Abstract
Purpose
The study aims to analyze the free vibration behavior of functionally graded porous beams with non-uniform rectangular cross-sections, investigating four distinct porosity distribution across the beam's thickness.
Methods
Utilizing the Euler–Bernoulli beam model and Hamilton’s principle, the equation of motion is derived. Four different boundary conditions (clamped–clamped, clamped-free, clamped–pinned, and pinned–pinned) are considered, and the resulting equation is solved using the differential transform method. Verification of accuracy is ensured through comparison with solutions for natural frequencies found in existing literature.
Results and Conclusion
The study provides validated natural frequency solutions for functionally graded porous beams with non-uniform rectangular cross-sections, confirming the accuracy of the proposed method through literature comparison. A comprehensive parametric study reveals significant insights into the influence of various factors on natural frequencies, including porosity volume fractions, types of porosity distribution, taper ratios, and boundary conditions. These findings deepen our understanding of free vibration analysis for functionally graded porous beams, offering valuable guidance for engineering design and structural optimization in relevant applications.
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Introduction
The concept of functionally graded materials (FGMs) originated in the field of engineering, where materials with continuously varying composition or microstructure were developed to optimize their mechanical, thermal, electrical and other properties. Functionally graded porous materials (FGPMs), such as metal foams, take this idea further by incorporating porosity as an additional design parameter.
FGPMs offer a series of advantages over homogeneous materials or composite materials with a layered structure. The void spaces created by the pores reduce the material’s density, resulting in a lighter structure. This characteristic is particularly worthwhile in industries such as aerospace and automotive, where weight reduction is a critical factor. Moreover, by controlling the distribution of porosity, it is possible to achieve specific combinations of properties, such as mechanical strength, thermal conductivity, or fluid permeability, within a single material [1]. In addition, the spatial variation of properties allows FGPMs to avoid discontinuities in temperature and stress distributions as a result delamination issues inherent to simple layered configurations, e.g., in Refs. [2,3,4,5] to name a few, can be eliminated [6].
On the other hand, the manufacturing methods employed in the production of FGM beams and panels inevitably result in the formation of pores within the material volume [7]. The presence of pores can introduce certain challenges and drawbacks to the FGM. One significant concern is the potential compromise in structural integrity. Pores weaken the material and reduce its load-bearing capacity, making it more susceptible to failure under stress or external forces. Moreover, pores affect the elastic and mechanical properties of the material changing structural responses of the FGM beams and panels. As a result, research focused on studying the mechanical behavior and dynamic characteristics of FGM structures with porosity is of great significance. Herewith, the accurate prediction of natural frequencies is crucial for vibration control of such objects.
The literature search revealed an extensive studies discussing the dynamic behavior of FGM beams and panels with and without porosities. Vibrations in perfect FGM beams, plates, and shells have been examined using classical and various shear deformation theories [8, 9]. Those analyses involved equivalent single-layer (ESL) models [10, 11], layer-wise (LW) descriptions [12, 13], and the three-dimensional approach [14,15,16]. Different methodologies have been employed, ranging from analytical techniques to numerical simulations, e.g., in Refs. [17,18,19,20,21] among the latest. However, it is crucial to investigate the influence of porosity since it serves as a vital parameter in the design of modern structures.
Inspired by recent advancements in FG porous engineering materials, a significant number of researchers have undertaken studies on the dynamics of FGP beams [22,23,24,25,26], and plates and shells [27,28,29]. In these studies, while analyzing the vibration response of FG porous structures, the analysts have made adjustments to the aforementioned theories and methodologies, originally developed for ideal FGM beams, plates, and shells in order to incorporate graded porosities. Those porosities can exhibit uniform or non-uniform symmetric/non-symmetric distributions throughout the thickness of the structures.
Inhomogeneous structures with variable cross-sections are extensively utilized in diverse engineering applications, including helicopter rotor blades, wind turbines, ship propellers, and space and marine structures. These structures are favored for their ability to meet specific architectural requirements while achieving optimized weight and strength distribution. A variety of methods have been employed to solve the differential equations of motion for variable thickness FGM beams. In Ref. [30], the authors employed the dynamic stiffness method to analyze the dynamics of homogeneous tapered Euler–Bernoulli beams. In addition, in Ref. [31], the free vibrations of axially functionally graded (AFG) tapered Euler–Bernoulli beams were studied using the differential transformation and differential quadrature methods. The natural frequencies of the AFG Euler–Bernoulli beam with non-uniform cross-section were also investigated in Ref. [32] through the differential transformation method (DTM). Furthermore, the spline finite point method was utilized in Ref.[33] for the analysis of free transverse vibration of AFG tapered Euler–Bernoulli beams. The authors in Ref. [34] employed the asymptotic development method to study the free vibration of non-uniform AFG Euler–Bernoulli beams. A new hybrid approach based on the combination of the power series expansions and the Rayleigh–Ritz method for stability and free vibration analyses of AFG non-uniform beams supported by a constant Winkler–Pasternak elastic foundation was presented in Ref. [35]. A precise solution for free vibration of FG beams with variable cross-section resting on a Pasternak foundation was proposed in Ref. [36] using the separate variable method and Laplace transform within the framework of 2-D elastic theory. Furthermore, the vibrational characteristics of AFG tapered beams based on both Euler–Bernoulli and Timoshenko theories were analyzed in Ref. [37] utilizing the variational iteration method. In Ref. [38], the weighted residual collocation method with exact solution shape functions for the uniform beam as trial functions was employed to investigate the free transverse vibrations of variable cross-section cantilever FG beams with nonlinear profiles. In addition, the dynamic characteristics of an internal flexible FGM Euler–Bernoulli tapered microbeam were studied in Ref. [39] based on the modified couple stress theory.
The literature search revealed that there is a limited number of research regarding the vibration response of non-uniform cross-section FG porous beams, in comparison to the extensive studies available on vibrations of constant thickness porous beams. For instance, in Ref. [40], the authors have investigated the free vibration characteristics of a rotating double-tapered FG porous beam using the DTM. However, their analysis primarily focused on specific boundary conditions, tapering profiles, and porosity levels, leaving space for further exploration in this field. In the other work of the same authors [41], the DTM has been employed to examine the thermo-mechanical vibration behavior of non-uniform FG porous Euler–Bernoulli beams under a variety of thermal loadings. Furthermore, in Ref. [42], a finite-element dynamic analysis was conducted to examine the response of non-uniform FG porous beams subjected to multiple moving forces, employing the Timoshenko beam theory. In addition, in Ref. [43], the authors investigated the free vibration behavior of rotating FGM beams, including porosities with even or uneven distributions, using a modified variational method. The method utilized the Chebyshev series expansion and incorporated the fully geometrically nonlinear beam theory with Coriolis effect. In Refs. [44, 45], a novel approach based on spatial state equations and the associated state transition matrix has been proposed to compute the natural frequencies and mode shapes of Euler–Bernoulli and Timoshenko beams with arbitrary variations in material and geometrical properties, as well as discontinuities within the beams. Recently, in Refs. [46, 47], the discrete singular convolution method has been utilized to analyze the dynamic characteristics and buckling of non-uniform, multi-span, functionally graded graphene foam-reinforced beams under elastic boundary conditions.
This paper focuses on the free vibration analysis of non-uniform rectangular cross-section porous FG beams with four different porosity distributions. These porosity distributions, namely even and uneven with symmetric and non-symmetric profiles, are assumed to vary through the beam’s thickness direction based on the modified Gibson–Ashby model [48]. The vibration response is analyzed using the Euler–Bernoulli beam theory. The equation of motion and natural boundary conditions are derived using Hamilton’s principle. These equations in conjunction with four different beam edges’ constraints such as pinned–pinned (P–P), clamped–clamped (C–C), clamped–pinned (C–P) and clamped-free (C-F) are solved using a semi-analytical DTM approach. Semi-analytical solutions of the natural frequencies are compared with existing results in the literature to validate the proposed technique and to ensure the accuracy and reliability of the approach. In addition, for the first time, a comprehensive parametric study is conducted to examine the influence of porosity volume fractions, types of porosity distribution, taper ratios, and boundary conditions on the natural frequencies of FG porous beams. The obtained results can serve as valuable references for validating other approaches and approximate methods, as well as providing insights to enhance the dynamic performance of FG porous beams.
Non-uniform FGP Beams
An FG porous beam with variable rectangular cross-section is schematically illustrated in Fig. 1. The beam has a length L and its cross-section parameters are width b and thickness h. The axis x indicates the beam length direction, while the axes y and z denote the directions of the beam’s width and thickness, respectively.
The cross-section variations are assumed to exhibit symmetry about the mid-line \((z=0)\) of the beam. The width and thickness of the beam as functions of x can be written as
where \(c_b = 1 - \frac{b_1}{b_0}\) and \(c_h = 1 - \frac{h_1}{h_0}\) are the width and height taper ratios, respectively. It is worth to mention that if \(c_b = c_h= 0\), the beam would be uniform; if \(c_b \ne 0\) and \(c_h= 0\), the beam would be tapered with width but has a constant height; if \(c_b= 0\) and \(c_h \ne 0\), the beam would be tapered with height but has a constant width; and if \(c_b \ne 0\) and \(c_h \ne 0\), the beam would be double tapered. The power coefficients m and n allow for accounting for arbitrary variation of the geometrical parameters along the beam’s length. Herewith, the rectangular cross-sectional area A(x) and the second moment of inertia I(x) vary along the beam’s length as follows:
where \(A_0\) and \(I_0\) represent the area and second moment of inertia of the rectangular cross-section at \(x=0\), respectively.
Porosity changes the material properties of the beam, specifically, Young’s modulus E and mass density \(\rho\). This is similar to material profiles observed in perfect functionally graded materials. Here, we assume that the material properties vary continuously across the beam thickness, that is, they are functions of z. Four types of porosity distribution profiles such as even (type I) and uneven symmetric with stiffer layers in surface areas (type II), symmetric with a stiffer layer in the central area (type III), and non-symmetric (type IV) are considered, as shown in Fig. 2. These porosity distributions along the height h of the beam’s cross-section at a given position on the x-axis can be defined as follows [23]:
for type I profile, in which \(\alpha =\frac{1}{e_0} - \frac{1}{e_0} \left( \frac{2}{\pi } \sqrt{1 - e_0} - \frac{2}{\pi } + 1 \right) ^2\),
for type II profile,
for type III profile, and
for type IV profile.
In (3)–(6), we denote \(e_0= 1 - E_1/E_0\) , \((0<e_0<1)\) and \(e_m = 1- \rho _1/\rho _0\), \((0<e_m<1)\), where \(E_1\) and \(E_0\) are minimum and maximum values of Young’s modulus, respectively, and also \(\rho _1\) and \(\rho _0\) are minimum and maximum values of mass density, respectively. Moreover, in the case of open-cell porous materials [48], the relationship between \(e_0\) and \(e_m\) can be expressed in the form \(e_m= 1 - \sqrt{1 - e_0}\).
It should be mentioned that the Poisson’s ratio \(\nu\) is assumed constant for all the types of porosity distributions.
Governing Equation of Motion
The inhomogeneous beam of length L is characterized by material properties that continuously vary in the through-thickness direction z, while the rectangular cross-section of the beam varies along the axial coordinate x. Transverse vibration of the beam takes place in the xz-plane. Let us consider the Euler–Bernoulli theory, which takes into account only the transverse displacement \(\tilde{w}(x,z,t)\) and the curvature of the mid-line. Then, the displacements along the x- and z-axes are expressed in the form:
Based on the displacement field (7), only the normal strain component occurs as
The corresponding normal stress can be obtained using one-dimensional Hooke’s law as
Within this assumption, the strain and kinetic energies are defined, accordingly, as follows:
Herein, appropriate stiffness and inertia coefficients in (10) are computed, respectively, as
Using Hamilton’s principle \(\delta \Pi = \delta \{ \int _{t_1}^{t_2} \left( U - K \right) dt \} =0\) with the virtual strain \((\delta U)\) and kinetic \((\delta K)\) energies, we can write the governing equation of motion of the FGP beam as
with natural boundary conditions and an initial condition as follows:
For harmonic vibration with frequency \(\omega\), the dynamic displacement field is defined by
Substituting (14) into (12), it gives us an ordinary differential equation describing free transverse vibration of a non-uniform cross-section FG porous beam:
Herewith, the stiffness \(D_{11}(x)\) and inertia m(x) coefficients can be expressed in the form:
where the averaged Young’s modulus \(E_z (x)\) and mass density \(\rho _z (x)\) are computed by analytical integration of (11) over the rectangular domain A(x) for each type of porosity profile (3)–(6). The explicit forms of these expressions can be found in Appendix A.
Differential Transform Method
From a mathematical perspective, integrating Eq. (15) presents complexity due to variable coefficients arising from coordinate-dependent material properties and cross-sections. As a result, closed-form solutions are feasible only for specific cross-sectional shapes, porosity profiles, and boundary conditions. In this context, numerical methods like the finite-element method (FEM) are more effective, as they offer the necessary versatility to explore various geometric configurations and material characteristics However, the differential transform method can also be effectively employed for this purpose. In contrast to the traditional FEM, the DTM stands out for its accessibility, simplicity, and avoidance of finite-element meshes. As a semi-analytical method, it is inherently symbolic and eliminates the need for auxiliary parameters, assumed functions, or specific initial/boundary conditions when seeking the solution, unlike the approximations used in FEM. In addition, the DTM provides a series expansion solution for differential equations, enabling deeper insights into the system’s behavior, whereas the FEM typically delivers numerical solutions without analytical expressions.
The DTM was initially introduced by G. E. Pukhov in 1978 [49], and the fundamental aspects of this method can be found in his original publications [50,51,52]. A recent comprehensive discussion on the status of the DTM, including its basics, drawbacks and limitations has been presented in Refs. [53, 54] and the references therein. An investigation into the convergence issues associated with DTM solutions has been reported in Refs. [32, 55]. Researchers, e.g., [56,57,58], have also explored innovative strategies to mitigate the limitations, combining the DTM with other techniques that provide accurate results in regions where the series solution may not suffice.
Besides the variety of the tasks to which the DTM can be applied, its accuracy and simplicity in calculating the natural frequencies makes it superior among many other semi-analytical methods mentioned in Introduction. The application of the DTM to address the free vibration problem of non-uniform inhomogeneous beams is reported in Refs. [31, 32, 40, 41] to name a few.
Following Ref. [32], we reformulate (15) in a form more suitable for its application in addressing the vibration problem using the DTM
where the variable coefficients will be denoted as \(\bar{D}_1(x)=2D_{11}'(x)/D_{11}(x)\), \(\bar{D}_2(x)=D_{11}''(x)/D_{11}(x)\) and \(\bar{M}(x)=m(x)/D_{11}(x)\). Here, and in what follows, the prime denotes a derivative with respect to the x-coordinate.
It’s worth noting that the variable coefficients in (17) account for changes in both thickness and length directions. As a result, they exhibit a more complex structure in terms of the variable x, compared to the coefficients associated with functionally graded material properties that vary solely in the axial direction [30,31,32]. This complexity significantly slows down the computation and convergence rate of the DTM. To overcome this issue, the division operation in the domain of differential transformations is employed for the coefficients \(\bar{D}_1(x)\), \(\bar{D}_2(x)\) and \(\bar{M}(x)\) before computing their appropriate images (discretes) [52].
Thus, by utilizing the domain of differential transformation, the solution of equation (17) at a certain point \(x_0\) of the interval \(0\le x \le L\) can be represented as a set of recurrent algebraic equations [32]:
where W(k), and \(D_1(k)\), \(D_2(k)\) and M(k) are the images of the unknown amplitude \(\bar{w}(x)\) and the given functions \(\bar{D}_1(x)\), \(\bar{D}_2(x)\) and \(\bar{M}(x)\), respectively.
It is obvious that each recurrent equation in the system 18 is derived by sequentially varying the index k. However, the images W(0), W(1), W(2), and W(3) are not directly obtained from 18 as observed. Therefore, we can simplify this expression to the following form:
where the explicit forms of the recurrent coefficients in (19) can be found in Ref. [32].
Once the spectrum W(k) for chosen number of images is obtained, the original function \(\bar{w}(x)\) is reconstructed as
Given that the images W(k) at \(k\geqslant 4\) depends on W(0) , W(1) , W(2) and W(3) , Eq. (20) takes the form:
By satisfying boundary conditions imposed on the beam ends in terms of transverse displacement \(\bar{w}\), rotation angle \(\theta\), bending moment M and shear force Q, such that
we arrive at the eigenvalue problem for each case of constraints in the following form [32]:
where the functions \(A_{ij}(\omega )\) are polynomials of \(\omega\).
Finally, the eigenvalues are calculated as roots of the characteristic equation:
A computational program has been developed within the Matlab environment to implement the DTM for solving the free vibration problem of inhomogeneous non-uniform FGP beams. The eigenvalue problem is solved using the standard algorithms provided by the Matlab package [59].
Results and Discussion
Verification
To verify the DTM adopted for solving the free vibration problem of inhomogeneous beams with non-uniform cross-sections, first, we examine various specific problems and compare the results obtained with DTM with those available in the existing literature. In the calculations, we adhered to the recommendations comprehensively discussed in Ref. [32] for providing the fast convergence of the solutions and to ensure the reliability of the results. In addition, as the calculations involve finding roots of high-degree polynomials, which can potentially lead to computational instability, we have implemented strategies recommended in the MATLAB documentation to enhance stability in symbolic calculations. It included optimizing code, symbolically simplifying polynomial equations before finding their roots, and utilizing functions to fine-tune the root-finding process [59].
We start with free vibration analysis of double-tapered homogeneous beams with the height and width varying linearly along the x-coordinate. This implies that we have chosen \(m=n=1\) in (1). Assuming that the cross-sectional dimensions of the beam vary with the same taper parameters for both height and width \(c_b=c_h=\alpha\), we can express (2) in the form: \(\frac{A(x)}{A_0} = \left( 1 - \alpha \frac{x}{L}\right) ^2\) and \(\frac{I(x)}{I_0} = \left( 1 - \alpha \frac{x}{L} \right) ^4\). The initial dimensions of the rectangular cross-section are taken as \(h_0\)=0.01 m and \(b_0\)=0.03 m, and the length of the beam is L= 1 m. The material parameters for this beam are defined such that Young’s modulus, \(E_0\)=210 GPa and the mass density, \(\rho _0\)=7800 kg/m\(^3\).
The non-dimensional natural transverse frequencies are specified as \({\bar{\omega }}_n= \omega _n L^2 \sqrt{\frac{\rho _0 A_0}{ E_0 I_0}}\). Herein, \(A_0\), \(I_0\), \(E_0\) and \(\rho _0\) are beam’s cross-section geometrical and material properties at \(x = 0\), respectively. For the sake of verification, the first three non-dimensional natural frequencies computed with the proposed technique are compared with those found in Refs. [30] and [33] for a variety of boundary conditions such as cantilever beam (C-F), fully clamped beam (C–C) and pinned–pinned beam (P–P), and at different values of the taper ratio, \(\alpha\). The results are collected in Table 1.
One can see in Table 1 that the results obtained using different approaches exhibit a high degree of consistency. This indicates that the proposed computation method demonstrates considerable accuracy in predicting the natural frequencies of homogeneous beams with variable cross-sections.
Moreover, to validate the ability of the proposed method to accurately restore the sought function (21) from its respective sets of images (18), the mode shapes of beams associated with the first three natural frequencies of the cantilever double-tapered homogeneous beam are constructed. In addition, we utilized ABAQUS software [60] to conduct the frequency analysis for the same homogeneous beams with non-uniform cross-sections. The mode shapes of the beam have been modeled using the beam element "B22" provided by the package. The comparisons of both computations for each taper ratio of the beam are depicted in Fig. 3.
The plots of the mode shapes demonstrate a high degree of consistency for each of three frequencies across all taper ratio cases. Thus, the precision of the computed natural frequencies plays a primary role in the accuracy of mode shape restoration in the DTM.
Next, we calculate the natural frequencies of the same double tapered beam with linear variations in height and width, that is using \(\frac{A(x)}{A_0} = \left( 1 - \alpha \frac{x}{L} \right) ^2\) and \(\frac{I(x)}{I_0} = \left( 1 - \alpha \frac{x}{L} \right) ^4\). In addition to these geometric variations, we also account for the axial variation of the beam’s material properties. Specifically, we consider the axially varying profiles of the Young’s modulus \(\frac{E(x)}{E_0} = \left( 1 + \frac{x}{L} \right)\) and the mass density \(\frac{\rho (x)}{\rho _0} = \left( 1 + \frac{x}{L} + \left( \frac{x}{L} \right) ^2 \right)\). The comparisons of first three non-dimensional natural transverse frequencies \({\bar{\omega }}_n\) computed with the DTM and those found in Refs. [31, 33, 34] for different boundary conditions and a variety of taper ratios are presented in Table 2.
Table 2 clearly demonstrates that the results match well among the four different approaches. This fact provides strong evidence for the ability of the proposed technique to accurately predict the natural frequencies of inhomogeneous beams with cross-sections varying along the beam’s length. In addition, it is worth noting that the Euler–Bernoulli model employed in the present calculations is suitable for our low-frequency analysis of slender beams.
In line with the previous example, we aimed to compare the mode shapes of the non-uniform AFGM beam, calculated using the DTM, with those obtained from ABAQUS to assess their accuracy. It’s important to mention that ABAQUS, utilizing the user-defined subroutine UMAT, enables the vibration analysis of FGM structures with constant thickness, as discussed in Ref. [61]. The recent expansion of this modeling technique to non-uniform FGM beams is elaborated in Ref. [62]. Utilizing these advancements, we computed the mode shapes for the non-uniform AFGM beam under investigation and their comparisons with those derived using the DTM are illustrated in Fig. 4
The plots clearly illustrate that the mode shapes of the non-uniform AFGM beams, for both of the modeling approaches, exhibit good agreement across all the taper ratio cases and for each of the three natural frequencies.
The accuracy of the presented computation approach in calculating natural frequencies of FGP beams is assessed further. In this respect, an FGP beam of length L= 1 m and a square cross-section, which is composed of the open-cell metallic foam with \(E_0=\) 200 GPa, \(\rho _0=\) 7850 kg/m\(^3\), and Poisson ratio equal to 1/3 is considered. The test problem provides a comparison of the first three non-dimensional natural frequencies \({\bar{\omega }}_n= \omega _n L \sqrt{\frac{\rho _0 \left( 1 - \nu ^2\right) }{E_0}}\) of a uniform FGP beam at the beam aspect ratio \(L/h=\)10. The FGP beam is assumed to be subjected to three distinct porosity distributions such as even (type I), uneven symmetric (type II), and uneven non-symmetric (type IV) profiles. The calculations are performed for various porosity coefficient \(e_0\) and different types of boundary conditions. The comparisons of the natural frequencies obtained in the present work and those available in Ref. [23] are presented in Table 3.
As observed in Table 3, the results exhibit good agreement for the first and, in some cases, the second natural frequencies across all boundary conditions and porosity coefficient values. However, notable discrepancies are observed for the third frequency. This discrepancy is attributed to the use of the third-order shear deformation theory for the FGP beam within the framework of the Chebyshev collocation method in Ref. [23]. This contrasts with the Euler–Bernoulli beam model used in our study, which neglects shear deformation and rotational effects in beam behavior. Nevertheless, the calculations in this study, which are based on the assumption of an initially planar cross-section remaining planar after deformation, offer practical engineering solutions for such structures with an emphasis on the simplicity and practicality of the Euler–Bernoulli beam model.
Parameter Study
Further, we use the proposed approach implementing the DTM to calculate natural frequencies of a series of non-uniform rectangular cross-section FGP beams. This includes cases with tapered width but constant height, tapered height but constant width, and double tapering with both height and width simultaneously. In the calculations, all four types of porosity profiles conditions through the beam thickness are taken into account. The material and geometrical properties of the FGP beams remain the same as those used in the previous test problems. The FGP beams under four types boundary and four values of non-zero porosity coefficients are investigated.
Let us consider a non-uniform FGP beam of length L= 1 m with a constant height \(h_0\) and a width b(x) that varies linearly with the x-coordinate. In other words, the cross-section characteristics are expressed as \(\frac{A(x)}{A_0} = \frac{I(x)}{I_0} = \left( 1- \alpha \frac{x}{L} \right)\). It is assumed that the beam aspect ratio is L/h= 20 and the taper ratio is \(\alpha\)= 0.2. Table 4 presents the first three dimensionless natural frequencies, normalized as \({\bar{\omega }}_n= \omega _n \frac{L^2}{h_0}\sqrt{\frac{12 \rho _0}{E_0}}\).
To better illustrate the influence of porosity on the free vibration of the non-uniform beams, we have generated graphs using the data provided in Table 4. These graphs depict non-dimensional natural frequencies plotted versus the porosity coefficient. Our analysis revealed that the first three frequencies of the porous beams exhibit similar trends for all considered boundary conditions. As a result, to limit the volume of the present paper, only findings pertaining to C–C constraints are presented in Fig. 5.
It is evident from the plots that the three natural frequencies, depending on the type of porosity distribution, demonstrate similar patterns of changes as the porosity coefficient increases. These changes exhibit similar trends across all kind of supports. Specifically, for the FGP beam with uneven symmetric (type II) distributions, the natural frequencies slightly increase as the porosity increases. On the other hand, for the FGP beams with the other types of distributions, the natural frequencies decrease as the porosity increases. This behavior can be attributed to the fact that, as the porosity coefficient rises, both beam stiffness and cross-sectional inertia decrease. However, in the case of uneven symmetric (type II) distribution, the reduction rate in beam stiffness is smaller than that in inertia, while in the other distributions, the opposite relationship holds. Remarkably, among the various profiles considered, the FGP beam with an uneven non-symmetric (type IV) profile shows the least decrease in natural frequencies. In contrast, the beam with an uneven symmetric (type III) profile experiences the most significant reduction compared to the other profiles.
The other study deals with non-uniform FGP beams of constant width \(b_0\) and height h(x) linearly varying with x-coordinate such that Eq. 2 take a form: \(\frac{A(x)}{A_0} = \left( 1 - \alpha \frac{x}{L} \right)\), \(\frac{I(x)}{I_0} = \left( 1 - \alpha \frac{x}{L} \right) ^3\) with \(\alpha\)=0.2. Table 5 collects the first three dimensionless natural frequencies for mentioned above four porosity profiles, considering four types of imposed boundary conditions and accounting for a range of porosity coefficients.
Similarly to the previous example, Fig. 6 presents plots of natural frequencies against porosity coefficient values, extracted from Table 5 for the beam clamped at both ends. Once more, these plots are necessary to clarify the influence of porosity on the free vibration characteristics of height-tapered porous beams.
Upon analyzing the plots presented in Fig. 5, it becomes apparent that while the natural frequencies differ from those observed in the case of the beam with tapered width, they exhibit similar trends in terms of frequency changing patterns as the porosity coefficient increases. Particularly, in the case of FGP beams with uneven symmetric (type II) distributions, the natural frequencies slightly increase with growing the porosity coefficient. Conversely, for FGP beams with other types of distributions, the natural frequencies decrease with an increase in porosity. Once again, the FGP beams with uneven non-symmetric (type IV) profiles experience a comparatively smaller decrease in natural frequencies compared to the other porosity distributions. Changing the boundary conditions among those considered does not alter the observed frequency trends as the porosity coefficient increases for the specified porosity distributions.
Last, non-uniform FGP beams with simultaneous linear variation of width and height along the x-coordinate are investigated. The cross-section parameters of the beams are defined as \(\frac{A(x)}{A_0} = \left( 1 - \alpha \frac{x}{L} \right) ^2\), \(\frac{I(x)}{I_0} = \left( 1 - \alpha \frac{x}{L} \right) ^4\), where \(\alpha\)=0.2. The first three non-dimensional natural frequencies for the specified range of the porosity profiles, boundary conditions, and porosity coefficient values are arranged in Table 6.
Figure7 shows plots of the natural frequencies versus the porosity coefficient for C–C boundary conditions, corresponding to the data in Table6. These plots clearly depict how porosity affects the natural frequencies of double-tapered beams. It is worth noting that similar trends are observed for the beams subjected to boundary conditions other than the shown clamped–clamped case for all three frequencies.
These plots do not exhibit any new aspects in frequency variations with the increase of the porosity parameter when compared to the observations in the previous two types of porous beams, namely those tapered with width and those tapered with height individually. This fact shows that the type of porosity profile is a dominant factor affecting the dynamic response of the tapered beams.
In addition, the data in Tables 4–6 are rearranged into plots to facilitate the comparison of the natural frequency versus porosity coefficient relationships between the beams of different taper shapes, porosity profiles, and boundary conditions. Each plot depicts frequency-porosity curves for FGP beams with distinct non-uniform geometries, including uniform, width-tapered, height-tapered, and double-tapered shapes. The plots are organized in alignment with four different porosity profiles, spanning from type I to type IV, all associated with a specific natural frequency.
In Fig. 8, one can see plots of non-dimensional natural frequencies (\({\bar{\omega }}_n\)) as they vary with porosity coefficients for clamped–clamped FGP beams of different taper shapes and porosity profiles. Each row corresponds to a specific frequency.
Analyzing the plots in Fig. 8, we revealed that, first, the geometric shapes of the FGP beams affect the natural frequencies. The frequencies of uniform and width-tapered beams have values close to each other, while, in turn, the frequencies of height-tapered and double-tapered beams are closely aligned but lower than those in the two previous beams. That is, the height taper ratio has a more pronounced effect on the natural frequencies compared to the width taper ratio. This is attributed to the fact that varying a height along the beam length directly impact the bending stiffness, leading to notable alterations in the natural frequencies. On the other hand, variations in the width taper ratio primarily affect the cross-sectional area that has a comparatively smaller impact on the natural frequencies [30].
Second, the porosity profile plays a significant role in the dynamic response of the beams of all shapes. In particular, for the FGP beams with an uneven symmetric profile with stiffer layers in the surface area (type II), all the first three natural frequencies exhibit a slight increase with an increase in the porosity coefficient. On the other hand, for beams with other porosity profiles, the frequencies decrease as the coefficient increases.
Arranging the non-dimensional natural frequencies (\({\bar{\omega }}_n\)) versus porosity coefficients for FGP beams with P–P and C–P supports in a manner similar to the plots in Fig. 8, we found out that these boundary conditions did not alter the trends observed in the frequency-porosity curves of the fully clamped FGP beam. As these plots do not provide new insights, we have not included them in the current context.
In the case of the cantilever FGP beam, the variations of the frequency-porosity curves resemble those in the FGP beams with C–C, P–P and C–P supports. However, the influence of the geometric shape on the natural frequencies is more pronounced for this beam type with all kinds of the porosity profiles as shown in Fig. 9. Specifically, the fundamental frequency, and to a lesser extent, the second frequency, exhibit notably distinct values depending on the beam shape.
Conclusions
The primary objective of this study is to examine the free vibration characteristics of beams with non-uniform cross-sections varying along the beam length, while the beams are composed of materials with functionally graded porosity changing across the beam thickness. The main focus is on calculating the natural frequencies of these beams under different boundary conditions and different types of the porosity profiles. In this study, the classical Euler–Bernoulli beam theory and Hamilton’s principle are utilized to derive the governing equation of motion for the beams. Subsequently, the differential transformation method is employed to solve this equation. This method, known as a semi-analytic approach to solving differential equations with variable coefficients, not only enhances computational accuracy but also reduces the computational cost compared to numerical methods such as the finite-element method. To validate the proposed technique, verification examples are provided, demonstrating the accuracy of the results of calculations. In summary, the results obtained from the parametric studies conducted in this research can be summarized as follows:
-
the presence of porosity and variations in geometry affect the free vibration of the beams under different support conditions, leading to alternations in their behavior compared to that of homogeneous uniform beams;
-
taper parameters have been observed to influence the vibration behaviors of the porous FGM beam in distinct ways. Specifically, the height taper ratio has a dominant effect on the transverse vibration, while the width taper ratio has a lesser impact on it;
-
various porosity profiles exhibit distinct effects on the natural frequencies of the FGP beams, resulting in diverse alterations in the relationships between frequencies and porosity coefficient;
-
the uneven symmetric porosity distribution with stiffer layer in central area of the cross-section (type III) affects the natural frequencies of the beam more significantly than the other porosity profiles for all types of boundary constraints;
-
the porosity profile in the form of uneven symmetric with stiffer layers in surface areas (type II) lead to improved performance of the beams, resulting in less variation in the natural frequencies with increasing porosity coefficient for all types of boundary constraints;
-
while the natural frequencies of FGP beams with uneven non-symmetric porosity profiles (type IV) are more sensitive to changes with growing the porosity compared to the beams with porosity profile type II, this porosity distribution causes a smaller decrease in the frequencies with increasing coefficient values compared to the porosity defined by an even pattern (type I) for all types of boundary constraints;
-
while the present beam model, developed using the simplest Euler–Bernoulli assumptions, provides reasonably accurate results, it may not be entirely suitable for sufficiently thick beams and definitely not for high frequency vibrations, i.e., the height to wavelength has to be small too. For enhanced accuracy, it is advisable to consider employing the Timoshenko beam theory or high-order shear deformation theories.
These results unequivocally highlight the importance of carefully selecting geometrical parameters and porosity profiles during the performance design process of FG porous beams. In this regard, the DTM proves to be an effective and accurate method for computing the natural frequencies of such beams.
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Appendix A
Appendix A
The averaged Young’s modulus \(E_z(x)\) and mass density \(\rho _z(x)\) in (16) determined by analytically integrating Eq. (11) over the rectangular domain A(x) for every porosity profile type (3)–(6) are presented as follows:
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Type I:
$$\begin{aligned} \begin{aligned} \alpha (x)&= \frac{1}{e_0} - \frac{1}{e_0}\left( \frac{2}{\pi }\sqrt{1 - e_0} - \frac{2}{\pi } + 1 \right) ^2, \\&\alpha _{*}(x) = \frac{2}{\pi } \\ \end{aligned} \end{aligned}$$(A.1) -
Type II:
$$\begin{aligned} \begin{aligned} \alpha (x)&= \frac{3}{\delta (x)}\Bigg [ \left( 1 - \frac{2}{\delta ^2(x)} \right) \sin \delta (x) + \frac{2}{\delta (x)}\cos \delta (x) \Bigg ],\\&\alpha _{*}(x) = \frac{\sin \delta (x) }{\delta (x)}, \\ \end{aligned} \end{aligned}$$(A.2)where \(\delta (x)= \frac{\pi h(x)}{2 h_0}\)
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Type III:
$$\begin{aligned} \begin{aligned} \alpha (x)&= \frac{3}{\delta (x)}\Bigg [ -\cos \delta (x) + \frac{2}{\delta (x)}\sin \delta (x) - \frac{2}{\delta ^2(x)}\left( 1 - \cos \delta (x) \right) \Bigg ],\\&\alpha _{*}(x) = \frac{1 - \cos \delta (x) }{\delta (x)} \\ \end{aligned} \end{aligned}$$(A.3) -
Type IV:
$$\begin{aligned} \begin{aligned} \alpha (x)&= \frac{3}{\delta _1(x)}\Bigg [ \left( 1 - \frac{2}{\delta _1^2(x)} \right) \sin \delta _1(x) + \frac{2}{\delta _1(x)}\cos \delta _1(x) \Bigg ]\cos \alpha _1,\\&\alpha _{*}(x) = \frac{\sin \delta _1(x) }{\delta _1(x)}\cos \alpha _1, \\ \end{aligned} \end{aligned}$$(A.4)where \(\delta _1(x) = \frac{\delta (x)}{2}\cos \alpha _1\)
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Burlayenko, V.N., Kouhia, R. Analysis of Natural Frequencies in Non-uniform Cross-section Functionally Graded Porous Beams. J. Vib. Eng. Technol. 12, 6527–6547 (2024). https://doi.org/10.1007/s42417-023-01268-x
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DOI: https://doi.org/10.1007/s42417-023-01268-x