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Abstract

In this paper, the scattering and vibration isolation of elastic waves from the open trench are analyzed and discussed in the time domain using the scaled boundary finite element method (SBFEM). Based on the theory of soil-structure interaction, the site with an open trench is decomposed into a near-field system and an infinite far-field system. The quadtree domain decomposition technique is employed for SBFEM mesh discretization of the near-field. The far-field is rigorously modeled by the displacement unit impulse response matrix. The obliquely plane elastic wave from the far-field is converted into a traction force acting on the near/far-field boundary. The time-space domain numerical model is established for elastic wave propagation in half-space with an open trench. Finally, through numerical examples to verify the effectiveness of the method of this paper, and parametric analyze the effect law of the incidence angle and the trench depth, etc., on the vibration isolation performance.

Keywords

open trench plane elastic wave scattering vibration isolation effect scaled boundary finite element method

1. Introduction

The man-made ground vibration including transportation, machinery equipment, and engineering construction is spread around through the ground, bringing adverse effects to the life of nearby residents, the safety of the surrounding buildings, and the accuracy of precision instruments. The ground vibration control has become one of the hot topics to be solved in the field of geotechnical engineering.

At present, the most common mitigation for the vibration propagation is the installation of wave barriers between the vibration source and the protected building, which include open and filled trench (Adam and Estorff, 2005; Ahmad and Al-Hussaini, 1991; Andersen and Nielsen, 2005; Beskos et al., 1986; Çelebi et al., 2009; Emad and Manolis, 1985; Herbut, 2020; Murillo et al., 2009; Saikia and Das, 2014; Shrivastava and Rao, 2002; Ulgen and Toygar, 2015; Woods, 1968; Xu et al., 2015; Zhou et al., 2021), row piles (Gao et al., 2006; Kattis et al., 1999), and wave impeding block (Gao et al., 2017; Ma et al., 2019). The open trench is considered to be the most efficient barrier for vibration isolation and is widely used in vibration isolation engineering. Up to now, the research methods on the vibration isolation performance of open trench mainly include experimental studies, numerical simulation, and theoretical analysis. In terms of experiments, Woods (1968) is the first to study the vibration isolation of the open trench in the near and far-fields through a series of in-situ tests in the field and proposes to use the amplitude reduction ratio to evaluate the vibration isolation effect of the barrier; Ahmad and Al-Hussaini (1991) study the size and location of the open and filled trench through field tests, which provide some guidelines for vibration isolation design; (Çelebi et al., 2009; Murillo et al., 2009; Ulgen and Toygar, 2015) experimentally study the effects of parameters such as load frequency, soil parameters, and barrier sizes on the vibration isolation behavior of open and filled trench under simple harmonic loads; In terms of numerical simulations, Saikia and Das (2014) analyze numerically the open trench vibration isolation problem under simple harmonic loads using the finite element Plaxis2D; Shrivastava and Rao (2002) investigate the effect of open and filled trench geometries on the isolation effect of Rayleigh waves by means of a three-dimensional finite element model. Emad and Manolis (1985) analyze the vibration isolation effect of arbitrarily shaped two-dimensional shallow trench based on the boundary element method, which finds that the shallow trench can reduce the foundation disturbance by 25% only in the medium frequency range, and trench geometry has less effect on the vibration isolation. Adam and von Estorff (2005); Andersen and Nielsen (2005) analyze the effect of trench geometry and location on the vibration isolation effect under train load by the coupled boundary element-finite element method. Herbut (2020) research on the vibration isolation effect of the open trench by finite element method from the view of reducing the vertical and horizontal components of vibration, the vibration isolation effect of the open trench on horizontal displacement is better than that on vertical displacement. Zhou et al. (2022) present a novel wave barrier (open trench-wave impedance block barrier) by considering the respective advantages of the open trench and wave impedance block. The novel wave barrier has a better isolation effect for the vibration in the low-frequency range through finite element analysis. In terms of theoretical analysis based on the theory of complex functions and conformal mapping methods, Xu et al. (2015) present a theoretical solution for single-trench for plane wave isolation and Zhou et al. (2021) give a theoretical solution for multiple-trench for plane SH wave isolation.

From the above, the research on the vibration isolation of open trench is mainly focused on the relevant analysis under different loads and different geological conditions. Artificial vibration waves consist mainly of body waves (S-wave and P-wave) and surface waves (Rayleigh wave, etc.), and near-field vibration isolation is mainly for body waves and far-field vibration isolation is mainly for surface waves. The time-domain analysis can accurately and visually describe the action of the open trench for elastic waves; However, there are few studies on the time-domain analysis of the open trench for elastic wave isolation. The scaled boundary finite element method (SBFEM) is a numerical method developed gradually in the course of simulation studies of elastic dynamics problems in infinite domains (Song, 2018; Wolf, 2003), which has the advantages of semi-analytical, high accuracy, reduced dimensional solution, and mesh flexibility. At present, the SBFEM has many applications to the problem of elastic wave scattering in half-space (Bazyar and Song, 2017; Chen et al., 2015b; Qu et al., 2021). Based on the theory of soil-structure interaction, the site with an open trench is decomposed into a near-field system and an infinite far-field system. The near field is discretized using a quadtree mesh (Man et al., 2014). The displacement unit impulse response matrix (Chen et al., 2014) with an effective time discretization approach is utilized to allow the scattering wave to propagate to infinity without reflection. A spatial approximation by sub-structuring the far field (Chen et al., 2015a; Zhang et al., 1999) and truncating the temporal local formulation of the displacement unit impulse response matrix reduces the computational time. The incident wave input with arbitrary angle is achieved by applying an equivalent nodal force at the near/far-field interface. A numerical model of SBFEM in elastic media for elastic wave propagation is established. Finally, through numerical examples to verify the effectiveness of the method of this paper, parametric analyzes the effect law of the incidence angle and the trench depth, etc., on the vibration isolation performance.

The structure of this paper is as follows. In Section 2, the basic formulation of SBFEM for the elastic wave stimulation problem is briefly described. In Section 3, the wave input formulation for the scattering wave problem is presented. In Section 4, the effectiveness of the present method is clarified and the vibration isolation effect of the open trench for elastic waves is discussed through three numerical examples, respectively. The major conclusions drawn from this study are summarized in Section 5.

2. The scaled boundary finite element method equations

The novel SBFEM is a fundamental solution-less boundary element method based on the finite element, which needs only discrete boundary and radial strict resolution, combined with the advantages of the boundary element method and finite element method. The scaled boundary finite method is a numerical method developed in infinite domain elastic dynamics, which has been successfully applied to the numerical simulation of elastic wave propagation.

The computational model of the open trench for the elastic wave vibration isolation problem using SBFEM is shown in Figure 1. The problem domain (Figure 1(a)) is decomposed into a bounded near-field system and an infinite far-field system (Figure 1(b)). The two components are linked by the interaction force R _b^∞(t) at the near/far-field intersection.

Figure 1.

Element boundary discretization in the SBFEM.

The SBFEM, unlike the FEM, first needs to discretize the circumferential boundary of the elements by numerical solution. By employing the coordinates and displacement values of the endpoints, the interpolation relationship between the coordinates and displacement of any point on the boundary can be obtained by the solution method of the one-dimensional line element in the FEM. When the line element of each boundary is solved, the nodal coordinates and displacement interpolation relations of the entire element boundary are received. Through deriving the governing equilibrium equation, the radial displacement interpolation function is solved analytically and multiplied with the circumferential boundary displacement interpolation function which yields the displacement field within the entire element.

The polygon element for modeling the near-field system using SBFEM is shown in Figure 2(a). The scale center O is established inside the polygon element, and any point on the boundary is directly visible from the scale center O to satisfy the similarity and visibility criteria of the near-field system elements. For convenience, the origin of the Cartesian coordinate system is chosen to be at the scale center. The boundaries of the polygon elements can be scaled toward the scale center to cover the entire polygon area. The scaled boundary coordinate system is defined by a radial coordinate ξ and a circumferential coordinate s. ξ runs from 0 at the scaling center to 1 on the polygon boundary for the near-field elements. For each element, s is from −1 to +1 (see Figure 2(b)).

Figure 2.

Computational model.

The representation of the far-field system in SBFEM is shown in Figure 2(b). Only the near-field/far-field interface is discretized. The center of scale is chosen to be on the extension of the straight free surface outside the far field. The free surfaces passing through the scaling center are treated as side faces and not discretized. ξ varies from 1 on the near/far-field interface to ∞ at infinity.

For 2D problems, the geometry of the isoparametric element is interpolated using the shape functions N _u(s) formulated in the local coordinate s of an element on boundary as

x (ξ, s) = ξ N_{u} (s) x_{b}

(1a)

y (ξ, s) = ξ N_{u} (s) y_{b}

(1b)

Along the radial lines passing through the scaling center and a node on the boundary, the nodal displacement functions u (ξ) are introduced. The displacements at a point(ξ,s) are interpolated from the displacement functions as

u (ξ, s) = N_{u} (s) u (ξ)

(2)

The SBFEM dynamic stiffness matrix equation for the near-field system is (Bazyar and Song, 2017; Qu et al., 2021; Wolf, 2003):

(S (ω) - E^{1}) {(E^{0})}^{- 1} (S (ω) - {(E^{1})}^{T}) + ω S {(ω)}_{, ω} - E^{2} + ω^{2} M^{0} = 0

(3)where S (ω) is the dynamic stiffness and E ⁰, E ¹, E ², and M ⁰ are the coefficient matrices of the finite element assembly elements, which are expressed in detail as follows:

E^{0} = {\int_{- 1}^{+ 1} (B^{1} (s))}^{T} D (s) B^{1} (s) | J (s) | d s

(4a)

E^{1} = {\int_{- 1}^{+ 1} (B^{2} (s))}^{T} D (s) B^{1} (s) | J (s) | d s

(4b)

E^{2} = {\int_{- 1}^{+ 1} (B^{2} (s))}^{T} D (s) B^{2} (s) | J (s) | d s

(4c)

M^{0} = {\int_{- 1}^{+ 1} (N (s))}^{T} ρ (s) N (s) | J (η) | d s

(4d)

The SBFEM dynamic stiffness matrix equation for the far-field system can be similarly expressed as (Bazyar and Song, 2017; Qu et al., 2021; Wolf, 2003):

(S^{\infty} (ω) + E^{1}) {(E^{0})}^{- 1} (S^{\infty} (ω) + {(E^{1})}^{T}) - ω S^{\infty} {(ω)}_{, ω} - E^{2} + ω^{2} M^{0} = 0

(5)

The motion equation in the time-domain for the near-field system is (Bazyar and Song, 2017; Wolf, 2003):

[\begin{array}{c} M_{s s} & M_{s b} \\ M_{b s} & M_{b b} \end{array}] {\begin{array}{c} {\ddot{u}}_{s}^{t} (t) \\ {\ddot{u}}_{b}^{t} (t) \end{array}} + [\begin{array}{c} C_{s s} & C_{s b} \\ C_{b s} & C_{b b} \end{array}] {\begin{array}{c} {\dot{u}}_{s}^{t} (t) \\ {\dot{u}}_{b}^{t} (t) \end{array}} + [\begin{array}{c} K_{s s} & K_{s b} \\ K_{b s} & K_{b b} \end{array}] {\begin{array}{c} u_{s}^{t} (t) \\ u_{b}^{t} (t) \end{array}} = {\begin{array}{c} F_{s}^{t} (t) \\ F_{b}^{t} (t) - R_{t}^{\infty} (t) \end{array}}

(6)where M , K , and C are the mass matrix, static stiffness matrix, and damping matrix of the near-field system, respectively, where the subscript s denotes the node inside the near-field domain and the subscript b denotes the node at the near/far-field intersection. u ^t(t) is the total displacement field of the node, which consists of the scattering displacement field u ^s(t) and the free displacement field u ^f(t).

u^{t} (t) = u^{f} (t) + u^{s} (t)

(7)

F^{t} (t) = F^{f} (t) + F^{s} (t)

(8)where F ^s(t) and F ^f(t) are the nodal forces caused by the scattering displacement u ^s(t) and free displacement u ^f(t) of the node, respectively, and F ^t(t) is the total nodal force.

F_{b}^{s} (t) = - \int_{0}^{t} S^{\infty} (τ) u_{b}^{s} (t - τ) d τ

(9)

Substituting equation (9) into equation (8) further yields:

\begin{array}{l} F_{b}^{t} (t) = F_{b}^{f} (t) - \int_{0}^{t} S^{\infty} (τ) u_{b}^{s} (t - τ) d τ \\ = F_{b}^{f} (t) - \int_{0}^{t} S^{\infty} (τ) u_{b}^{f} (t - τ) d τ - \int_{0}^{t} S^{\infty} (τ) u_{b}^{t} (t - τ) d τ \end{array}

(10)

The interaction forces at the near/far field intersection can be expressed as:

R_{b}^{\infty} (t) = \int_{0}^{t} S^{\infty} (τ) u_{b}^{t} (t - τ) d τ

(11)

The detailed calculation of the convolution integral with respect to time in Equations. (9) ∼ (11) is described in the ref (Bazyar and Song, 2017; Chen et al., 2015b).

3. The input method of plane elastic wave

In order not to lose generality, we only consider a plane P wave incident at an angle of incidence θ₁ into the half-space here, and the incident wave encountering a ground surface will generate a reflected wave P and a reflected SV wave (Graff, 2012), as shown in Figure 3.

Figure 3.

Plane P-wave input at the near/far-field interface.

From Figure 3, the free displacement field at observation point P can be expressed as follows (Bazyar and Song, 2017; Huang et al., 2017):

u_{x}^{f} (x, y, t) = u_{P}^{i n} (x, y, t) \sin θ_{1} + \frac{A_{2}}{A_{1}} u_{P}^{r e} (x, y, t) \sin θ_{1} + \frac{B_{2}}{A_{1}} \frac{c_{P}}{c_{S}} u_{S V}^{r e} (x, y, t) \cos θ_{2}

(12a)

u_{y}^{f} (x, y, t) = u_{P}^{i n} (x, y, t) \cos θ_{1} - \frac{A_{2}}{A_{1}} u_{P}^{r e} (x, y, t) \cos θ_{1} + \frac{B_{2}}{A_{1}} \frac{c_{P}}{c_{S}} u_{S V}^{r e} (x, y, t) \sin θ_{2}

(12b)where u_Pⁱⁿ(x,y,t), u_P^re(x,y,t), and u_sv^re(x,y,t) are the displacement components of incident P, reflected P, and reflected SV waves at observation point P, respectively;

\frac{A_{2}}{A_{1}}

and

\frac{B_{2}}{A_{1}}

are the relative displacement amplitudes of reflected P and reflected SV waves; and c_P and c_S are the wave velocities of P and SV waves, respectively.

\frac{A_{2}}{A_{1}} = \frac{\sin 2 θ_{1} \sin 2 θ_{2} - k^{2} \cos^{2} 2 θ_{2}}{\sin 2 θ_{1} \sin 2 θ_{2} + k^{2} \cos^{2} 2 θ_{2}}

(13a)

\frac{B_{2}}{A_{1}} = \frac{\sin 2 θ_{1} \cos 2 θ_{2}}{\sin 2 θ_{1} \sin 2 θ_{2} + k^{2} \cos^{2} 2 θ_{2}}

(13b)

k = \frac{\sin θ_{1}}{\sin θ_{2}} = \frac{c_{P}}{c_{S}} = 2 {(\frac{2 (1 - ν)}{1 - 2 ν})}^{1 / 2}

(13c)

θ_{2} = \arcsin (\frac{\sin θ_{1}}{k})

(13d)

Assuming that the wavefront of the incident plane P wave reaches the point C at the time t=0, the displacement components u_Pⁱⁿ(x,y,t), u_P^re(x,y,t), and u_sv^re(x,y,t) of the incident P wave, reflected P wave, and reflected SV wave at the observation point P can be expressed as an excitation function with respect to the time response g(t):

u_{P}^{i n} (x, y, t) = g (t - Δ t_{1})

(14a)

u_{P}^{r e} (x, y, t) = g (t - Δ t_{2})

(14b)

u_{S V}^{r e} (x, y, t) = g (t - Δ t_{3})

(14c)where Δt represents the delayed response time of the incident or reflected wave arriving at point P.

Δ t_{1} = \frac{(x - x_{0}) \sin θ_{1} + (y - y_{0}) \cos θ_{1}}{c_{P}}

(15a)

Δ t_{2} = Δ t_{1} + \frac{2 (R - y - y_{0}) \cos θ_{1}}{c_{P}}

(15b)

Δ t_{3} = Δ t_{1} + \frac{\cos (θ_{1} + θ_{2})}{c_{S V} \cos θ_{2}} (R - y - y_{0}) + \frac{R - y - y_{0}}{c_{P} \cos θ_{2}}

(15c)

The stress–displacement relationship can be derived from Hooke’s law and geometric equation in elastic mechanics.

{\begin{array}{c} σ_{x} \\ σ_{y} \\ τ_{x y} \end{array}} = \frac{E}{1 + ν} [\begin{array}{c} \frac{1 - ν}{1 - 2 ν} & \frac{1 - ν}{1 - 2 ν} & 0 \\ \frac{1 - ν}{1 - 2 ν} & \frac{1 - ν}{1 - 2 ν} & 0 \\ 0 & 0 & \frac{1 - ν}{1 - 2 ν} \end{array}] [\begin{array}{c} \frac{\partial}{\partial x} & 0 \\ 0 & \frac{\partial}{\partial y} \\ \frac{\partial}{\partial y} & \frac{\partial}{\partial x} \end{array}] {\begin{array}{c} u_{x} \\ u_{y} \end{array}}

(16)

The equivalent nodal forces resulting from the free-field motion can be determined from the shape function and the unit surface traction (Bazyar and Song, 2017; Huang et al., 2017; Qu et al., 2021).

F_{b}^{f} (t) = \int N^{T} t_{b}^{f} d s

(17a)

t_{b}^{f} = σ^{f} \cdot n

(17b)

σ^{f} = [\begin{array}{c} σ_{x}^{f} & τ_{x y}^{f} \\ τ_{x y}^{f} & σ_{y}^{f} \end{array}]

(17c)

n = [\begin{array}{c} n_{x} \\ n_{y} \end{array}]

(17d)where N , t _b^f, ds, σ ^f, and n are shape function of each boundary element, surface traction, element surface, stress tensor, and outward normal vector at each node on the near/far-field interface, respectively.

4. Numerical examples

The problem of the input of a plane P-wave in the half-space is realized by the SBFEM, and the detailed calculation steps are described in the ref (Bazyar and Song, 2017). Three numerical examples are presented in this section, the first one investigates the motion displacement of the incident plane P-wave in the free-field (without the open trench) to facilitate comparison with the analytical solution of the ref (Graff, 2012), which for verifying the results of the numerical simulation of elastic wave propagation are the same as the analytical solution. The second numerical calculation takes the scattering of elastic waves by a semi-circular canyon as an example to verify the accuracy of SBFEM in the elastic wave scattering problem. The last example considers the scattering of elastic waves by open trench (trench width is w and trench depth is h) for analyzing the vibration isolation effect of the trench on elastic waves.

4.1. Example 1

The near-field region is intercepted as a rectangle with a width of 100 m and a depth of 50 m. The grid division of the free field is shown in Figure 4, where the maximum element grid size is less than 0.625 m. This region can ensure that the incidence and reflection processes of elastic waves are observed. It is assumed that the half-space is a homogeneous isotropic elastic medium with material properties as shown in Table 1.

Figure 4.

Meshing of the free-field using quadtree.

Table 1.

Material properties of the elastic half-space.

Young’s modulus E	Mass density ρ	Poisson’s ratio ν	SV-wave velocity c_S	P-wave velocity c_P
MPa	kg/m³	—	m/s	m/s
58.08	2600	0.32	92	120

Considering the time response g(t) as a Ricker wavelet for the input of the plane P-wave.

g (t) = A_{\max} [1 - 2 {(π f (t - t_{0}))}^{2}] \exp (- {(π f (t - t_{0}))}^{2})

(18)where A_max=0.001m, f=5.0Hz, and t₀=0.5s are the maximum magnitude of the time history, the main frequency of the Fourier spectrum, and the time when the displacement reaches its peak, respectively. The wavelength of the main shear wave is λ_f =18.4m meeting 0.625m<λ_f /10, which ensures the stability of numerical calculation. The features of the function g(t) are shown in Figure 5.

Figure 5.

Excitation features of Ricker wavelet.

Taking the incidence angle θ₁=30^°, the horizontal and vertical displacement clouds in the free field under plane P-wave incidence are shown in Figure 6. It is obvious in Figure 6 that the incident angle of the plane P-wave is 30°, and the reflected P-wave and reflected SV-wave are generated when the incident wave encounters the surface boundary, and the measured values of the reflected P-wave and reflected SV-wave reflection angles are 30° and 22.5°, respectively, which are consistent with the calculated results of equation (13d). It shows that this method can effectively simulate the propagation of P-wave in the half-space.

Figure 6.

Displacement clouds in the free field under the plane P-wave incidence.

Table 2.

Material properties of half-space with semi-circular canyon.

Young’s modulus E	Mass density ρ	Poisson’s ratio ν	SV-wave velocity c_S	P-wave velocity c_P
MPa	kg/m³	—	m/s	m/s
25,000	2600	1/3	1923.1	3597.7

To further verify the reliability of the proposed calculation results, the time response of horizontal and vertical displacements at observation points A, B, and C (see Figure 3(a)) are plotted from Figure 7 and compared with the analytical solution(Graff, 2012). The result of this paper agrees very well with the result of ref (Graff, 2012) as can be found in Figure 7, which fully illustrates that the method of this paper can not only effectively simulate the propagation of P-wave in half- plane, but also has a very reliable calculation accuracy.

Figure 7.

Displacement responses at observation point A, B, and C in the free-field.

4.2. Example 2

As further verification of the accuracy of the SBFEM in modeling the elastic propagation problem in this paper, the scattering of elastic waves by semi-circular canyons with plane P-wave incidence are analyzed in this example. Considering the equation (18) as a Ricker wavelet for the input of the plane P-wave, where, A_max=0.001m, f =9.6Hz, t₀=0.5s, and λ_f=200m. The near-field area is intercepted as a rectangle and its width is 400 m, depth is 200 m, the radius of the semi-circular canyons is R = 50 m, and the quadtree mesh discretization of the semi-circular canyons as shown in Figure 8, the maximum element grid size is less than 10m<λ_f /10, which ensures the stability of numerical calculation. For a better comparison with the results of BEM (Wong, 1982), the dimensionless frequency is taken as Ω=2πfR/c_s=0.5, where c_s is the main shear wave velocity. The material properties of the semi-plane with semi-circular canyon are listed in Table 2. The frequency domain response obtained by the Fourier transform of the displacement time history is plotted in Figure 9, which shows the amplification of horizontal and vertical displacements of the ground surface caused by a plane P-wave (incidence angle of 30°), where the solid line is the SBFEM result and the circle is the BEM result (Wong, 1982). From Figure 9, the SBFEM results are basically in agreement with the BEM results, which illustrates the accuracy and reliability of the SBFEM in modeling the elastic propagation problem.

Figure 8.

Meshing of the near-field with the semi-circular canyons using quadtree.

Figure 9.

Displacement amplification of ground motion of semi-circular canyon.

4.3. Example 3

4.3.1. Scattering of elastic waves by the open trench

Assume that the half-space is a homogeneous, isotropic elastic medium with the material properties shown in Table 1. Taking the equation (18) as a Ricker wavelet for the input of the plane P-wave, where, A_max=0.001m, f =0.5Hz, t₀=0.5s, and λ_f =18.4m. The near-field region is intercepted as a rectangle with its width of 100 m and depth of 50 m to allow observation of the process of the action of the trench on the elastic wave. Considering the open trench width w = 1 and depth h = 8, the quadtree mesh of the near-field region is divided as shown in Figure 10, where the maximum element grid size is less than 0.625m<λ_f /10. The horizontal and vertical displacement response clouds are shown in Figure 11 at different times for incidence angles θ₁=0^° and θ₁=60^°, respectively. The scattered waves are generated when the elastic wave encounters the boundary of the open trench. As shown in Figure 11(a), there is only vertical displacement in the half-space (t = 0.55s) under the vertical incidence of the plane P-wave (θ₁=0^°). The horizontal displacement is generated in the half-space when the plane P-wave propagates further and encounters the open trench (t = 0.80s), and the vertical displacement near the open trench is obviously amplified. Therefore, it is difficult for the open trench to play a vibration isolation role when the plane P-wave is incident vertically to the surface. When the incidence angle is θ₁=60^° (see Figure 11(b)), the trench has an obvious barrier phenomenon for the elastic wave propagation, the displacement on the front side of the trench is amplified (t = 0.80s), and correspondingly the displacement on the back side is weakened (t = 0.90s). This phenomenon is more obvious with the increase of the incident angle, and it can also be found that the barrier effect of the trench on the horizontal displacement is obvious than that on the vertical displacement. The larger the angle of incidence, the better the vibration isolation effect of the trench.

Figure 10.

Meshing of the near-field with the open trench using quadtree.

Figure 11.

Displacement clouds of a field with an open trench under the plane P-wave incidence.

4.3.2. Evaluation of vibration isolation effect

We normalized the parameters to the trench width considering that the trench width has a small effect on the vibration isolation performance (Woods, 1968). In order to evaluate the vibration isolation effect of the open trench for plane P-wave, the maximum displacement response attenuation ratio u_i/u_i0 (i = x, the horizontal displacement; i = y, the vertical displacement) is introduced, u_i is the displacement after setting the barrier, and u_i0 is the displacement of the free-field before setting the barrier. It can be found that the smaller the value of u_i/u_i0, the better the vibration isolation effect.

In order to analyze the effect of incident angle on vibration isolation performance, the variation law of u_i/u_i0 with x/w for different values of h/w is shown in Figure 12. When the incident angle θ₁=0^°, which means the incident wave is perpendicular to the ground surface, the open trench has no vibration isolation effect for both horizontal and vertical displacements, and the displacement in the area near the trench boundary is amplified, especially the horizontal displacement is magnified infinitely. As the incidence angle is larger, we find that the vibration isolation effect of the open trench for horizontal displacement is significantly better than that for vertical displacement, and for horizontal displacement, the best vibration isolation area is near the back side of the open trench, and for vertical displacement, the vertical displacement is amplified in a certain range near the back side of the open trench, but as x/w continues to increase there are vibration isolation areas appear. For different values of h/w, with the increase of the incident angle, the vibration isolation area increases and the u_i/u_i0 value in the isolation area decreases significantly, which means that the open trench provides better vibration isolation for the incident wave with larger incident angle.

Figure 12.

Effect of incidence angle on the vibration isolation performance of the open trench.

In order to further analyze the effect of the trench depth on the vibration isolation performance, the effect of the trench depth on the vibration isolation performance for different values of θ₁ is shown in Figure 13. It can be seen from Figure 13 that the effect of depth on the area size of vibration isolation is small, while the effect on the u_i/u_i0 in the vibration isolation area is very obvious, and the u_i/u_i0 decreases significantly with the increase of the depth h/w. For a certain value of θ₁, the appearance of the best isolation region for vertical displacement is almost independent of the depth h/w (θ₁=30^°, the best isolation region appears at x/w = 15; θ₁=60^°, the best isolation region appears at x/w = 20; and θ₁=85^°, the best isolation region appears at x/w = 20). In addition, the displacement amplification effect in front of the trench increases with depth h/w the more obvious it is. Therefore, we should consider both the vibration isolation area and vibration isolation efficiency in the actual vibration isolation project, choose a reasonable location to excavate the open trench according to the vibration isolation area, and choose a reasonable excavation depth according to the vibration isolation efficiency in order to achieve vibration isolation requirements under economic conditions.

Figure 13.

Effect of depth on the vibration isolation performance of the open trench.

5. Conclusions

In this paper, the SBFEM is established for the time-domain analysis of the elastic wave scattering from the open trench. The quadtree domain decomposition technique is employed for SBFEM discretization of the near-field. The far-field is rigorously modeled by the displacement unit impulse response matrix. The obliquely plane elastic wave from the far-field is converted into a traction force acting on the near/far-field boundary. The effect of the open trench for the isolation of elastic waves is analyzed with the example of plane P-wave incidence. Numerical examples show that:

(1) The vibration isolation effect of the open trench for horizontal displacement is better than that for vertical displacement.

(2) As the incidence angle increases, the better the vibration isolation effect of the open trench; and when the incidence angle is larger, by further increasing the trench depth, which will make the trench has a better vibration isolation effect.

(3) The location of the horizontal displacement vibration isolation and vertical displacement vibration isolation areas are different, so we should pay attention to the excavation location of the trench when near-field vibration isolation. With the increase of depth, the displacement amplification phenomenon near the front side of the trench is more obvious. Therefore, we should consider both the vibration isolation area and vibration isolation efficiency in the actual vibration isolation project, choose a reasonable location to excavate the open trench according to the vibration isolation area, and choose a reasonable excavation depth according to the vibration isolation efficiency in order to achieve vibration isolation requirements under economic conditions.

Footnotes

Acknowledgments

The authors are grateful to Professor Chongmin Song and Dr. Yanlin Qu from the School of Civil and Environmental Engineering, University of New South Wales, Australia, for their guidance on the work of this paper. We are also grateful to the editors and reviewers for their valuable and constructive comments on this paper.

Declaration of conflicting interests

The author(s) declared no potential conflicts of interest with respect to the research, authorship, and/or publication of this article.

Funding

The author(s) disclosed receipt of the following financial support for the research, authorship, and/or publication of this article: This work was supported by the Chinese Natural Science Foundation (Grant No. 51978320, Grant No. 11962016) and the Funds for Creative Research Groups of Gansu Province of China [20JR5RA478].

ORCID iD

Fengxi Zhou

References

Adam

von Estorff

(2005) Reduction of train-induced building vibrations by using open and filled trenches. Computers and Structures 83: 11–24.

Ahmad

Al-Hussaini

(1991) Simplified design for vibration screening by open and in-filled trenches. Journal of geotechnical engineering 117: 67–88.

Andersen

Nielsen

(2005) Reduction of ground vibration employing barriers or soil improvement along a railway track. Soil Dynamics and Earthquake Engineering 25: 701–716.

Bazyar

Song

(2017) Analysis of transient wave scattering and its applications to site response analysis using the scaled boundary finite-element method. Soil Dynamics and Earthquake Engineering 98: 191–205.

Beskos

Dasgupta

Vardoulakis

(1986) Vibration isolation using open or filled trenches - Part 1 : 2-D homogeneous soil. Computational Mechanics 1: 43–63.

Çelebi

Fırat

Beyhan

, et al. (2009) Field experiments on wave propagation and vibration isolation by using wave barriers. Soil Dynamics and Earthquake Engineering 29: 824–833.

Chen

Birk

Song

(2014) Numerical modelling of wave propagation in anisotropic soil using a displacement unit-impulse-response-based formulation of the scaled boundary finite element method. Soil Dynamics and Earthquake Engineering 65: 243–255.

Chen

Birk

Song

(2015a) Time-domain analysis of wave propagation in 3-D unbounded domains by the scaled boundary finite element method. Soil Dynamics and Earthquake Engineering 75: 171–182.

Chen

Birk

Song

(2015b) Transient analysis of wave propagation in layered soil by using the scaled boundary finite element method. Computers and Geotechnics 63: 1–12.

10.

Emad

Manolis

(1985) Shallow trenches and propagation of surface waves. Journal of Engineering Mechanics 111: 279–282.

11.

Gao

Chen

, et al. (2017) Numerical study on the active vibration isolation by wave impeding block in saturated soils under vertical loading. Soil Dynamics and Earthquake Engineering 93: 99–112.

12.

Gao

Qiu

, et al. (2006) Three-dimensional analysis of rows of piles as passive barriers for ground vibration isolation. Soil Dynamics and Earthquake Engineering 26: 1015–1027.

13.

Graff

(2012) Wave Motion in Elastic Solids. Courier Corporation.

14.

Herbut

(2020) Vibration mitigation efficiency of an inclined, curved, open trench. PLoS One 15: e0229010.

15.

Huang

Zhao

(2017) Non-linear seismic responses of tunnels within normal fault ground under obliquely incident P waves. Tunnelling and Underground Space Technology 61: 26–39.

16.

Kattis

Polyzos

Beskosu

(1999) Modelling of pile wave barriers by effective trenches and their screening effectiveness. Soil Dynamics and Earthquake Engineering 18: 1–10.

17.

Zhou

Zhang

(2019) Vibration isolation of saturated foundations by functionally graded wave impeding block under a moving load. Journal of the Brazilian Society of Mechanical Sciences and Engineering 41: 1–10.

18.

Man

Song

Natarajan

, et al. (2014) Towards automatic stress analysis using scaled boundary finite element method with quadtree mesh of high-order elements. arXiv preprint arXiv:1402.5186 .

19.

Murillo

Thorel

Caicedo

(2009) Ground vibration isolation with geofoam barriers: centrifuge modeling. Geotextiles and Geomembranes 27: 423–434.

20.

Chen

Liu

, et al. (2021) A direct time-domain procedure for the seismic analysis of dam–foundation–reservoir systems using the scaled boundary finite element method. Computers and Geotechnics 138: 104364.

21.

Saikia

Das

(2014) Analysis and design of open trench barriers in screening steady-state surface vibrations. Earthquake Engineering and Engineering Vibration 13: 545–554.

22.

Shrivastava

Rao

(2002) Response of soil media due to impulse loads and isolation using trenches. Soil Dynamics and Earthquake Engineering (1984) 22: 695–702.

23.

Song

(2018) The Scaled Boundary Finite Element Method. Hoboken: John Wiley & Sons Ltd.

24.

Ulgen

Toygar

(2015) Screening effectiveness of open and in-filled wave barriers: a full-scale experimental study. Construction and Building Materials 86: 12–20.

25.

Wolf

(2003) The Scaled Boundary Finite Element Method. John Wiley & Sons.

26.

Wong

(1982) Effect of surface topography on the diffraction of P, SV, and Rayleigh waves. Bulletin of the Seismological Society of America 72: 1167–1183.

27.

Woods

(1968) Screening of surface wave in soils. Journal of the Soil Mechanics and Foundations Division 94: 951–980.

28.

Shi

Guo

(2015) Theoretical analysis of isolation effects of an open trench on incident SH waves. Chinese Journal of Underground Space and Engineering 11: 647–651.

29.

Zhang

Wegner

Haddow

(1999) Three-dimensional dynamic soil–structure interaction analysis in the time domain. Earthquake engineering & structural dynamics 28: 1501–1524.

30.

Zhou

Liang

Liu

(2021) Analysis of elastic wave scattering and vibration isolation performance of multiple open trenches: SH incident. Journal of Vibration and Shock 40: 263–268.

31.

Zhou

(2022) Study on the vibration isolation performance of an open trench-wave impedance block barrier using perfectly matched layer boundaries. Journal of Vibration and Control 28: 329–338.

Time-domain analysis for the scattering of plane elastic waves in half-space with an open trench

Abstract

Keywords

1. Introduction

2. The scaled boundary finite element method equations

3. The input method of plane elastic wave

4. Numerical examples

4.1. Example 1

4.2. Example 2

4.3. Example 3

4.3.1. Scattering of elastic waves by the open trench

4.3.2. Evaluation of vibration isolation effect

5. Conclusions

Footnotes

Acknowledgments

Declaration of conflicting interests

Funding

ORCID iD

References