Abstract
The initial boundary value problems of dynamics are considered for the isotropic elastic body with double porosity. By the Laplace transform these problems are reduced to boundary value problems of pseudo-oscillations. Special representations are constructed for the general solution of pseudo-oscillation equations by means of metaharmonic functions. Such an approach facilitates the solution of problems and their solutions are written explicitly in form of absolutely and uniformly converging series. It is proved that inverse transforms yield solutions of initial dynamic problems. The question concerning the uniqueness of regular solutions of the considered problems is investigated.
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1 Introduction
In recent years, interest has arisen in the study of problems of elasticity and thermoelasticity for porous solids. Theories of porous media are applied in many branches of engineering, technology [1, 2], geomechanics [3] and biomechanics [4].
The quasi-static theory for elastic materials with double porosity was developed by Aifantis and his coauthors in 1979-1986 [5,6,7,8]. This theory which the authors called consolidation theory combines the Barenblatt model [9] for a fluid flow in a medium of double porosity and the Biot model [10] for elastic materials with single porosity. In the quasi-static case the basic equations for water-saturated media with double porosity were obtained in [11, 12]. A fundamental solution of a system of equations of stationary oscillations in Aifantis’s quasi-static theory of elasticity was constructed for solid bodies with double porosity in the paper [13].
However the above-mentioned theories of porous elasticity did not take into account the inertia term and the studies involved only static and quasi-static problems. But the inertia effect plays a key role in the investigation of various problems of oscillations and wave propagation in elastic media with double porosity. Hence it is important to study a complete dynamic model for materials with double porosity. A dynamic system for the description of deformation in media with single porosity was worked out by Biot [14, 15]. Flow and deformation processes in media with double porosity are considered with the inertia effect taken into account in the paper [16]. A complete dynamic case of the combined linear theory of flow and deformation of media with double porosity is treated in the paper [17]. Love and Rayleigh waves are respectively studied in [18, 19], respectively. The historical development of the mechanics of porous bodies, fundamental results and the sphere of their application are presented in detail in the monographs [20,21,22,23].
From the standpoint of application it is especially important to construct solutions in explicit form because such solutions allow one to perform effectively quantitative analyses of the considered problem. Questions related to this topic are considered, for example, in the works [24,25,26,27,28], where the explicit solutions of static boundary value problems of elasticity are constructed for the specific liquid-saturated media with double porosity. In [29, 30], the static two-dimensional boundary value problems are solved explicitly for a porous disk with voids.
In this article, two-dimensional boundary value problems of dynamics for porous materials are solved explicitly.
Methods for solving problems for private oscillations are not considered. These questions can be found in many papers, for example, [31,32,33].
In the present paper in Sect. 2 the basic equations of the motion of fluid-saturated media with double porosity are given, the basic the initial boundary value problems are formulated for an isotropic elastic body with double porosity. By the Laplace transform these problems are reduced to boundary value problems of pseudo-oscillations.
In Sect. 3 Green’s identities are established and the uniqueness theorems are proved for solutions of both the initial problems and the corresponding problems of pseudo-oscillations.
In Sect. 4 the general solution of pseudo-oscillation equations are constructed by means of metaharmonic functions.
Examples of the application of these representations are given in Sect. 5. The problems of pseudo-oscillations for a specific elastic body - a porous disk - are solved. Solutions to these problems are obtained in the form of series. Conditions are provided that ensure the absolute and uniform convergence of these series and the use of the inverse Laplace theorem. It is proved that the inverse transforms provide a solution to the initial dynamic problems.
2 Formulation of boundary value problems
Let us consider the motion of a medium consisting of porous and permeable blocks separated from each other by a system of cracks (e.g. bone, granite). At every point of the medium are introduced two pressures: liquid pressure in pores and that in cracks. For such a body, called a medium with double porosity [7, 8], in the Aifantis theory of consolidation the problems of the theory of elasticity are formulated with the following boundary conditions: there are given the values of the displacement vector (or stress) and those of mean pressures (or values normal derivatives pressures) of liquid in pores and cracks.
Basic equations of the motion of fluid-saturated media with double porosity contain the displacement vector in the neighborhood of some point and also the fluid pressure in cracks and the fluid pressure in pores in the neighborhood of the same point.
Let D be a finite plane region surrounded by a closed curve K. In what follows we assume that an isotropic and homogeneous porous elastic solid occupies a region of D.
A system of equations of the linear theory of elastic materials with double porosity has the form [8, 9]:
where \( {\mathbf{x}} = (x_{1} ,x_{2} ) \in D, \) \( t \in T, \)\( T \equiv [0,\,\infty ) \) is time interval; \( \lambda \), \( \mu \), \( \rho \), \( \beta_{1} \), \( \beta_{2} \), \( m_{i} ,\;\alpha_{i} ,\;k\quad \)are the known elastic and physical constants, \( {\mathbf{u}}({\mathbf{x}},t) = (u_{1} ,u_{2} ) \) is the displacement of the point \( {\mathbf{x}} \); \( p_{1} ({\mathbf{x}},t) \) and \( p_{2} ({\mathbf{x}},t) \) are the average pressure values in the neighborhood of \( {\mathbf{x}} \) in the cracks and pores, respectively.
Let us formulate the following initial boundary value problems.
Find in the \( D \times T \) domain a regular solution \( {\mathbf{U}}({\mathbf{x}},t) = ({\mathbf{u}}({\mathbf{x}},t),\;p_{1} ({\mathbf{x}},t),\;p_{2} ({\mathbf{x}},t)) \) of system (2.1) that satisfies the initial conditions
and, on the boundary \( K \), one of the conditions:
where \( {\mathbf{z}} = (z_{1} ,z_{2} ) \in S, \) \( {\mathbf{n}}({\mathbf{z}}) = (n_{1} ({\mathbf{z}}),n_{2} ({\mathbf{z}})) \) is the external normal to \( K \); \( {\mathbf{f}} = (f_{1} ,f_{2} ) \), \( {\mathbf{U}}({\mathbf{x}},t) \in C^{1} (\bar{D}) \cap C^{2} (D), \) \( \bar{D} = D \cup K \); \( f_{1} ,\,f_{2} ,\,f_{3} ,\,f_{4} \) are the given functions on \( S \); \( \partial_{l} = \frac{\partial }{\partial l} \), \( l \) is an arbitrary function. It is assumed [7] that \( m_{i} > 0 \), \( k > 0 \), \( i = 1,2 \).
is the stress vector in the porous medium and
is the stress vector in classical elasticity.
Let us assume that on the boundary \( K \) the so-called consistency conditions [31]
are fulfilled, while for large \( t \) the functions \( {\mathbf{U}} \)and \( f \) satisfy the conditions
uniformly with respect to \( {\mathbf{x}} \in D \) and \( {\mathbf{z}} \in K, \); \( \xi_{0} \ge 0, \) \( M \)>0 are constant values, \( i = 0,1,2, \) \( q = 0,1,2,3,4 \); \( j = 1,2,3,4. \)
Consider the Laplace transform giving the originals \( {\mathbf{U}} \) and \( f_{j} \) their images \( {\tilde{\mathbf{U}}} \)and \( \tilde{f}_{j} \), respectively,
where \( \tau = \xi + i\eta \), \( \text{Re} \tau = \xi > 0 \), \( {\rm I}m\tau = \eta \in ( - \infty ;\infty ), \) \( {\tilde{\mathbf{U}}} = ({\tilde{\mathbf{u}}},\tilde{p}_{1} ,\tilde{p}_{2} ); \) \( j = 1,2,3,4. \)
Given the conditions (2.2) and applying the rule of differentiation of the original, the dynamic problems I and II can be reduced to the following auxiliary so-called tasks of pseudo-oscillations:
3 Uniqueness theorems
In this section Green’s identities are established and the uniqueness theorems are proved for solutions of both the initial problems and the corresponding problems of pseudo-oscillations.
As is known [31], in the \( D \times T \) domain, for arbitrary regular vectors \( {\mathbf{u}} = (u_{1} ,u_{2} ) \)
and \( \partial_{t} {\mathbf{u}} = (\partial_{t} u_{1} ,\partial_{t} u_{2} ) \) and differential operator \( A(\partial_{x} ) = \mu \Delta + (\lambda + \mu )\,\varvec{grad}\,\varvec{div} \) Green’s formula has the form
where \( E\,(\partial_{t} {\mathbf{u}}({\mathbf{x}},t),{\mathbf{u}}({\mathbf{x}},t)) \) is the nonnegative well-defined quadratic form. It is symmetric: \( E(\partial_{t} \,{\mathbf{u}}({\mathbf{x}},t),\,\,{\mathbf{u}}({\mathbf{x}},t)) = E({\mathbf{u}}({\mathbf{x}},t),\,\,\partial_{t} {\mathbf{u}}({\mathbf{x}},t)) \), and therefore
where
is the potential deformation energy, \( 3\lambda + 2\mu > 0 \), \( \mu > 0 \). Using formulas (3.2) and the formulas
from (2.1) and (3.1) we obtain Green’s formula for porous bodies in the case of dynamic problems:
where the vector \( {\mathbf{R}}(\partial_{x} ,{\mathbf{n}}){\mathbf{U}}({\mathbf{x}},t) \) is defined from (2.5).
Let \( {\mathbf{U^{\prime}}} \) and \( {\mathbf{U^{\prime\prime}}} \) be arbitrary regular solutions of anyone of problems (2.1), (2.2), (2.3) or (2.1), (2.2), (2.4). Then the difference \( {\mathbf{U}}({\mathbf{u}},p_{1} ,p_{2} ) = {\mathbf{U^{\prime}}} - {\mathbf{U^{\prime\prime}}} \)is a regular solution of the corresponding homogeneous problems. In that case, the right-hand side of formula (3.3) is equal to zero and we can write
Therefore in the time interval \( t \in [0;\infty ) \) the value of the integral
diminishes or remains constant and equal to zero. But since the integrand is nonnegative and equal to zero at the initial moment of time, each of the summands must be equal to zero too. Hence it follows that \( {\mathbf{u}} = 0, \) \( p_{1} = 0 \), \( p_{2} = 0 \), \( {\mathbf{U}}({\mathbf{u}},p_{1} ,p_{2} ) \)=0. So, the following statement is true.
Theorem 1
A unique regular solution of homogeneous problems of dynamic is identically zero.Now let us prove the uniqueness theorems for pseudo-oscillatory problems. Let \( {\tilde{\mathbf{U}}} = ({\tilde{\mathbf{u}}},\tilde{p}_{1} ,\tilde{p}_{2} ) \) be a solution of the homogeneous problem corresponding to one of problems (2.9), (2.10) or (2.9), (2.11), and \( {\mathbf{\bar{\tilde{U}}}} = ({\mathbf{\bar{\tilde{u}}}},\bar{\tilde{p}}_{1} ,\bar{\tilde{p}}_{2} ) \) be the complex-conjugate vector. For arbitrary regular vectors \( {\tilde{\mathbf{u}}} \) and \( {\mathbf{\bar{\tilde{u}}}} \) and differential operator \( A(\partial_{x} ) = \mu \Delta + (\lambda + \mu )\varvec{grad}\,\varvec{div} \) Green’s formula has the form
where\( E({\tilde{\mathbf{u}}},{\mathbf{\bar{\tilde{u}}}}) = \)\( \frac{1}{3} \)\( (3\lambda + 2\mu )\left| {\frac{{\partial \tilde{u}_{1} }}{{\partial x_{1} }} + \frac{{\partial \tilde{u}_{2} }}{{\partial x_{2} }}} \right|^{2} + \frac{\mu }{3}\left[ {\left| {\frac{{\partial \tilde{u}_{1} }}{{\partial x_{1} }} - \frac{{\partial \tilde{u}_{2} }}{{\partial x_{2} }}} \right|^{2} + 3\left| {\frac{{\partial \tilde{u}_{2} }}{{\partial x_{2} }}} \right|^{2} } \right] + \mu \left| {\frac{{\partial \tilde{u}_{1} }}{{\partial x_{2} }} + \frac{{\partial \tilde{u}_{2} }}{{\partial x_{1} }}} \right|^{2} . \)
Since \( 3\lambda + 2\mu > 0 \), \( \mu \)>0 and \( {\tilde{\mathbf{u}}} \cdot {\mathbf{\bar{\tilde{u}}}} = \left| {{\tilde{\mathbf{u}}}} \right|^{2} > 0 \), we have \( E({\tilde{\mathbf{u}}},{\mathbf{\bar{\tilde{u}}}}) = \)\( E({\mathbf{\bar{\tilde{u}}}},{\tilde{\mathbf{u}}}) \),
Applying the equality \( \int\limits_{D} {\tilde{p}_{i} } \Delta \,\bar{\tilde{p}}_{i} d{\mathbf{x}} = \int\limits_{K} {\tilde{p}_{i} } \partial_{n} \bar{\tilde{p}}_{i} dK - \int\limits_{D} {\left| {\varvec{grad}\,\tilde{p}_{i} } \right|}^{2} d{\mathbf{x}} \), \( i = 1,2 \) for system (2.9) we obtain Green’s formula for the porous body
For zero boundary conditions the right-hand side of equality (3.6) is equal to zero. Taking equality (3.5) into account and separating the real and the imaginary part in (3.6), we obtain
where \( a_{1} = \alpha_{1} + \frac{k\xi }{{\left| \tau \right|^{2} }} \), \( a_{2} = \alpha_{2} + \frac{k\xi }{{\left| \tau \right|^{2} }} \), \( a_{12} = \frac{k\xi }{{\left| \tau \right|^{2} }}. \)
Since \( \xi ,\,\,k,\,\,\alpha_{1} ,\,\,\alpha_{2} > 0 \), we have \( a_{1} a_{2} - a_{12}^{2} > 0 \).
If \( \eta = 0, \) then from (3.7) we obtain \( {\mathbf{U}}({\mathbf{u}},p_{1} ,p_{2} ) = 0 \). If \( \eta \ne 0, \) then from (3.8) it follows that \( {\tilde{\mathbf{u}}} = 0, \) \( \varvec{grad}\,\tilde{p}_{i} = 0, \) \( \tilde{p}_{1} = \)\( \tilde{p}_{2} = \varvec{const}. \) Taking (2.9) into account, we finally obtain \( \tilde{p}_{1} = \)\( \tilde{p}_{2} = 0. \) The following statement is true.
Theorem 2
Problems \( {\rm I}_{\tau } \) and \( {\rm I}{\rm I}_{\tau } \) have unique solutions.
4 General representation of solution of a system of equations pseudo-oscillations
In this section for the general solution of system (2.9), special representation are constructed through elementary functions.
Applying the operator \( \varvec{div} \) to the first equation of system (2.9), we obtain a system of equations with respect to the sought value \( \varvec{div}\,\,{\tilde{\mathbf{u}}}, \)\( \tilde{p}_{1} \) and \( \tilde{p}_{2} \). The determinant of this system has the following form
where \( \lambda_{0} = \lambda + 2\mu > 0 \). Expression (4.1) with respect to \( \Delta \) is a third degree polynomial with complex coefficients, \( \lambda_{0} m_{1} m_{2} > 0 \). Let us write it as the product
where the numbers \( ( - \omega_{j}^{2} ) \) are the root of polynomial (4.1), \( j = 1,2,3. \) Relations between these roots are expressed by Vieta’s formulas
It is assumed that \( \omega_{0}^{2} \equiv \omega_{3}^{2} . \)
Thus, using (4.2), with respect to \( \varvec{div}\,\,{\tilde{\mathbf{u}}}, \) \( \tilde{p}_{1} \) and \( \tilde{p}_{2} \) we obtain the new equations
Now, applying the operator \( \varvec{rot} = - \partial_{2} + \partial_{1} \) to the first equation of system (2.9), we obtain
where \( \omega_{4}^{2} = - \frac{{\rho \tau^{2} }}{\mu }, \) \( \varvec{rot}\,\,{\tilde{\mathbf{u}}} = \phi {}_{4} \).
A solution of system (4.4) can be written in the form
where \( \phi_{l} ({\mathbf{x}},\tau ) \) are scalar metaharmonic functions with a complex argument
while \( \omega_{l}^{2} \) are complex numbers which differ from one another in the half-plane \( \text{Re} \tau > 0 \), \( \omega_{1}^{2} \ne \omega_{2}^{2} \ne \omega_{3}^{2} \);
where
By an immediate check we conclude that representations (4.6) satisfy equations (2.9).
Remark
The check of the third equation of system (2.9) becomes easier if (4.9) in formula (4.8) is replaced by the following
It is proved that \( \varepsilon_{j} = \varepsilon^{\prime}_{j} \); \( j = 1,2,3. \)
5 Construction of solutions of boundary value problems of pseudo-oscillations for the porous disk
In this section, using representation (4.6), problems \( {\rm I}_{\tau } \) and \( {\rm I}{\rm I}_{\tau } \) are solved explicitly for a circle.
Let region D have the form of a disk bounded by a circumference K with radius R, the center of which coincides with the origin. Solutions of problems of pseudo-oscillation are obtained in the form of the series. The conditions are given which provide the absolute and uniform convergence of these series and the use of the Laplace inverse theorem. It is proved that inverse transforms yield solutions of initial dynamic problems.
Problem \( {\rm I}_{\tau } \) Regular solutions of equations (4.7) in the circle can be represented as follows [34]:
where \( {\mathbf{x}} = (r,\psi ), \) \( r^{2} = x_{1}^{2} + x_{2}^{2} , \) \( J_{m} \) is the Bessel function of a complex variable with integer index \( m \)\( {\mathbf{\rm X}}_{ml} = (\varvec{X}_{ml}^{'} ,\;\varvec{X}_{ml}^{''} ) \) is the sought constant vector, \( {\varvec{\upnu}}_{m} (\psi ) = (\cos m\psi ,\,\sin m\psi ), \) \( {\mathbf{s}}_{m} (\psi ) = ( - \sin m\psi ,\,\cos m\psi ), \) \( l = 1,\,2,\,3,\,4. \)
Let us write the boundary conditions (2.10) of Problem \( {\rm I}_{\tau } \) in terms of normal and tangent components
where \( \tilde{f}_{n} = n_{1} \,\tilde{f}_{1} + n_{2} \,\tilde{f}_{2} , \) \( \tilde{f}_{s} = - n_{2} \,\tilde{f}_{1} + n_{1} \,\tilde{f}_{2} \).
From representation (4.6) we write
We expand the functions \( \tilde{f}_{n} \), \( \tilde{f}_{s} \) and \( \tilde{f}_{i + 2} \) into Fourier series \( \tilde{f}_{n} ({\mathbf{z}},\tau ) = \sum\limits_{m = 0}^{\infty } {({\varvec{\upalpha}}_{m} (\tau ) \cdot {\varvec{\upnu}}_{m} (\psi )),} \)
where \( {\varvec{\upalpha}}_{m} (\tau ) = (\alpha_{m1} ,\,\alpha_{m2} ), \) \( {\varvec{\upbeta}}_{m} (\tau ) = (\beta_{m1} ,\,\beta_{m2} ) \) and \( {\varvec{\updelta}}_{mi} (\tau ) = (\delta_{mi1} ,\,\delta_{mi2} ) \) are the Fourier coefficients of the respective functions \( \tilde{f}_{n} \), \( \tilde{f}_{s} \) and \( \tilde{f}_{i + 2} \), \( i = 1,2 \).
Taking (4.6) into account, we substitute representations (5.1) into (5.3) and pass to the limit as \( r \to R \). Then, taking (5.4) into account, from the boundary conditions (5.2), for each \( m \) we obtain a system of algebraic linear equations
where \( J^{\prime}_{m} \) is the derivative of the function \( J_{m} \) with respect to its argument. We solve system (5.5) and substitute the obtained values of the vectors \( {\mathbf{\rm X}}_{mj} \) and \( {\mathbf{\rm X}}_{m4} \) into (5.1), and thereafter into (4.6). We obtain the solution of Problem \( {\rm I}_{\tau } \).
Problem \( {\rm I}{\rm I}_{\tau } \)Passing in (2.5) to the normal and tangent components we obtain
where \( \tilde{u}_{n} ({\mathbf{x}},\tau ) \) and \( \tilde{u}_{s} ({\mathbf{x}},\tau ) \) are defined by formulas (5.3). The boundary conditions (2.11) can be written in the form
where \( \tilde{f}_{n} \), \( \tilde{f}_{s} \) and \( \tilde{f}_{i + 2} \) are the known functions. It is assumed that they are expandable into Fourier series. Substitution (5.3) into (5.6), using (5.1) and (5.4) and passing to the limit as \( r \to R \), from (5.7) we obtain for each \( m \) a system of algebraic linear equations
Substituting the solution of system (5.8) into (5.1), and then into (4.6), we thus find the solutions \( {\tilde{\mathbf{u}}}({\mathbf{x}},\tau ), \) \( \tilde{p}_{1} ({\mathbf{x}},\tau ) \) and \( \tilde{p}_{2} ({\mathbf{x}},\tau ) \) of Problem \( {\rm I}{\rm I}_{\tau } \). From the uniqueness of the solutions of Problems \( {\rm I}_{\tau } \) and \( {\rm I}{\rm I}_{\tau } \) it follows that for each \( m \) the determinants of systems (5.5) and (5.8) are different from zero.
As is known, for \( m \to \infty \) and \( \left| \zeta \right| \le m \) we have the relation (see e.g. [35])
After substituting it into the solutions \( {\mathbf{\rm X}}_{mj} \)and \( {\mathbf{\rm X}}_{m4} \) of system (5.5), from representations (5.1) we can write
where \( \alpha_{m}^{'} = \hbox{max} (\left| {\alpha_{m} } \right|,\left| {\beta_{m} } \right|,\left| {\delta_{m1} } \right|,\left| {\delta_{m2} } \right|) \), \( c \) is the constant not depending on \( m \). As seen from (5.10) and (4.6), for \( {\tilde{\mathbf{u}}}({\mathbf{x}},\tau ), \) \( \tilde{p}_{1} ({\mathbf{x}},\tau ) \) and \( \tilde{p}_{2} ({\mathbf{x}},\tau ) \), and also for their first order derivatives to be expanded into series which absolutely and uniformly converge on the boundary \( K \), it is sufficient that the Fourier coefficients \( \alpha_{m}^{'} \) satisfy the condition \( \left| {\alpha_{m}^{'} } \right| \le \frac{c}{{m^{3} }},\quad m = 1,2, \ldots \)The latter estimate holds if \( \tilde{f} \in C^{2} (K) \). For Problem \( {\rm I}{\rm I}_{\tau } \), just like for \( {\rm I}_{\tau } \), we can conclude that the condition \( \tilde{f} \in C^{1} (K) \) ensures the uniform and absolute convergence of the series \( {\tilde{\mathbf{u}}}({\mathbf{x}},\tau ), \) \( \tilde{p}_{1} ({\mathbf{x}},\tau ) \) and \( \tilde{p}_{2} ({\mathbf{x}},\tau ) \) and their first order derivatives when \( {\mathbf{x}} \in \bar{D}. \)
By analyzing the general form of solutions \( {\mathbf{\rm X}}_{ml} \) \( (l = 1,2,3,4) \) and applying conditions (2.6) and (2.7) as well as the asymptotic properties of the Bessel function for large \( \zeta \) \( (\text{Re} \zeta > 0) \) and relatively small \( m \)
we can establish that the conditions \( f_{l} ({\mathbf{z}},t) \in C^{4} (0 \le t \)<\( \infty ) \) give the following estimate for the solution of Problem \( {\rm I}_{\tau } \)
for all \( \tau \)uniformly for each \( {\mathbf{x}} \), \( {\mathbf{x}} \in \bar{D}; \) \( l = 1,\,2,\,3,\,4. \) By an analogous reasoning we conclude that under the condition \( f_{l} ({\mathbf{z}},t) \in C^{3} (0 \le t < \infty ) \) estimate (5.11) is fulfilled for the solution of Problem \( {\rm I}{\rm I}_{\tau } \) too. Since the Bessel functions are analytic in the complex half-plane \( \text{Re} \tau > 0 \), the values \( {\mathbf{\rm X}}_{mj} \) and \( {\mathbf{\rm X}}_{m4} \), as well as \( \phi_{j} \), \( \phi_{4} \) \( (j = 1,2,3) \) and \( {\tilde{\mathbf{U}}} = (\tilde{u}_{1} ,\tilde{u}_{2} ,\tilde{p}_{1} ,\tilde{p}_{2} ) \) are also analytic functions \( \tau \) in the half-plane \( \text{Re} \tau > 0 \) for both problems. Under condition (5.11) the integral \( \int\limits_{ - \infty }^{\infty } {\left| {{\tilde{\mathbf{U}}}({\mathbf{x}},\,\,\xi + i\eta )} \right|d\eta } \) converges and \( {\tilde{\mathbf{U}}}({\mathbf{x}},\tau ) \to 0 \), as \( \left| \tau \right| \to \infty , \) uniformly with respect to \( {\mathbf{x}} \), \( {\mathbf{x}} \in \bar{D} \). By the Laplace inversion theorem (see e.g. [31]) vector \( {\tilde{\mathbf{U}}}({\mathbf{x}},\tau ) \) is an image, and the original is defined by the integral
where \( \text{Re} \tau = \xi \)>\( \xi_{0} \ge 0, \) \( \xi_{0} \) is the growth exponent of the original. Condition (5.11) is sufficient for the existence of the derivatives \( \partial_{t} {\mathbf{U}}({\mathbf{x}},t) \) and \( \partial_{t}^{2} {\mathbf{u}}({\mathbf{x}},t) \).
Having in view expressions (2.8), (2.10) or (2.11), by direct computations we ascertain that the vector \( {\mathbf{U}}({\mathbf{x}},t) \)defined by formula (5.12) satisfies system (2.1), the initial conditions (2.2), and also the boundary conditions (2.3) or (2.4). In the formula (5.12) vector \( {\tilde{\mathbf{U}}}({\mathbf{x}},\tau ) \) is solution pseudo-oscillations problems (2.9), (2.10) or (2.9), (2.11).
6 Conclusions
-
1.
The novelty of the paper. We consider two-dimensional dynamic initial boundary value problems of elasticity for the body with double porosity. By the Laplace transform (2.8) these problems are reduced to the boundary value problems of pseudo- oscillations (2.9)–(2.11). For the general solution of system (2.9), special representations (4.6) are constructed through elementary (metaharmonic) functions. The properties of these functions are well known in mathematical physics. Such an approach facilitates the solution of two-dimensional problems of pseudo-oscillations. The solutions of this problems are obtained in the form of absolutely and uniformly convergent series. The conditions are written under which the inverse transforms exist and yield solutions of the initial problems. Green’s formulas are derived and the uniqueness theorems are proved for solutions of both the initial problems and the corresponding problems of pseudo-oscillations.
-
2.
Main result. Explicit solutions to the original problems are expressed by the formula (5.12), where vector \( {\tilde{\mathbf{U}}}({\mathbf{x}},\tau ) \) is solution pseudo-oscillations problems (2.9), (2.10) or (2.9), (2.11).
-
3.
The application of the considered method enables us to investigate a wide class of problems for systems of equations in modern linear theories of elasticity, thermoelasticity and porous elasticity for materials with double porosity; build explicit solutions basic boundary value problems not only for a circle, but also for a ring, a plane with a circular hole, etc.
Compliance with ethical standards
Conflict of interest: The authors declare that they have no conflict of interests.
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Tsagareli, I. Solution of dynamic boundary value problems for an elastic disk with double porosity. SN Appl. Sci. 2, 1962 (2020). https://doi.org/10.1007/s42452-020-03764-1
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DOI: https://doi.org/10.1007/s42452-020-03764-1