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Two-Dimensional Fractional Order Generalized Thermoelastic Porous Material

Abstract

In the work, a two-dimensional problem of a porous material is considered within the context of the fractional order generalized thermoelasticity theory with one relaxation time. The medium is assumed initially quiescent for a thermoelastic half space whose surface is traction free and has a constant heat flux. The normal mode analysis and eigenvalue approach techniques are used to solve the resulting non-dimensional coupled equations. The effect of the fractional order of the temperature, displacement components, the stress components, changes in volume fraction field and temperature distribution have been depicted graphically.

Keywords:
Fractional derivative; Porous material; Normal mode analysis; Eigenvalue approach

1 INTRODUCTION

Porous materials make their appearance in a wide variety of settings, natural and artificial and in diverse technological applications. As a consequence a number of problems arise dealing, among others, with statics and strength, fluid flow and heat conduction, and the dynamics of such materials. In connection with the latter, we note that problems of this kind are encountered in the pre diction of behavior of sound-absorbing materials and in the area of exploration geophysics, the steadily growing literature bearing witness to the importance of the subject Pecker and Deresiewiez (1973)Pecker, C. and Deresiewiez, H. (1973). Thermal Effects on Wave in Liquid-Filled Porous Media. Journal of Acta Mechanica 16: 45-64..

The problem of a fluid-saturated porous material has been studied for many years. A short list of papers pertinent to the present study includes (Biot 1941Biot, M. A. (1941). General theory of three-dimensional consolidation. Journal of Applied Physics 12: 155-164., 1956Biot, M. A. (1956).Theory of propagation of elastic waves in a fluid-saturated porous solid. I. Low-frequency range. Journal of the Acoustical Society of America, 28: 168-178.), Gassmann (1951)Gassmann, F. (1951). Uber die elastizitat poroser medien. Veirteljahrsschrift der Natur forschenden Gesellschaft in Zzirich. 96: 1-23., Biot and Willis (1957)Biot, M. A., and Willis, D. G. (1957). The elastic coefficients of the theory of consolidation. Journal of Applied Mechanics, 24:594-601., Biot (1962)Biot, M. A. (1962). Mechanics of deformation and acoustic propagation in porous media. Journal of Applied Physics, 33: 1482-1498., Deresiewicz and Skalak (1963)Deresiewicz, H. and Skalak, R. (1963). On uniqueness in dynamic poroelasticity, Bulletin of the Seismological Society of America, 53: 783-788., Mandl (1964)Mandl, G. (1964). Change in skeletal volume of a fluid-filled porous body under stress, Journal of Mechanics and Physics of Solids, 12: 299-315., Nur and Byerlee (1971)Nur, A. and Byerlee, J. D. (1971). An exact effective stress law for elastic deformation of rock with fluids. Journal of Geophysics Ressearch, 76:6414-6419., Brown and Korringa (1975)Brown, R. J. S. and Korringa, J. (1975). On the dependence of the elastic properties of a porous rock on the compressibility of the pore fluid. Geophyics, 40:608-616., Rice and Cleary (1976)Rice, J. R., and Cleary, M. P. (1976). Some basic stress diffusion solutions for fluid-saturated elastic porous media with compressible constituents. Reviews of Geophysics and Space Physics, 14: 227-24., Burridge and Keller (1981)Burridge, R., and Keller, J. B. (1981). Poroelasticit,y equations derived from microstructure. Journal of the Acoustical Society of America, 70: 1140-1146., (Zimmerman et al. 1986Zimmerman, R. W., Somerton, W. H., and King, M. S. (1986). Compressibility of porous rocks. Journal of Geophysics Ressearch, 91:12765-12777.,1994Zimmerman, R. W., Myer, L. R., and Cook, N. G. W. (1994). Grain and void compression in fractured and porous rock. International Journal of Rock Mechanics and Mining Sciences &Geomechanics Abstracts, 31:179-184.), Berryman and Milton (1991)Berryman, J. G., and Milton, G. W. (1991). Exact results for generalized Gassmann's equations in composite porous media with two constituents. Geophyics, 56: 1950-1960., Thomp son and Willis (1991)Thompson, M., and Willis, J.R. (1991). A reformation of the equations of anisotropic poroelasticity. Journal of Applied Mechanics, 58: 612-616.], Pride et al. (1992)Pride, S. R., Gangi, A. F., and Morgan, F. D. (1992). Deriving the equations of motion for porous isotropic media. Journal of the Acoustical Society of America, 92: 3278-3290., Berryman and Wang (1995)Berryman, J. G., and Wang, H. F. (1995). The elastic coefficients of double-porosity models for fluid transport in jointed rock. Journal Geophysics Research, 100: 24611-24627., Tuncay and Corapcioglu (1995)Tuncay, K., and Corapcioglu, M. Y.: Effective stress principle for saturated fractured porous media. Water Resources Res. 31, 3103-3106 (1995)., Alexander and Cheng (1991)Cheng, A. H. D. (1991). Integral equation for Poroelasticity in Frequency Domain with BEM solution, Journal of Engineering Mechanics, 117(5): 1136-1157, Charlez, P. A., and Heugas, O. (1992)Charlez, P.A. and Heugas, O. (1992). Measurement of thermoporoelastic properties of rocks: theory and applications, Ed. J.A. Hudson. 42-46., Abousleiman et al. (1998)Abousleiman, Y. and Cui, L. (1998). Poroelastic Solutions in Transversely Isotropic Media for Wellbore and Cylinder. International Journal of Solid and Structure, 35: 4905-4903., Ghassemi and Diek (2002)Ghassemi, A., Diek, A. (2002). Porothermoelasticity for swelling shales. Journal of Petrolim Science & Engineering, 34: 123-135., Tod (2003)Tod, S. R. (2003). An anisotropic fractured poroelastic effective medium theory. International Journal of Geophysics, 155: 1006-1020..

Eringen (1970)Eringen, A.C. (1970). Foundations of micropolar thermoelasticity, CSIM Udine, Course of Lectures 23, CD-ROM. and Nowacki (1966)Nowacki, M. (1966). Couple-stresses in the theory of thermoelasticity, Procceding of IUTAM Symposium, 1: 259-278. developed the linear theory of micropolar thermoelasticity which are known as micropolar coupled thermoelasticity to include thermal effects. Goodman and Cowin (1972)Goodman, M.A. and Cowin, S.C. (1972). A continuum theory for granular material, Archive for Rational Mechanics and Analysis, 44: 248-265. established a continuum theory for granular materials, whose matrix material (or skeletal) is elastic and interstices are voids and they introduced the concept of distributed body, which represents a continuum model for granular materials (sand, grain, powder, etc) as well as porous materials (rock, soil, sponge, pressed powder, cork, etc.). Nunziato and Cowin (1979)Nunziato, J.W. and Cowin, S.C. (1979). A non-linear theory of elastic material with voids, Archive for Rational Mechanics and Analysis, 44, 174-200., developed the non-linear theory of elastic materials with void, underlying the basic concept that the bulk density of the material is written as the product of two fields, the density field of the matrix material and the volume fraction field (the ratio of volume occupied by grains to the bulk volume at a point of the material) Kumar and Gupta (2010)Kumar, R. and Gupta, R.R. (2010). Axi-symmetric deformation in the micropolar porous generalized thermoelastic medium, Bulletin of the Polish Academy of Sciences Technical Sciences, 58(1): 129-139 ]. Othman (2007)Othman, M. I. A. (2005). Effect of rotation and relaxation time on a thermal shock problem for a half-space in generalized thermo-viscoelasticity. Acta Mechanica, 174: 129-143. studied the effect of rotation and relaxation time on a thermal shock problem for a half-space in generalized thermo-viscoelasticity and Othman and Singh (2005)Othman, M. I. A. and Singh, B. (2007). The effect of rotation on generalized micropolar thermoelasticity for a half-space under five theories. International Journal of Solid and Structure, 44: 2748-2762. studied the effect of rotation on generalized micropolar thermoelasticity for a half-space under five theories. Youssef (2007)Youssef, H. M. (2007). Theory of generalized porothermoelasticity, International Journal of Rock Mechincs and Mining Science, 44: 222-227. constructed theory of generalized porothermoelasticity which describe the behavior of thermoelastic porous medium in the context of the theory of generalized thermoelasticity with one relaxation time (Lord-Shulman). The energy and the entropy equations have been derived also in general co-ordinates. The uniqueness of the solution for the complete system of the equations of the theorem has been proved by Kumar et al. (2013)Kumar, R., Gupta, V. and Abbas, I. A. (2013). Plane deformation due to thermal source in fractional order thermoelastic media. Journal of Computational and Theoritical Nanoscience, 10(10):2520-2525. and he discussed the plane deformation due to thermal source in fractional order thermoelastic media, while Abbas and Kumar (2014)Abbas, I.A. and Kumar, R. (2014). Deformation Due to thermal source in Micropolar Generalized Thermoelastic Half- Space by Finite element method, Journal of Computational and Theoritical Nanoscience, 11(1): 185-190 studied the deformation due to thermal source in micropolar generalized thermoelastic half- space by finite element method.

Recently, a new formula of heat conduction has been considered in the context of the fractional integral operator definition by Youssef (2010)Youssef, H. M. (2010). Theory of fractional order generalized thermoelasticity. Journal of Heat and Transfer (ASME), 132: 1-6.. This new consideration generated the fractional order generalized thermoelasticity which was cited by Youssef who approved the uniqueness of its solutions.

Youssef solved one dimensional problem in the context of the fractional order generalized thermoelasticity and discussed the effects of the fractional order parameter on all the studied fields and with Al-Leheabi i(2010)Youssef, H. M., Al-Leheabi, E. O. (2010). Fractional order generalized thermoelastic half-space subjected to ramp-type heating, Journal of Mechanics Research and Communication, 37: 448-452.. Youssef (2012)Youssef, H. M. (2012). Two-dimensional thermal shock problem of fractional order generalized thermoelasticity, Acta Mechanics 223(6): 1219-1231. solved two-dimensional thermal shock problem of fractional order generalized thermoelasticity with thermal shock. Povstenko (2005)Povstenko, Y. Z. (2005). Fractional heat conduction equation and associated thermal stress, Journal of Thermal Stresses, 28: 83-102. solved a problem of fractional heat conduction equation and associated thermal stress. The counterparts of our problem in the contexts of the thermoelasticity theories have been considered by using analytical and numerical methods (Abbas et al. 2002Abd-alla , A. N. and Abbas, I. A. (2002).A Problem of generalized magneto-thermo-elasticity for an infinitely long, perfectly conducting cylinder, Journal of Thermal Stresses, 25: 1009-1025, 2008Abbas, I.A. and Abd-alla, A. N. (2008). Effects of thermal relaxations on thermoelastic interactions in an infinite orthotropic elastic medium with a cylindrical cavity, Archive of Applied Mechanics, 78: 283-293., 2009Abbas, I.A. (2009). Generalized magneto-thermoelasticity in a non-homogeneous isotropic hollow cylinder using finite element method. Archive of Applied Mechanics, 79(1): 41-50., 2011Abbas, I.A. & Othman, M.I. (2011). Effect of rotation on plane waves at the free surface of a fiber-reinforced thermoelastic half-space using the finite element method. Meccanica, 46, (2): 413-421, 2012Abbas, I.A. & Othman, M.I. (2012).Generalized thermoelsticity of thermal shock problem in an isotropic hollow cylinder and temperature dependent elastic moduli, Chinese Physics B, 21(1): 014601.).

In this paper, a two-dimensional problem of a porous material will be considered within the context of the fractional order generalized thermoelasticity theory with one relaxation time. The medium will be assumed initially quiescent for a thermoelastic half space whose surface is traction free and has a constant heat flux. The normal mode analysis and eigenvalue approach techniques will be used to solve the resulting non-dimensional coupled equations. The effect of the fractional order of the temperature, displacement components, the stress and components, changes in volume fraction field distribution will be depicted graphically.

2 GOVERNING EQUATIONS

For homogeneous, linear and thermally elastic medium with voids and temperature dependent mechanical properties, the basic equations in the context of the Lord and Shulman (1997)Lord, H. and Shulman, Y. (1967). A generalized dynamical theory of thermoelasticity, Journal of Mechanics and Physics of Solid,15: 299-309. model and Cowin and Nunziato (1983)Cowin, S. C. and Nunziato, J. W. (1983). Linear Elastic Materials with Voids, Journal of Elasticity 13(2): 125-147. in absence of body forces and heat source are given by Kumar and Devi (2011)Kumar, R. and Devi, S. (2011). Deformation in porous thermoelastic material with temperature dependent properties, Applied Mathematics & Information Science, 5(1): 132-147..

The equations of motion Kumar and Devi (2011)Kumar, R. and Devi, S. (2011). Deformation in porous thermoelastic material with temperature dependent properties, Applied Mathematics & Information Science, 5(1): 132-147.:

And

The generalized heat conduction equation Youssef (2010)Youssef, H. M. (2010). Theory of fractional order generalized thermoelasticity. Journal of Heat and Transfer (ASME), 132: 1-6. and Kumar and Devi (2011)Kumar, R. and Devi, S. (2011). Deformation in porous thermoelastic material with temperature dependent properties, Applied Mathematics & Information Science, 5(1): 132-147.:

where the fractional integral operator defined as follows Youssef (2010)Youssef, H. M. (2010). Theory of fractional order generalized thermoelasticity. Journal of Heat and Transfer (ASME), 132: 1-6.:

and Γ(α) is the Gamma function.

The constitutive equations

The cubical dilatation

where ρ is the mass density, T the temperature change of a material particle, To the reference uniform temperature of the body, ui the displacement vector components, eij the strain tensor; σij the stress tensor, cE the specific heat at constant strain, γ the thermal elastic coupling tensor in which γ = (3λ + 2μ)αt, αt is the coefficient of linear thermal expansion, K is a material constant thermal conductivity, λ, μ are elastic parameters, β, b, ξ1, m, w 0 and ψ are the material constants due to presence of voids and ϕ is the change in volume fraction field of voids.

Formulation and solution of the problem

We consider an isotropic, homogenous and elastic body with voids in two-dimensional fills the region 0 ≤ x < ∞, -∞ < z < ∞ subjected to a time-dependent heat source and traction free on the surface x = 0. The governing equations will be written in the context of Lord and Shulman model when the body has no heat sources or anybody forces, and we will use the Cartesian co-ordinates (x, y, z) and the components of the displacement ui = (u, 0, w) to write them as follows:

The equations of motion are in the forms

and

The heat conduction equation

The heat flux equation in x-direction

The constitutive relations are

and

The cubical dilatation

For our convenience, the following non-dimensional variables and notations are used:

where .

In terms of the non-dimensional quantities defined above, the governing equations will be reduce to (dropping the dashed for convenience)

where

3 NORMAL MODE ANALYSIS

The solution of considered physical variables can be decomposed in terms of normal mode as following form

where ω is a complex constant, , b is the wave numbers in the z-directions. Using equation (24), equations (16)-(23) become respectively:

where

Equations (25)-(28) can be written in a vector-matrix differential equation as follows

where

and

4 SOLUTION OF THE VECTOR-MATRIX DIFFERENTIAL EQUATION

Let us now proceed to solve equation (30) by the eigenvalue approach proposed by Das et al. (2009)Das, N. C., Lahiri, A. and Sarkar, S. (2009). Eigenvalue value approach three dimensional coupled thermoelasticity in a rotating transversely isotropic medium. Tamsui Oxf. Journal of Mathimatical Science, 25: 237-257.. The characteristic equation of the matrix W takes the form

where

The roots of the characteristic equation (33) which are also the eigenvalues of matrix W in the form

The eigenvector

which are corresponding to eigenvalue λ can be calculated as

From equations (36)-(40) we can easily calculate the eigenvector , corresponding to eigenvalue λj, j = 1,2,3,4,5,6,7,8.

For further reference, we shall use the following notations:

The solution of equation (30) can be given by:

where the terms containing exponentials of growing nature in the space variable x have been discarded due to the regularity condition of the solution at infinity, A 1, A 2, A 3 and A 4 are constants to be determined from the boundary condition of the problem. Thus, the field variables can be written for x ≥ 0, t > 0, -∞ ≤ z ≤ ∞, as:

To complete the solution we have to know the constants A 1, A 2, A 3 and A 4, so we will use the following boundary conditions.

5 APPLICATION

We will consider that the bounding plane of the medium x = 0 traction free and has a constant heat flux with constant strength.

Thus, the appropriate boundary conditions are

and

which gives

where qo is the strength of the heat flux and it is constant

From the boundary conditions (50), (51) and (53), we obtain

where the element of matrix Hrs are given by:

6 NUMERICAL RESULTS AND DISCUSSIONS

Following Kumar and Devi (2011)Kumar, R. and Devi, S. (2011). Deformation in porous thermoelastic material with temperature dependent properties, Applied Mathematics & Information Science, 5(1): 132-147., magnesium material was chosen for purposes of numerical evaluations. The physical data are given as

Figures 1-8 represent the temperature distribution, displacement u distribution, displacement w distribution, the change in volume fraction field of voids distribution, the strain distribution, the stress σxx distribution, the stress σxz distribution and the stress σzz distribution respectively at constant time t = 2.5 and constant z = 0.5 with different values of the fractional parameter α = 0.5, 1.0, 1.5 which express for the weak thermal conductivity, normal thermal conductivity and super thermal conductivity respectively.

Figure 1:
The temperature distribution with different value of the fractional parameter.

Figure 2:
The displacement u distribution with different value of the fractional parameter.

Figure 3:
The displacement w distribution with different value of the fractional parameter.

Figure 4:
The change in volume fraction field of voids distribution with different value of the fractional parameter.

Figure 5:
The strain distribution with different value of the fractional parameter.

Figure 6:
The stress σxx distribution with different value of the fractional parameter.

Figure 7:
The stress σxz distribution with different value of the fractional parameter.

Figure 8:
The stress σzz distribution with different value of the fractional parameter.

In figure 1, the fractional order parameter α has a significant effect on the temperature distribution, where increasing on α causes increasing on T and the rate of change of T with respect to x also increases when α increases which is compatible with the definition of the thermal conductivity.

In figures 2 and 3, the fractional order parameter α has a significant effect on the displacement u and w distributions, where increasing on α causes increasing on the absolute values of u and w, and the rate of change of them with respect to x also increase when α increases which is compatible with the definition of the thermal conductivity.

Figure 4 shows the variation of change in volume fraction field respect to x with different value of the fractional order parameter α. It is seen that, the volume fraction starts with its maximum value at the origin and decreases until attaining zero. The fractional order parameter α has a significant effect on the change in volume fraction field of voids distribution Φ, where decreases with the decrease in the value of fractional parameter α.

In figure 5, the fractional order parameter α has a significant effect on strain distribution e, where increasing on α causes increasing on e, and the rate of change of e with respect to x also increases when α increases which is compatible with the definition of the thermal conductivity.

In figures 6-8, the fractional order parameter α has significant effects on all components of the stress distribution, where increasing on α causes increasing the absolute values of the stresses, and the rate of change of them with respect to x also increase when α increases which is compatible with the definition of the thermal conductivity.

7 CONCLUSION

In this work, the effect of the fractional order of the temperature, displacement components, the stress components, changes in volume fraction field and temperature distribution have been studying for a two-dimensional problem of a porous material is considered within the context of the fractional order generalized thermoelasticity theory with one relaxation time. We found that, the fractional order parameter has significant effects on all the studied fields and the results supporting the definition of the classification of the thermal conductivity of the materials to three types; weak, normal and super conductivity.

References

  • Abbas, I.A. & Othman, M.I. (2012).Generalized thermoelsticity of thermal shock problem in an isotropic hollow cylinder and temperature dependent elastic moduli, Chinese Physics B, 21(1): 014601.
  • Brown, R. J. S. and Korringa, J. (1975). On the dependence of the elastic properties of a porous rock on the compressibility of the pore fluid. Geophyics, 40:608-616.
  • Lord, H. and Shulman, Y. (1967). A generalized dynamical theory of thermoelasticity, Journal of Mechanics and Physics of Solid,15: 299-309.
  • Abbas, I.A. & Othman, M.I. (2011). Effect of rotation on plane waves at the free surface of a fiber-reinforced thermoelastic half-space using the finite element method. Meccanica, 46, (2): 413-421
  • Abbas, I.A. (2009). Generalized magneto-thermoelasticity in a non-homogeneous isotropic hollow cylinder using finite element method. Archive of Applied Mechanics, 79(1): 41-50.
  • Abbas, I.A. and Abd-alla, A. N. (2008). Effects of thermal relaxations on thermoelastic interactions in an infinite orthotropic elastic medium with a cylindrical cavity, Archive of Applied Mechanics, 78: 283-293.
  • Abbas, I.A. and Kumar, R. (2014). Deformation Due to thermal source in Micropolar Generalized Thermoelastic Half- Space by Finite element method, Journal of Computational and Theoritical Nanoscience, 11(1): 185-190
  • Abd-alla , A. N. and Abbas, I. A. (2002).A Problem of generalized magneto-thermo-elasticity for an infinitely long, perfectly conducting cylinder, Journal of Thermal Stresses, 25: 1009-1025
  • Abousleiman, Y. and Cui, L. (1998). Poroelastic Solutions in Transversely Isotropic Media for Wellbore and Cylinder. International Journal of Solid and Structure, 35: 4905-4903.
  • Berryman, J. G., and Milton, G. W. (1991). Exact results for generalized Gassmann's equations in composite porous media with two constituents. Geophyics, 56: 1950-1960.
  • Berryman, J. G., and Wang, H. F. (1995). The elastic coefficients of double-porosity models for fluid transport in jointed rock. Journal Geophysics Research, 100: 24611-24627.
  • Biot, M. A. (1941). General theory of three-dimensional consolidation. Journal of Applied Physics 12: 155-164.
  • Biot, M. A. (1956).Theory of propagation of elastic waves in a fluid-saturated porous solid. I. Low-frequency range. Journal of the Acoustical Society of America, 28: 168-178.
  • Biot, M. A. (1962). Mechanics of deformation and acoustic propagation in porous media. Journal of Applied Physics, 33: 1482-1498.
  • Biot, M. A., and Willis, D. G. (1957). The elastic coefficients of the theory of consolidation. Journal of Applied Mechanics, 24:594-601.
  • Burridge, R., and Keller, J. B. (1981). Poroelasticit,y equations derived from microstructure. Journal of the Acoustical Society of America, 70: 1140-1146.
  • Charlez, P.A. and Heugas, O. (1992). Measurement of thermoporoelastic properties of rocks: theory and applications, Ed. J.A. Hudson. 42-46.
  • Cheng, A. H. D. (1991). Integral equation for Poroelasticity in Frequency Domain with BEM solution, Journal of Engineering Mechanics, 117(5): 1136-1157
  • Cowin, S. C. and Nunziato, J. W. (1983). Linear Elastic Materials with Voids, Journal of Elasticity 13(2): 125-147.
  • Das, N. C., Lahiri, A. and Sarkar, S. (2009). Eigenvalue value approach three dimensional coupled thermoelasticity in a rotating transversely isotropic medium. Tamsui Oxf. Journal of Mathimatical Science, 25: 237-257.
  • Deresiewicz, H. and Skalak, R. (1963). On uniqueness in dynamic poroelasticity, Bulletin of the Seismological Society of America, 53: 783-788.
  • Eringen, A.C. (1970). Foundations of micropolar thermoelasticity, CSIM Udine, Course of Lectures 23, CD-ROM.
  • Gassmann, F. (1951). Uber die elastizitat poroser medien. Veirteljahrsschrift der Natur forschenden Gesellschaft in Zzirich. 96: 1-23.
  • Ghassemi, A., Diek, A. (2002). Porothermoelasticity for swelling shales. Journal of Petrolim Science & Engineering, 34: 123-135.
  • Goodman, M.A. and Cowin, S.C. (1972). A continuum theory for granular material, Archive for Rational Mechanics and Analysis, 44: 248-265.
  • Kumar, R. and Devi, S. (2011). Deformation in porous thermoelastic material with temperature dependent properties, Applied Mathematics & Information Science, 5(1): 132-147.
  • Kumar, R. and Gupta, R.R. (2010). Axi-symmetric deformation in the micropolar porous generalized thermoelastic medium, Bulletin of the Polish Academy of Sciences Technical Sciences, 58(1): 129-139
  • Kumar, R., Gupta, V. and Abbas, I. A. (2013). Plane deformation due to thermal source in fractional order thermoelastic media. Journal of Computational and Theoritical Nanoscience, 10(10):2520-2525.
  • Mandl, G. (1964). Change in skeletal volume of a fluid-filled porous body under stress, Journal of Mechanics and Physics of Solids, 12: 299-315.
  • Nowacki, M. (1966). Couple-stresses in the theory of thermoelasticity, Procceding of IUTAM Symposium, 1: 259-278.
  • Nunziato, J.W. and Cowin, S.C. (1979). A non-linear theory of elastic material with voids, Archive for Rational Mechanics and Analysis, 44, 174-200.
  • Nur, A. and Byerlee, J. D. (1971). An exact effective stress law for elastic deformation of rock with fluids. Journal of Geophysics Ressearch, 76:6414-6419.
  • Othman, M. I. A. (2005). Effect of rotation and relaxation time on a thermal shock problem for a half-space in generalized thermo-viscoelasticity. Acta Mechanica, 174: 129-143.
  • Othman, M. I. A. and Singh, B. (2007). The effect of rotation on generalized micropolar thermoelasticity for a half-space under five theories. International Journal of Solid and Structure, 44: 2748-2762.
  • Pecker, C. and Deresiewiez, H. (1973). Thermal Effects on Wave in Liquid-Filled Porous Media. Journal of Acta Mechanica 16: 45-64.
  • Povstenko, Y. Z. (2005). Fractional heat conduction equation and associated thermal stress, Journal of Thermal Stresses, 28: 83-102.
  • Pride, S. R., Gangi, A. F., and Morgan, F. D. (1992). Deriving the equations of motion for porous isotropic media. Journal of the Acoustical Society of America, 92: 3278-3290.
  • Rice, J. R., and Cleary, M. P. (1976). Some basic stress diffusion solutions for fluid-saturated elastic porous media with compressible constituents. Reviews of Geophysics and Space Physics, 14: 227-24.
  • Thompson, M., and Willis, J.R. (1991). A reformation of the equations of anisotropic poroelasticity. Journal of Applied Mechanics, 58: 612-616.
  • Tod, S. R. (2003). An anisotropic fractured poroelastic effective medium theory. International Journal of Geophysics, 155: 1006-1020.
  • Tuncay, K., and Corapcioglu, M. Y.: Effective stress principle for saturated fractured porous media. Water Resources Res. 31, 3103-3106 (1995).
  • Youssef, H. M. (2007). Theory of generalized porothermoelasticity, International Journal of Rock Mechincs and Mining Science, 44: 222-227.
  • Youssef, H. M. (2010). Theory of fractional order generalized thermoelasticity. Journal of Heat and Transfer (ASME), 132: 1-6.
  • Youssef, H. M. (2012). Two-dimensional thermal shock problem of fractional order generalized thermoelasticity, Acta Mechanics 223(6): 1219-1231.
  • Youssef, H. M., Al-Leheabi, E. O. (2010). Fractional order generalized thermoelastic half-space subjected to ramp-type heating, Journal of Mechanics Research and Communication, 37: 448-452.
  • Zimmerman, R. W., Myer, L. R., and Cook, N. G. W. (1994). Grain and void compression in fractured and porous rock. International Journal of Rock Mechanics and Mining Sciences &Geomechanics Abstracts, 31:179-184.
  • Zimmerman, R. W., Somerton, W. H., and King, M. S. (1986). Compressibility of porous rocks. Journal of Geophysics Ressearch, 91:12765-12777.

Publication Dates

  • Publication in this collection
    July 2015

History

  • Received
    16 Sept 2014
  • Reviewed
    16 Dec 2014
  • Accepted
    13 Feb 2015
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