf()αhuxx+αvuzz+wxx+wzz\begin{equation}p = - {M}_f \left({\alpha }_h\frac{{\partial {u}_x}}{{\partial x}} + {\alpha }_v\frac{{\partial {u}_z}}{{\partial z}} + \frac{{\partial {w}_x}}{{\partial x}} + \frac{{\partial {w}_z}}{{\partial z}}\right)\end{equation}Where cij(i,j=1,2,3,4...…”
Section: Fundamental Solutions For Layered Poroelastic Mediamentioning
confidence: 99%
“…For the plane strain problem in a Cartesian coordinate system, the constitutive equations for the transversely isotropic poroelastic medium can be listed as bellow 13 𝜎 𝑥 = 𝑐 44 . Also, the expression for fluid discharge 𝑄 𝑓 is defined 13 :…”
Section: Basic Equationsmentioning
confidence: 99%
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“…Thereafter, Biot's poroelastodynamics theory has been employed by many researchers to study dynamic interaction problems between foundations and fluidsaturated porous media due to its close relevance to various practical problems in civil engineering. For example, the dynamic responses of rigid foundations under vertical loading were investigated by Kassir and Xu [2] for rigid strips, Jin and Liu [3], Zeng and Rajapakse [4] and Ai et al [5] for rigid circular plates, and Halpern and Christiano [6], Senjuntichai et al [7][8] and Keawsawasvong and Senjuntichai [9] for rigid rectangular plates. In addition, the influence of the flexibility of foundations on dynamic interaction between foundations and supporting poroelastic media was also investigated by Senjuntichai and Kaewjuea [10] for multiple flexible strips and Senjuntichai and Sapsathiarn [11] for a flexible circular plate.…”
Section: Introductionmentioning
confidence: 99%