Abstract
In this paper, the finite element solutions of crack-tip fields for an elastic porous solid with density-dependent material moduli are presented. Unlike the classical linearized case in which material parameters are globally constant under a small strain regime, the stiffness of the model presented in this paper can depend upon the density with a modeling parameter. The proposed constitutive relationship appears linear in the Cauchy stress and linearized strain independently. From a subclass of the implicit constitutive relation, the governing equation is bestowed via the balance of linear momentum, resulting in a quasi-linear partial differential equation (PDE) system. Using the classical damped Newton’s method, the sequence of linear problems is then obtained, and the linear PDEs are discretized through a bilinear continuous Galerkin-type finite element method. We perform a series of numerical simulations for material bodies with a single edge-crack subject to a variety of loading types (i.e. the pure mode-I, II, and mixed-mode). Numerical solutions demonstrate that the modeling parameter in our proposed model can control preferential mechanical stiffness with its sign and magnitude along with the change of volumetric strain. This study can provide a mathematical and computational foundation to further model the quasi-static and dynamic evolution of cracks, utilizing the density-dependent moduli model and its modeling framework.
Keywords
Introduction
Mechanical stiffness of a porous solid is dependent not only on the mechanical property of solid grain but also on the bulk skeleton composed of connected or disconnected pores (or microstructures). For example, the shear stiffness of sandy soil can be lost and act like liquid when soil liquefaction occurs. 1 It is also well known that the mechanical properties of metal matrix composite or alloy are largely dependent on the defects, that is, porosity. 2 Furthermore, the pore space can be partially or fully saturated with fluid (e.g. gas or liquid) inside, which can induce the poromechanical effects.3–5 In the field of petroleum engineering and rock mechanics, 6 hydraulic fracturing7,8 (or commonly known as fracking) is a well-known stimulation technology for the development of shale gas with high pressure gradient, which aims to generate tensile fractures in the rock. The success of hydraulic fracturing is highly dependent on the mechanical properties of rock,7,9 as it is much more efficient for sand which is stiffer than soft clay or mud for tensile failure. Considering the heterogeneity in the composites, simple averaging of rock properties might mislead, but rigorous mathematical formulation (e.g. the multiple porosity model4,10) is required.
Material properties and mechanical strength can also be reliant on certain modes of loading preferentially. For instance, brittle materials are generally weak in tension, and their tensile strength is known to be only one-tenth of compressive strength. 11 Meanwhile, ductile materials are known to possess approximately equal strength in tension and compression, but weak in shear. Experimental results regarding hydraulic fracturing also substantiate that shear failure may occur in advance before the tensile failure around the crack-tip, 12 where mixed-mode of loading exists. Regarding this stiffness anisotropy, we particularly pay attention to the density change of a porous material. Microstructures of material including pore space are required to bond with one another to transmit the tensile loading. 11 Meanwhile, the fracture propagation is demanding under a compressive loading, as transverse cracks can emerge and tend to congregate, resulting in the increased density of material. Representatively, concrete or ceramics is weak under tension but strong against compression, thus composite (or reinforced) material can be synthesized with them to have higher tensile strength. Rock is another exemplary material such that it is stiffer against compressive loading but weaker against tensile or shear loading. On the other end, two-dimensional (2D) material 13 (e.g. the graphene) is considered to be one of the strongest materials able to withstand tensional loading, due to the 2D nature of the structure. In essence, the preferential strength can be related to material moduli that are dependent upon density of the material or change in volumetric strain: the dilation versus compaction.
Furthermore, this density-dependent stiffness concept is physically reasonable in that elastic properties of a porous material are known to have nonlinear relations along with the porosity,14,15 even though it is not straightforward to model these in the continuum scale. Conventional practice of modeling porous solid is based on the elastic and infinitesimal strain regime, wherein the Cauchy stress is expressed as a function of deformation gradient and density at material points. This classical relationship, where material moduli are generally constants, has been successfully used in various applications. However, this classical linearized theory of elasticity cannot accommodate the phenomena found in many metallic alloys (see Saito et al. 16 and Hou et al. 17 ) and concrete (see Grasley et al. 18 ) that exhibit nonlinear mechanical responses well within the range of “small strains,” nor aforementioned realistic responses.
The objective of this study to investigate elastic porous solids of preferential stiffness with an explicit type of the density-dependent moduli model. Recently, Rajagopal19–23 has established a new class of constitutive relations for the description of non-dissipative elastic bodies (for more details about “novel” elastic constitute relationships). These implicit constitutive relations have been explored in many studies to describe the state of stress-strain in the neighborhood of crack-tip,24–33 for the behavior of thermoelastic bodies,34,35 viscoelastic materials,36–42 and quasi-static crack evolution.43,44 Utilizing the implicit constitutive relation in Rajagopal45,46 and Rajagopal and Saccomandi 47 and the density-dependent moduli derived with a simplified parameter of the model, we address the preferential or anisotropic stiffness of a material with in the sense of tension/compaction that is, change in void: dilation and compaction. Another goal is to weigh up the applicability of the density-dependent material moduli model for the quasi-static or dynamic propagation of a network of cracks under mechanical/thermal loading.
To this end, we assume a homogeneous porous solid with a crack inside, where the mechanical regime is under small strain and pure elasticity without any failure. Particularly for the stiffness variations, we focus on the crack (or damaged pores) and its tip under different modes of loadings: mode-I, II, and mixed-mode. Instead of an explicit porosity, that is, one of the state variables based on the mixture theory3,48,49 that can also be saturated with fluid inside, a pure solid matrix with implicit porosity is considered through the change of volumetric strain. We employ a computational model that is physically and mathematically consistent with the framework developed in Yoon et al. 43 and Lee et al. 44 a universal approach based on the Newton’s method and standard finite element method (FEM). This approach yields a numerically stable and efficient algorithm against the serious nonlinear problem of our interest. In the numerical experiments, our iterative algorithm displays an optimal order convergence for a BVP with a manufactured solution. Comparing this nonlinear model with the conventional linearized elasticity model, distinct variations of stress and strain distributions are demonstrated, especially near the crack-tip area under different modes of loading, that is, parallel and perpendicular to the crack. We also compare the stress intensity factor, drained bulk modulus, and volumetric strain change to elucidate the preferential stiffness of the elastic porous solid. Furthermore, we find that the intensity of preferential stiffnessis controllable through the parameter of the model, relating the void to density variation of a porous solid. Upon the efficacy of the density-dependent material moduli model and its modeling framework, current study can further be expanded to the topics such as the fracture evolution (hydraulic fracture), fluid transport, or heat transfer in deformable porous media.
Formulation of the density-dependent material moduli model
The current investigation is prompted by a recent study (see Rajagopal45,46 and Rajagopal and Saccomandi 47 for more details) on developing new nonlinear constitutive relationships between the linearized strain and Cauchy stress. The density-dependent material moduli model is worthwhile in characterizing the cracks or damaged pores in porous solids such as rocks and concrete.
Basic notations
In this section, we provide a brief introduction to the geometrical and mechanical description of the elastic porous solid body, highlighting its mass balance. Let
where the partition consists of a Neumann boundary
In the rest of this paper, we use the usual notations of Lebesgue and Sobolev spaces.50,51 We denote
with the inner (scalar) product and the norm defined, respectively, as:
The closure of
The space of displacements satisfying the homogeneous and non-homogeneous Dirichlet boundary conditions are defined as:
Let
where
Henceforth, we shall not distinguish the dependence of the quantities on
Let
where
The principle of angular momentum balance implies that the Cauchy stress tensor is symmetric, that is,
The balance of mass (or continuity equation) in the material description follows that
where
More details about the kinematics and kinetics can be found in Truesdell and Noll. 52
Implicit constitutive relations
In this study, our focus is to study the behavior of elastic (nondissipative) porous solids whose material moduli depend on the density. The response of such materials to the mechanical loading can be straightforwardly described by implicit constitutive relations, introduced by Rajagopal45,46 and the references therein.
A generalization for the elastic body defined through an implicit type constitutive relation19,20 between the Cauchy stress and deformation gradient is of the form:
where
Assuming that the function
where the material moduli
Using the linearization assumption given in (8) and the subsequent asymptotic results for the classical terms (9), we obtain a special subclass of the implicit constitutive relations of the form:
where the terms
where the material moduli
Another subclass of models of the above general class of relations (19) wherein the constitutive relation is linear in both
In the above relation (21), the moduli
where
Taking
By the balance of mass in the reference configuration (as in (14)), one can express the above relation as
with both functions
Boundary value problem and numerical method
In this section, we develop a boundary value problem and the numerical approach for computing the stress and strain fields in the elastic porous solid body which includes a crack-tip.
Mathematical model
The elastic material body under consideration is homogeneous, isotropic, initially unstrained, and unstressed. Let
To model the stress response of the material whose material moduli are dependent upon the density, for example, the elastic porous solids, we make use of implicit constitutive relations (see Rajagopal and Wineman
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for details). A special subclass of such elastic bodies can be obtained if one starts with (24) and use
We note that the above constitutive relationship is invertible, and the inverted relation is written for the Cauchy stress as:
which is the definition for the stress of the proposed density-dependent model. Plugging (28) into (27), we note that the stress and strain relation reduces to the same form of the linearized elasticity:
where the fourth-order tensor
and both the constants
Note that
and the generalized (drained) bulk modulus
With
Combining the balance of linear momentum (26) and the constitutive relationship (27), we obtain the following governing system of equations:
The above system of partial differential equations (PDEs) needs to be supplemented by appropriate boundary conditions with
where
The above boundary value problem can also be formulated in variational form as a problem of minimizing the total strain-energy density functional. This approach will be studied in future communication. As (36) is nonlinear, it is not tractable in the current form to any well-known analytical or numerical methods. In the following section, we propose Newton’s method for the linearization at the differential equation level, followed by the bilinear finite element method as a discretization technique.
Newton’s iterative method and variational formulation
To construct the numerical approximation to the boundary value problem (BVP) (36), we first linearize the differential equation to obtain a sequence of linear problems. Consider a mapping
The assumption of smoothness that we made for the Sobolev space (4) and the quasi-linearity of the operator in (37) bestow us to apply the Newton’s method to obtain the linearized version of the PDE model (34).
Given the initial guess
where
for each
Then, combining the equations (40), (34a), and (34b), we obtain the updated model equations:
Then, the solution at the next iteration level is constructed by using
where
From equation (43d), note that it is clear that we need to impose the zero Dirichlet boundary conditions at each iteration level for Newton’s update
Continuous weak formulation
Here, we provide a variational formulation for the linearized version of the nonlinear BVP derived in the previous section. Also, the function spaces used to define the variational formulation have already been defined in the beginning, and the same setting is applied. To pose a weak formulation, we multiply the equations in the strong formulation (43a) with the test function from
where the bilinear term
Finite element discretization
Finally, we first recall some basic notions and structure of the classical finite element method (FEM) to discretize the weak formulation (44). The meshes used for all computations in the numerical examples presented in this paper are quadrilaterals. Let
For any
where
The discrete counterpart of the continuous formulation (
where the linear and bilinear terms are given by:
where
and
The solution at the next iteration level is given by
Note that we obtain an initial solution for the Newton’s iteration via solving the linear problem (i.e. with
The following algorithm (
The new value for
Finally, the overall algorithm for the boundary value problem with the whole nonlinear density-dependent model is presented in
Numerical experiments and discussion
The primary purpose of this section lies in verifying the constitutive relation of density-dependent material moduli for an elastic porous solid via modeling and computational approaches provided in the previous sections. Using the proposed and classical models, we present several numerical tests to compare the stress and strain distributions in the computational domains under different mechanical loadings. Distributions of preferential stiffness from the density-dependent model can be confirmed particularly near the crack-tip preferentially. Ultimately, our goal is to suggest the rationale for this nonlinear model, from which physically meaningful and reliable responses of the damaged pores or the crack-tip can be described under the mechanical loading.
All numerical implementations are done using the deal.II,
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finite element library. Against the nonlinearity, the Newton’s method is employed with the lower bound of the convergence (i.e. the tolerance) as
-convergence study
In this section, we introduce a sample problem to verify the mathematical description and algorithm of the numerical model proposed in this study. To this end,
for an unit square domain (1 m × 1 m) as Figure 1. The Dirichlet condition that satisfies the exact solution is applied for all the boundaries (from

An unit square domain and the Dirichlet boundary conditions for h-convergence study.
The Results of
Boundary value problems with mechanical loadings
Premise and setup for numerical experiments
In this study, the elastic regime is of interest, thus we do not consider any dissipation of energy. We also do not consider any fluid saturation in the solid, thus the porous solid of our interest is in the unsaturated condition. Neither is any explicit porosity concept in the model nor any initial porosity value that is directly measurable through experiments, or calculated via formula. However, the implicit concept of porosity is still considered with the volumetric strain,
From

Numerical domains (unit square, 1 m × 1 m) for
Example 1: No crack problems
In this example, no crack or slit exists but an intact porous solid is considered. Note that two different traction loads are applied to the top boundary
while
Note that we have slightly different Dirichlet boundary conditions for the bottom boundary (
Figures 3 and 4 demonstrate the displacements for

Displacements (unit: m) on the reference line (

Displacements (unit: m) on the reference line (
To investigate the preferential stiffness with these positive and negative

Numerical domains (unit square, 1 m × 1 m) with cracks for
Example 2: Tensile loading with crack
For
The roller boundary conditions are applied to
Stress and strain
In Figure 6(a)–(c),

[
[
We also investigate with the stress intensity factor (SIF) calculated on the reference line in Figure 5(a). The calculation of SIF for the mode-I (
where
with the same location for

[
Volumetric strain and bulk modulus
Here, we illustrate the change of the drained bulk modulus

[
Example 3: In-plane shear loading with crack
For
Stress and strain
For this in-plane shear loading, we plot

[
[
Two SIFs on the reference line (Figure 5(b)) are illustrated in Figure 10 using (57) and (58). We find that at about x/L

[
Volumetric strain and bulk modulus
In Figure 11, the bulk modulus and volumetric strain for each case are plotted. We confirm that the stiffness of each case is illustrated in the opposite compared to

[Example 3] Bulk modulus (
Example 4: mixed-mode loading with crack
In this last example, the mixed-mode (i.e. the mode-I and II) of loading is applied. The boundary conditions are as follows:
Note that we have the same bottom boundary
Stress and strain
We plot both

[Example 4] (a–c) stress

[
[
Using (57) and (58), the SIF of each mode on the reference line is presented in Figure 14. Compared to

[
Volumetric strain and bulk modulus
From Figure 15 (middle) and (right), we identify that the volumetric strains for all cases are about the same. Until about the point of x/L

[
Conclusion
The purpose of this paper is to study mechanical responses of an elastic porous solid with preferential stiffness of which material moduli are dependent upon the density, and to provide a stable finite element solution of stress and strain fields, particularly around the crack-tip. The proposed model based on the same linearization as the linearized elasticity, that is, the gradient of the displacement is infinitesimal, cannot stem from the conventional framework of Cauchy elasticity. It is structured on a special constitutive relation (27) for elastic porous solids that show significantly distinctive responses from those using classical linearized models. For our numerical approaches, we employ a universal and computationally efficient method of Newton’s method and FEM under the framework developed in Yoon et al. 43 and Lee et al. 44 to overcome the nonlinearity of the model with partial differential equation. The proposed algorithm in the study is verified for the optimal convergence rate using the method of manufactured solution. Three different types of loading are considered in this work. Even though the constitutive relation studied in this paper is simplified via a single parameter describing the mechanical response of the material under scrutiny, the distinctive variations in the fields of stress and strain are found around the crack-tip or damaged pores. Some key findings of this work are:
In a domain without a crack, the modeling parameter “
For a domain with an edge crack under three different types of loading, both crack-tip stress concentration and strain energy density are found to be the maximum directly in front of the crack-tip, which is consistent with the observation obtained within the classical linearized elasticity model. This implies that the density-dependent moduli model can apply to the crack propagation phenomenon.
For a domain with the edge crack under pure tensile loading (or mode-I type of loading), the crack-tip axial strains are larger with smaller bulk modulus for higher positive
In the example with in-plane shear loading (or mode-II type of loading), the density-dependent model for positive
Finally, for the mixed-mode loading (combination of mode-I and mode-II loadings), under about the same amount of volumetric strain changes on the reference line, the deviations between the cases are concentrated still around the crack-tip, and the positive
As the fracture toughness or its propagation is known to be related to the newly generated porosity or damaged pores, the model for an elastic porous solid with the preferential material property can be expanded to study a (quasi-static) crack evolution in the porous material via an appropriate numerical method such as the regularized phase-field approach.43,44 Application of the extended finite element method (similar to the works in Riazi et al. 65 and Afrazi et al. 66 ) to study quasi-static evolution problems within the context of the proposed model can be another key idea for future investigation. Another important next topic can include bridging the modeling parameter to the material parameter via comparing with some experimental data and identifying its role for the purpose of characterization.
Footnotes
Acknowledgements
SMM thanks the support of the College of Science & Engineering, Texas A&M University-Corpus Christi.
Handling Editor: Chenhui Liang
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: HCY appreciates the support of the basic research fund (Project No. GP2020-006) of the Korea Institute of Geoscience and Mineral Resources (KIGAM).
