EFFECT OF INITIAL STRESS ON THE REFECTION OF MAGNETO-ELECTRO-THERMO-ELASTIC WAVES FROM AN ISOTROPIC ELASTIC HALF-SPACE

Size: px
Start display at page:

Download "EFFECT OF INITIAL STRESS ON THE REFECTION OF MAGNETO-ELECTRO-THERMO-ELASTIC WAVES FROM AN ISOTROPIC ELASTIC HALF-SPACE"

Transcription

1 International Journal of Physics and Mathematical Sciences ISSN: 77- (Online) 4 Vol. 4 (4) October-December, pp /Kakar EFFECT OF INITIAL STRESS ON THE REFECTION OF MAGNETO-ELECTRO-THERMO-ELASTIC WAVES FROM AN ISOTROPIC ELASTIC HALF-SPACE *Rajneesh Kakar Department of Engineering & Technology, GNA University, Phagwara, India *Author for Correspondence ABSTRACT The present work illustrates a theoretical study of the refection of magneto-electro-thermo-elastic plane waves from an isotropic pre-stressed elastic half-space in generalized thermoelasticity under GL-theory. Magnetic field and electric field acts initially parallel to the plane boundary of the elastic half-space. Refection of magneto-electro-thermoelastic waves under generalized thermoelasticity theory is used to study the refection of plane waves from a semi-infinite elastic solid in a vacuum. The expressions for the refection coefficients are obtained mathematically. Results are plotted with MATLAB software to show the effect of temperature, magnetic field, electric field, relaxation time and initial stresses on the reflection of incident SV-wave. Mathematics Subject Classification: 74F5; 74H5; 8D4. Keywords: Reflection Coefficients; Magnetic Field; Electric Field; Relaxation Time; GL- theory INTRODUCTION Problem related to magneto-electro-thermoelastic plane wave deals with the interactions among strain, temperature, and electromagnetic fields in transversely isotropic and anisotropic medium has many applications in geophysics, optics, electrical power engineering and seismology. The modelling of surface waves dispersion effects has become of growing interest to geotechnical engineers and geophysicists. The seismic waves usually studied in seismology and seismic surveying are those produced by earthquakes, explosions, or impacts. These waves are complex vibrations of limited duration having the nature of an impulse. The problem of propagation velocity of these complex vibrations requires additional research. When the wavelength of the harmonic component is significantly small compared with the heterogeneity, such as thickness of layers, the oscillations are propagated following the laws of geometrical optics. By knowing the reflection and refraction, the magneto-thermal elastic plane waves are the useful source for imagining the interior of the Earth. According to the conventional heat conduction theory, the thermal disturbances travel at infinite velocities. However, from the physical point of view, the above concept is unrealistic in the situation of very low temperature near absolute zero. The hyperbolic equations of motion are applicable in such cases and the elastic disturbances propagate with finite speeds. Thus, generalized thermoelasticity theories are proposed to examine modified thermoelastic models involving a hyperbolic type of heat equation. Shekhar and Parvez (3) purposed plane waves propagating in transversely isotropic dissipative half space under the effect of rotation, magnetic field and stress. Othman and Song () discussed reflection of magneto-thermo-elastic wave by using generalized theory of elasticity. Mehditabar et al., (4) investigated magneto -thermo-elastic functionally graded conical shell. Othman () studied electro-magneto-thermoelastic thermal shock plane waves for a finite conducting half-space. Niraula and Noda () purposed non-linear electro-magneto-thermo-elasticity by deriving material constants. Niraula and Wang (6) studied the property of magneto-electro-elastic material with a penny-shaped crack subjected to temperature loading. Kaur and Sharma () discussed reflection and transmission of thermoelastic plane waves at liquid-solid interface. Fractional order generalized electro-magneto-thermo-elasticity was given by Ya et al., (3). Propagation of plane waves at the interface of an elastic solid half-space and a microstretch thermoelastic diffusion solid half-space was investigated by Kumar et al., (3). Chakraborty (3) Copyright 4 Centre for Info Bio Technology (CIBTech) 79

2 International Journal of Physics and Mathematical Sciences ISSN: 77- (Online) 4 Vol. 4 (4) October-December, pp /Kakar discussed reflection of plane elastic waves in half-space subjected to temperature and initial stress. Singh and Yadav () discussed the reflection of plane waves in a rotating transversely isotropic magneto-thermoelastic solid half-space. Singh and Bala () purposed the reflection of P and SV waves from the free surface of a two-temperature thermoelastic solid half-space. Kakar and Kakar (3) theoretical discussed electro-magneto-thermo viscoelastic surface waves in non-homogenous solid medium under the effect of gravity, compression and couple-stress In this paper, we have discussed the problem of reflection of magneto-electro-thermoelastic waves under initial stress in transversely isotropic solid half space. Biot s equations are modified in terms of Green and Lindsay s theory of thermoelasticity. We find that P-wave is affected due to the presence of thermal and magnetic field whereas SV-wave remains unaffected which is in accordance with the GL-theory since the temperature and magnetic field in an infinite space results only in irrotational changes. The governing equations are solved in light of modified heat equation to obtain reflection coefficients for P-wave, thermal wave and SV-wave. The effect of temperature, magnetic field, electric field, relaxation time and initial stresses on reflection coefficients of incident SV-wave are plotted under certain practical assumptions. Governing Equations The governing equations of linear, isotropic and homogenous magneto-electro-thermoelastic solid with initial stress are a. The stress-strain-temperature relation: sij P( ij ij ) epp ij eij ( ) ij, () k where, T sij are the components of stress tensor, P is initial pressure, ij is the Kronecker delta, ij are the components of small rotation tensor,, are the counterparts of Lame parameters, e ij are the components of the strain tensor, α is the volume coefficient of thermal expansion, k T is the isothermal compressibility, is small temperature increment, is the absolute temperature of the medium, is the reference uniform temperature of the body chosen such that The displacement-strain relation: u u i j eij () xj x i where, u i are the components of the displacement vector. The small rotation-displacement relation: u u i j ij (3) xj x i where, u i are the components of the displacement vector. b. The modified Fourier s law: hi a* h i K (4) xi where, K is the thermal conductivity, aa, * are the thermal relaxation times c. The heat conduction equation : 3 3 u v u v K c γ p ij x y t t xt yt xt yt (5) Copyright 4 Centre for Info Bio Technology (CIBTech) 8.

3 International Journal of Physics and Mathematical Sciences ISSN: 77- (Online) 4 Vol. 4 (4) October-December, pp /Kakar where, K is the thermal conductivity, cp is specific heat per unit mass at constant strain, is the first relaxation time, is second relaxation time, ij is the Kronecker delta, is density and T is the incremental change of temperature from the initial state of the solid half space. Moreover the use of the relaxation times, and a parameter ij marks the aforementioned fundamental equations possible for the three different theories: Classical Dynamical theory:, ij Lord and Shulman s theory:,, ij Green and Lindsay s theory:, ij d. Maxwell s equations:,,, e e (6) t t where,, B, e and e are electric field, magnetic field, permeability and permittivity of the medium. e. The components of electric and magnetic field:,, h,,, e (7) where, h is the perturbed magnetic field over and e is the perturbed electric field over E. f. Maxwell stress components for electro-magneto-thermoelastic medium: Tij e Hiei H jej Hkek ij ] e[ Eiei E jej Ekek ij where i, j, k =,,3 (8) where, H, H, H are the components of primary magnetic field, E, E, E are the components of i primary electric field, j k e i, e j, e k are the stress components acting along X-axis, Y-axis, Z-axis respectively and ij is the Kronecker delta. Using Eq. (8), we get u v T u v eh ee x y x y and T (9) The dynamical equations of motion for the propagation of wave have been derived by Biot (965) and in two dimensions these are given by s s u P Bx () x y y t i j k s s v P By () x y x t where, s, s and s are incremental thermal stress components. The first two are principal stress components along x- and y-axes, respectively and last one is shear stress component in the x-y plane, is the density of the medium and u, v are the displacement components along x and y directions respectively, B is body force and its components along x and y axis are B and B respectively. is the v u rotational component i.e. x y and P s s. The body forces along x and y axis under constant primary magnetic field H parallel to z-axis are given by x y Copyright 4 Centre for Info Bio Technology (CIBTech) 8

4 International Journal of Physics and Mathematical Sciences ISSN: 77- (Online) 4 Vol. 4 (4) October-December, pp /Kakar u v u v Bx eh ee x xy x xy () u v u v By eh ee xy x xy x (3) where, e and e are permeability and permittivity of the medium. Following Biot (965), the stress-strain relations with incremental isotropy are s ( P) exx ( P) eyy exx x (4) s exx ( ) eyy x (5) s e (6) xy where, u xx, v e eyy, e v u xy (7) x x x y where, e xx and eyy are the principle strain components and exy is the shear strain component, (3 ) t, t is the coefficient of linear expansion of the material, are Lame s constants, is the incremental change of temperature from the initial state and is second relaxation time. Formulation of the Problem We consider a transversely isotropic, homogeneous elastic half space under constant magnetic and electric field acting along z-axis and initial compressive stress P acting along x-axis at absolute temperature (Figure ). y-axis Atmosphere y x-axis θ θ θ Elastic half space Incident SV-wave θ θ Reflected SV-wave Reflected P-wave Reflected Thermal wave Figure : Reflection of magneto-electro-thermo-elastic plane waves Copyright 4 Centre for Info Bio Technology (CIBTech) 8

5 International Journal of Physics and Mathematical Sciences ISSN: 77- (Online) 4 Vol. 4 (4) October-December, pp /Kakar A plane SV-wave is incident at an angle at y, such that it get reflected and giving three waves namely reflected SV at an angle, thermal-waves at an angle and P-wave at an angle respectively as shown in the diagram Boundary Conditions The following boundary conditions are supplemented at y : i. f s Pe, x xy ii. f s, y iii. T ht. (8) y Solution of the Problem From Eq. (), Eq. (3), Eq. (4), Eq. (5), Eq. (6) and Eq. (7), we get u P v P u u v x xy y x xy P eh ee u t x tx v P u P v u v y xy x xy y eh ee Eq. (5) can be modified as u v u v K = cp +γ ij t t t x y t x y Eq. (9) and Eq. () can be solved by choosing potential functions and as u and v x y x y From Eq. (9) and (), we get ( H E P) t ( H E P) t e e e e v t y ty P t From Eq. () and Eq. (), we get ( H E ) t ( H E ) t P t e e e e (5) (9) () () () (3) (4) (6) Copyright 4 Centre for Info Bio Technology (CIBTech) 83

6 International Journal of Physics and Mathematical Sciences ISSN: 77- (Online) 4 Vol. 4 (4) October-December, pp /Kakar Eq. (3) and Eq. (5) represent magneto-electro-thermo compression waves along x- axis and y- axis respectively, whereas Eq. (4) and Eq. (6) represent magneto-electro-thermo distortional waves along x- axis and y- axis respectively. For initial stress along x- axis, the four equations (3)-(6) reduced to two equations as T T (7) c t ( H E P) t e e (8) c t where, P ( eh ee P) c and c (9) c is known as P-wave velocity and c is called SV-wave velocity. Also, for P-wave v and for SV-wave u. Now, from Eq. () and (), we get K = c p +γ ij t t t t (3) where, x y From equations (7), (8) and (3), we conclude that P-wave depends on the presence of magnetic, electric and thermal field whereas SV-wave remains unaffected which is in accordance with the GL-theory. The solution of Eq. (7), Eq. (8) and Eq. (3) is plane harmonic waves travelling perpendicular to the x-y plane, which is given as exp[ i { k ( x sin y cos ) t }] (3) exp[ i { l ( x sin y cos ) t }] (3) exp[ i { k ( x sin y cos ) t }] (33) where, k and l are compression and rotational wave numbers, is angular frequency. From Eq. (7), Eq. (9) and Eq. (33), we get c k i (34) c From Eq. (3), Eq. (3) and Eq. (33), we get i i k ic i k (35) ij p In order to satisfy Eq. (34) and Eq. (35), the determinant of the coefficients of both Eq. (34) and Eq. (35) will be zero, therefore c k i c (36) ij p i i k ic i k Copyright 4 Centre for Info Bio Technology (CIBTech) 84

7 International Journal of Physics and Mathematical Sciences ISSN: 77- (Online) 4 Vol. 4 (4) October-December, pp /Kakar Expanding Eq. (36), we get 4 i i (37) where, γ kc c c i c c,,, p p i ij i and i Eq. (37) is biquadratic in, it means that P-wave and thermal wave travel with different velocities. Therefore, on striking the SV-wave at y = making an angle in the solid half space it will have one reflected SV-wave making an angle, P-wave and thermal wave at an angle and (figure ). Therefore from the above discussion we can take displacement potential and perturbation temperature in the following form exp[ i{ k ( xsin ycos ) t}] exp[ i{ k ( xsin ycos ) t}] (39) exp[ i{ l( xsin ycos ) t}] exp[ i{ l( xsin ycos ) t}] (4) exp[ i{ k ( xsin ycos ) t}] exp[ i{ k ( xsin ycos ) t}] (4) where,, represent amplitudes of the P-wave and thermal wave, represents amplitude of incident SV wave and is the amplitude of reflected SV-waves respectively. Also,, and are related to respective wave numbers as k sin k sin l sin (4) Eq. (4) can be written in terms to Snell s law as sin sin sin (43) where, c and, c, and kc kc are the roots of equation i c c i, and are given as 4 (38) (44) Introducing Eq. (3) and Eq. (33) in into Eq. (3), we get i ij i i i i i and i ij i i i i i (45) Copyright 4 Centre for Info Bio Technology (CIBTech) 85

8 International Journal of Physics and Mathematical Sciences ISSN: 77- (Online) 4 Vol. 4 (4) October-December, pp /Kakar i ij i exp[ i{ k( xsin y cos ) t} i i i i i ij i exp[ i{ k( xsin y cos ) t}] (46) i i i i Introducing Eq. (4), Eq. (5), Eq. (6) and Eq. () in the first boundary condition of Eq. (8), we get P xy x y (47) Introducing Eq. (4), Eq. (5), Eq. (6) and Eq. () in the second boundary condition of Eq. (8), we get eh ee eh ee (48) y y xy y ty Since we have taken the upper layer is thermally insulated, therefore from the third boundary condition of Eq. (8), we get T (49) y Substituting Eq. (39) and Eq. (4) in Eq. (47) and with the help of Eq. (4) and Eq. (4), we get cos sin sin cos (5) Similarly, substituting Eq. (39), Eq. (4) and Eq. (4) in Eq. (48) and with the help of Eq. (9), Eq. (3), Eq. (4) and Eq. (43), we get ' sin sin ( sin ) i (5) sin ( sin ) ' sin i P P where, and c c Substituting Eq. (46) in Eq. (49) and with the help of Eq. (44), we get cos cos (5) i i Eliminating from Eq. (5) and Eq. (5), we get i i cos i cos cos sin cos sin Copyright 4 Centre for Info Bio Technology (CIBTech) 86 (53)

9 International Journal of Physics and Mathematical Sciences ISSN: 77- (Online) 4 Vol. 4 (4) October-December, pp /Kakar Eliminating from Eq. (5) and Eq. (5), we get i cos sin sin sin cos cos i cos sin cos i sin ' Equating Eq. (53) and Eq. (54), we get R P Equating Eq. (54) and Eq. (55), we get R SV Equating Eq. (5) and Eq. (55), we get C RP where, A, B, C and H are given as i i i i cos [ i { cos( ) ( )cos cos sin ' sin sin } cos ] cos [ { cos( ) ( )cos cos sin ' sin sin } cos ] (58) cos cos sin ' (59) C cos cos sin ' (6) cos [ { cos( ) ( )cos cos sin ' sin sin } cos ] cos [ i { cos( ) ( )cos cos sin ' sin sin } cos ] (6) R SV reflection coefficients of plane SV-wave, R P ( c ) represents reflection coefficients of thermal wave and R P ( c ) reflection coefficients of P- wave. Copyright 4 Centre for Info Bio Technology (CIBTech) 87 (54) (55) (56) (57)

10 International Journal of Physics and Mathematical Sciences ISSN: 77- (Online) 4 Vol. 4 (4) October-December, pp /Kakar Numerical Analysis and Calculations Approximate expression for reflection coefficients is obtained by assuming practical values of and for elastic materials. Solving Eq. (38) and retaining only first degree terms of and, we get T and 3 Eq. (43) can be written as sin sin,sin sin, i (6) T i cos sin sin, cos sin sin. The equations (58-6) can be written by using Eq. (63) as RP, R SV and RP (64) where, pq( ') r scos, cos sin ( ')( T ) Copyright 4 Centre for Info Bio Technology (CIBTech) 88, (63) T q sin T pq( ') r scos, p 4 sin cos T, s sin, 3 T r cos T cos sin T cos i sin. (65) From Eq. (64), we conclude that there is no P-wave in the reflection when practical values and for elastic materials are assumed. Various graphs are plotted between R, R, R and for taking S.,.3,.5,.7,.9 for SV P( c) P( c) tensile stress and S.,.3,.5,.7..9 for compressional stress. R SV, RP ( c) and RP ( c) are calculated by taking parameters for copper alloy (Table ). The results are compared with purposed model and standard model from approximation and are illustrated graphically with the help of MATLAB software. The results are closed to the standard model. The various curves are plotted by approximating the Eq. (55), Eq. (56) and (57) by considering relaxation factor and coupling factor very small, we observed that no thermal P-wave is reflected while both reflected SV-wave and reflected P-wave is seen. Figure to Figure 6 are plotted without using approximation, Figure 7 to Figure are plotted after using approximation for Eq. (64) at various incident angles. A graphical view is taken for variation of angle of incidence θ from to 4 and from to 5 ; two series are taken while plotting the graphs i.e. taking S.,.3,.5,.7,.9 for tensile stresses and S.,.3,.5,.7..9 for P compressional stresses. Here S is known as stress parameter. It is observed that SV-wave is greatly affected by the presence of magnetic field and temperature of the solid half space. Figure shows that the maxima and minima of reflection coefficients of SV-wave are in the range 3 for S.,.3,.5,.7,.9. The variation of reflection coefficients for SV reflected,

11 Reflection Coefficient SV-Wave SV-Wave International Journal of Physics and Mathematical Sciences ISSN: 77- (Online) 4 Vol. 4 (4) October-December, pp /Kakar wave in magneto-thermal medium is same for both compressional and tensile stress; the only difference is the reversal of the stress (Figure 3). Figure 4 is plotted for the reflection coefficients of P-wave, the reflection coefficient is minimum at and in figure 5, the maxima and minima of reflection coefficients of SV-wave are in the range 3. Figure 6 is plotted for reflection coefficient of thermal wave for various values of stress S.,.3,.5,.7,.9, from this figure it is clear that the maximum value of reflection coefficients of thermal waves occur at an angle of incident without using approximation. However in figure 7, the range of maxima and minima for reflection coefficients of thermal waves is 4 when approximation is used. Figure 8 shows that the maximum of reflection coefficients of SV-wave is at an angle 3 for S.,.3,.5,.7..9 after using approximation. Table Parameter Numerical Value kg / m, H 9 e.4 N/ m N/ m E 9 e 9.5 N/ m.5 6 t 6.6 K, K 4 W / ( m. K ) c.39 KJ / Kg K p 4.5 N/ m 8 Tensile Stress (Without Approximation) 6 4 S=. S=.3 S=.5 S=.7 S= Figure Copyright 4 Centre for Info Bio Technology (CIBTech) 89

12 Reflection Coefficient P-Wave Reflection Coefficient SV-Wave SV-Wave International Journal of Physics and Mathematical Sciences ISSN: 77- (Online) 4 Vol. 4 (4) October-December, pp /Kakar Similarly, Figure 9 to Figure is plotted for reflected SV, reflected P and reflected thermal wave after using approximation. Figure to Figure 4 are plotted for reflected SV, reflected P and reflected thermal wave at various values of magnetic field and electric field, keeping initial stress at.5. It is observed that in the presence of magneto-electro field, there is remarkable variation in these curves. Figures (5 7) are plotted between the reflection coefficients of P, T and SV waves against angle of incidence θ for relaxation times τ = s,.4 s,.8 s at constant H = and S =.5, it is clearly observed that the effect of relaxation time is prominent for τ =.4 s and the effect is more for increase in relaxation time. Figure 8 to Figure are plotted for reflected SV, reflected P and reflected thermal wave at various values of electric field keeping initial stress at.5. It is observed that in the presence of electric field there is remarkable variation in these curves.. Compressional Stress (Without Approximaton).8.6 S= -. S= -.3 S= -.5 S= -.7 S= Figure 3 6 Tensile Stress (Without Approximation) S=. S=.3 S=.5 S=.7 S= Figure 4 Copyright 4 Centre for Info Bio Technology (CIBTech) 9

13 Reflection Coefficient Thermal Wave Reflection Coefficient P-Wave International Journal of Physics and Mathematical Sciences ISSN: 77- (Online) 4 Vol. 4 (4) October-December, pp /Kakar 5 Compressional Stress (Without Approximation) S= -. 5 S= -.3 S= -.5 S= -.7 S= Figure 5 5 Tensile Stress (Without Approximation) 5 S=. S=.3 S=.5 S=.7 S= Figure 6 Copyright 4 Centre for Info Bio Technology (CIBTech) 9

14 Reflection Coefficient SV-Wave Reflection Coefficient SV-Wave International Journal of Physics and Mathematical Sciences ISSN: 77- (Online) 4 Vol. 4 (4) October-December, pp /Kakar Tensile Stress (After Using Approximation) S=. S=.3 S=.5 S=.7 S= Figure S= -. S= -.3 S= -.5 S= -.7 S= -.9 Compressional Stress (After Using Approximation) Figure 8 Copyright 4 Centre for Info Bio Technology (CIBTech) 9

15 Reflectin Coefficient P-Wave Reflection Coefficient P-Wave P-Wave International Journal of Physics and Mathematical Sciences ISSN: 77- (Online) 4 Vol. 4 (4) October-December, pp /Kakar Tensile Stress (After Using S=. S=.3 S=.5 S=.7 S= Incident Figure Compessional Stress (After Using Approximation) S= -. S= -.3 S= -.5 S= -.7 S= Figure Copyright 4 Centre for Info Bio Technology (CIBTech) 93

16 Reflection Coefficient SV-Wave Reflection Coefficient Thermal Wave International Journal of Physics and Mathematical Sciences ISSN: 77- (Online) 4 Vol. 4 (4) October-December, pp /Kakar 5 5 Tensile Stress (After Using Approximation) S=. S=.3 S=.5 S=.7 S= Figure S=.5 H= H= 4 H= 6 H= Figure Copyright 4 Centre for Info Bio Technology (CIBTech) 94

17 Reflection Coefficient Thermal Wave Reflection Coefficient P-Wave International Journal of Physics and Mathematical Sciences ISSN: 77- (Online) 4 Vol. 4 (4) October-December, pp /Kakar S=. H= H= 4 H= 6 H= Figure S=.5 H= H= 4 H= 6 H= Figure 4 Copyright 4 Centre for Info Bio Technology (CIBTech) 95

18 Reflection Coefficient P-Wave Reflection Coefficient Thermal Wave Wave International Journal of Physics and Mathematical Sciences ISSN: 77- (Online) 4 Vol. 4 (4) October-December, pp /Kakar Figure Figure 6 Copyright 4 Centre for Info Bio Technology (CIBTech) 96

19 Reflection Coefficient Thermal Wave Reflection Coefficient SV-Wave International Journal of Physics and Mathematical Sciences ISSN: 77- (Online) 4 Vol. 4 (4) October-December, pp /Kakar Figure S=.5 E= E= 4 E= 6 E= Figure 8 Copyright 4 Centre for Info Bio Technology (CIBTech) 97

20 Reflection Coefficient P-Wave Reflection Coefficient SV-Wave International Journal of Physics and Mathematical Sciences ISSN: 77- (Online) 4 Vol. 4 (4) October-December, pp /Kakar S=.5 E= E= 4 E= 6 E= Figure S=. E= E= 4 E= 6 E= Figure Conclusion The purpose of this study is to show the combined effect of temperature, magnetic field, electric field, relaxation time and stress on the propagation of elastic plane SV-waves through a solid isotropic elastic half space. It has been observed that in case of free space, very small energy is reflected, however in case of magneto-electro-thermal medium, the SV incident wave is greatly modifies in the presence of stress as well as magnetic field of the medium. The results are compared with purposed model and standard model using from approximation. It is clearly observed that the effect of relaxation time on reflection coefficients of P, T and SV waves is prominent for τ =.4 s and the effect is more for increase in relaxation time. The results are closed to the standard model. This model is useful to study the problems involving heat change, electromagnetic field, mechanical stress applied at the boundary of the surface. The results presented in this paper may be useful for geophysicists to analyze material structures and rocks through nondestructive testing. The solution of such problems also affects different geomagnetic cases. Copyright 4 Centre for Info Bio Technology (CIBTech) 98

21 International Journal of Physics and Mathematical Sciences ISSN: 77- (Online) 4 Vol. 4 (4) October-December, pp /Kakar ACKNOWLEDGMENT The authors are thankful to unknown reviewers for their valuable comments. REFERENCES Biot MA (965). Mechanics of Incremental Deformations (John Wiley and Sons, Inc.) New York. Chakraborty N (3). Reflection of plane elastic waves at a free surface under initial stress and temperature field, TEPE () Kakar R and Kakar S (3). Theoretical analysis of electro-magneto-thermo viscoelastic surface waves in non-homogenous solid medium subjected to gravity, compression and couple-stress, International Journal of Modern Applied Physics () Kaur R and Sharma JN (). Study of reflection and transmission of thermoelastic plane waves at liquid- solid interface, Journal of International Academy of Physical Sciences 6() 9 6. Kumar R, Garg SK and Ahuja S (3). Propagation of plane waves at the interface of an elastic solid half-space and a microstretch thermoelastic diffusion solid half-space, Latin American Journal of Solids and Structures (6) 8 8. Mehditabar A, Akbari Alashti R and Pashaei MH (4). Magneto -thermo-elastic analysis of a functionally graded conical shell, Steel and Composite Structures, an International Journal 6() Niraula OP and Wang BL (6). A magneto-electro-elastic material with a penny-shaped crack subjected to temperature loading, Acta Mechanica 87(-4) Niraula OP and Noda N (). Derivation of material constants in non-linear electro-magneto-thermo-elasticity, Journal of Thermal Stresses 33() -34. Othman MIA (). Generalized electro-magneto-thermoelasticity in case of thermal shock plane waves for a finite conducting half-space with two relaxation times, Mechanics and Mechanical Engineering 4() 5-3. Othman MIA and Song Y (). Reflection of magneto thermo-elastic waves from a rotating elastic half-space in generalized thermoelasticity under three theories, Mechanics and Mechanical Engineering 5() 5-4. Shekhar S and Parvez IA (3). Effect of rotation, magnetic field and initial stresses on propagation of plane waves in transversely isotropic dissipative half space, Applied Mathematics Singh B and Bala K (). Reflection of P and SV waves from the free surface of a two-temperature thermoelastic solid half-space, Journal of Mechanics of Materials and Structures 7() Singh B and Yadav AK (). Reflection of plane waves in a rotating transversely isotropic magneto-thermoelastic solid half-space, Journal of Theoretical and Applied Mechanics 4(3) Ya J, Xiao G and Tian JL (3). Fractional order generalized electro-magneto-thermo-elasticity, European Journal of Mechanics Copyright 4 Centre for Info Bio Technology (CIBTech) 99

Reflection of SV- Waves from the Free Surface of a. Magneto-Thermoelastic Isotropic Elastic. Half-Space under Initial Stress

Reflection of SV- Waves from the Free Surface of a. Magneto-Thermoelastic Isotropic Elastic. Half-Space under Initial Stress Mathematica Aeterna, Vol. 4, 4, no. 8, 877-93 Reflection of SV- Waves from the Free Surface of a Magneto-Thermoelastic Isotropic Elastic Half-Space under Initial Stress Rajneesh Kakar Faculty of Engineering

More information

International Journal of Pure and Applied Sciences and Technology

International Journal of Pure and Applied Sciences and Technology Int. J. Pure Appl. Sci. Technol., 3() (0), pp. 7-39 International Journal of Pure and Applied Sciences and Technology ISSN 9-607 Available online at www.ijopaasat.in Research Paper Reflection of Quasi

More information

Reflection of Plane Waves from a Rotating Magneto Thermoelastic Medium with Two Temperature and Initial Srtress Under Three Theories

Reflection of Plane Waves from a Rotating Magneto Thermoelastic Medium with Two Temperature and Initial Srtress Under Three Theories Mechanics and Mechanical Engineering Vol. 21, No. 2 (2017) 217 232 c Lodz University of Technology Reflection of Plane Waves from a Rotating Magneto Thermoelastic Medium with Two Temperature and Initial

More information

Stoneley Waves at the Boundary Surface of Modified Couple Stress Generalized Thermoelastic with Mass Diffusion

Stoneley Waves at the Boundary Surface of Modified Couple Stress Generalized Thermoelastic with Mass Diffusion Journal of Applied Science and Engineering, Vol. 21, No. 1, pp. 18 (2018) DOI: 10.6180/jase.201803_21(1).0001 Stoneley Waves at the Boundary Surface of Modified Couple Stress Generalized Thermoelastic

More information

Research Article Reflection of Plane Waves in Generalized Thermoelastic Half Space under the Action of Uniform Magnetic Field

Research Article Reflection of Plane Waves in Generalized Thermoelastic Half Space under the Action of Uniform Magnetic Field International Engineering Mathematics Volume 2016 Article ID 4954063 9 pages http://dx.doi.org/10.1155/2016/4954063 Research Article Reflection of Plane Waves in Generalized Thermoelastic alf Space under

More information

DAMPING OF GENERALIZED THERMO ELASTIC WAVES IN A HOMOGENEOUS ISOTROPIC PLATE

DAMPING OF GENERALIZED THERMO ELASTIC WAVES IN A HOMOGENEOUS ISOTROPIC PLATE Materials Physics and Mechanics 4 () 64-73 Received: April 9 DAMPING OF GENERALIZED THERMO ELASTIC WAVES IN A HOMOGENEOUS ISOTROPIC PLATE R. Selvamani * P. Ponnusamy Department of Mathematics Karunya University

More information

21. Fractional order magneto-thermoelasticity in a rotating media with one relaxation time

21. Fractional order magneto-thermoelasticity in a rotating media with one relaxation time 21. Fractional order magneto-thermoelasticity in a rotating media with one relaxation time M. Bachher 1, N. Sarkar 2 1 Media Girl s High School, Gobardanga, 24-Pgs (N), West Bengal, India 2 Department

More information

Available online Journal of Scientific and Engineering Research, 2016, 3(6): Research Article

Available online  Journal of Scientific and Engineering Research, 2016, 3(6): Research Article vailable online www.jsaer.com 6 (6):88-99 Research rticle IN: 9-6 CODEN(U): JERBR -D Problem of Generalized Thermoelastic Medium with Voids under the Effect of Gravity: Comparison of Different Theories

More information

Some Consideration in Microstretch Thermoelastic Diffusive Medium with Mass Diffusion-A Review

Some Consideration in Microstretch Thermoelastic Diffusive Medium with Mass Diffusion-A Review 2014 1 st International Congress on Computer, Electronics, Electrical, and Communication Engineering (ICCEECE2014) IPCSIT vol. 59 (2014) (2014) IACSIT Press, Singapore DOI: 10.7763/IPCSIT.2014.V59.17 Some

More information

Reflection and refraction of thermoelastic plane waves at an interface between two thermoelastic media without energy dissipation

Reflection and refraction of thermoelastic plane waves at an interface between two thermoelastic media without energy dissipation Arch. Mech., 58, 1, pp. 155 185, Warszawa 006 Reflection and refraction of thermoelastic plane waves at an interface between two thermoelastic media without energy dissipation RAJNEESH KUMAR, PARTH SARTHI

More information

EFFECT OF DISTINCT CONDUCTIVE AND THERMODYNAMIC TEMPERATURES ON THE REFLECTION OF PLANE WAVES IN MICROPOLAR ELASTIC HALF-SPACE

EFFECT OF DISTINCT CONDUCTIVE AND THERMODYNAMIC TEMPERATURES ON THE REFLECTION OF PLANE WAVES IN MICROPOLAR ELASTIC HALF-SPACE U.P.B. Sci. Bull., Series A, Vol. 75, Iss. 2, 23 ISSN 223-727 EFFECT OF DISTINCT CONDUCTIVE AND THERMODYNAMIC TEMPERATURES ON THE REFLECTION OF PLANE WAVES IN MICROPOLAR ELASTIC HALF-SPACE Kunal SHARMA,

More information

Chapter I. Introduction

Chapter I. Introduction 1 Chapter I Introduction Elasticity is the branch of Physics which deals with analysis of stress and strain. A material is said to be elastic, which deforms under stress and returns to its original shape

More information

Effect of Thermal Stress and Magnetic Field on Propagation of Transverse Wave in an Anisotropic Incompressible Dissipative Initially Stressed Plate

Effect of Thermal Stress and Magnetic Field on Propagation of Transverse Wave in an Anisotropic Incompressible Dissipative Initially Stressed Plate Appl. Math. Inf. Sci. 11, No. 1, 195-00 (017) 195 Applied Mathematics & Information Sciences An International Journal http://dx.doi.org/10.18576/amis/11014 Effect of Thermal Stress and Magnetic Field on

More information

PEAT SEISMOLOGY Lecture 9: Anisotropy, attenuation and anelasticity

PEAT SEISMOLOGY Lecture 9: Anisotropy, attenuation and anelasticity PEAT8002 - SEISMOLOGY Lecture 9: Anisotropy, attenuation and anelasticity Nick Rawlinson Research School of Earth Sciences Australian National University Anisotropy Introduction Most of the theoretical

More information

ISSN: X (p); (e)

ISSN: X (p); (e) TORSIONA SURFACE WAVE IN SEF-REINFORCED AYER SANDWICHED BETWEEN TWO VISCO-EASIC HAF-SPACES UNDER THE INITIA STRESS Nidhi Dewangan, Sanjeev A. Sahu and Soniya Chaudhary S.G.G. Govt P.G. College, Kurud,

More information

Mathematical Model for Thermal Shock Problem of a Generalized Thermoelastic Layered Composite Material with Variable Thermal Conductivity

Mathematical Model for Thermal Shock Problem of a Generalized Thermoelastic Layered Composite Material with Variable Thermal Conductivity COMPUTATIONAL METHODS IN SCIENCE AND TECHNOLOGY ( 65-7 (6 Mathematical Model for Thermal Shock Problem of a Generalized Thermoelastic Layered Composite Material with Variable Thermal Conductivity H. M.

More information

THE REFLECTION PHENOMENA OF SV-WAVES IN A GENERALIZED THERMOELASTIC MEDIUM

THE REFLECTION PHENOMENA OF SV-WAVES IN A GENERALIZED THERMOELASTIC MEDIUM Internat. J. Math. & Math. Sci. Vol., No. 8 () 59 56 S67 Hindawi Publishing Corp. THE REFLECTION PHENOMENA OF SV-WAVES IN A GENERALIZED THERMOELASTIC MEDIUM ABO-EL-NOUR N. ABD-ALLA and AMIRA A. S. AL-DAWY

More information

Propagation and Reflection of Plane Waves in a Rotating Magneto Elastic Fibre Reinforced Semi Space with Surface Stress

Propagation and Reflection of Plane Waves in a Rotating Magneto Elastic Fibre Reinforced Semi Space with Surface Stress Mechanics and Mechanical Engineering Vol. 21, No. 4 (2017) 1043 1061 c Lodz University of Technology Propagation and Reflection of Plane Waves in a Rotating Magneto Elastic Fibre Reinforced Semi Space

More information

Internal Heat Source in Temperature Rate Dependent Thermoelastic Medium with Hydrostatic Initial Stress

Internal Heat Source in Temperature Rate Dependent Thermoelastic Medium with Hydrostatic Initial Stress Mechanics and Mechanical Engineering Vol. 20, No. 3 (2016) 263 277 c Lodz University of Technology Internal Heat Source in Temperature Rate Dependent Thermoelastic Medium with Hydrostatic Initial Stress

More information

PROPAGATION OF WAVES AT AN IMPERFECTLY

PROPAGATION OF WAVES AT AN IMPERFECTLY Journal of Theoretical and Applied Mechanics, Sofia, 2011, vol. 41, No. 3, pp. 77 92 PROPAGATION OF WAVES AT AN IMPERFECTLY BONDED INTERFACE BETWEEN TWO MONOCLINIC THERMOELASTIC HALF-SPACES Joginder Singh

More information

Receiver. Johana Brokešová Charles University in Prague

Receiver. Johana Brokešová Charles University in Prague Propagation of seismic waves - theoretical background Receiver Johana Brokešová Charles University in Prague Seismic waves = waves in elastic continuum a model of the medium through which the waves propagate

More information

LECTURE 5 - Wave Equation Hrvoje Tkalčić " 2 # & 2 #

LECTURE 5 - Wave Equation Hrvoje Tkalčić  2 # & 2 # LECTURE 5 - Wave Equation Hrvoje Tkalčić " 2 # "t = ( $ + 2µ ) & 2 # 2 % " 2 (& ' u r ) = µ "t 2 % & 2 (& ' u r ) *** N.B. The material presented in these lectures is from the principal textbooks, other

More information

Dr. Parveen Lata Department of Basic and Applied Sciences, Punjabi University, Patiala, Punjab, India.

Dr. Parveen Lata Department of Basic and Applied Sciences, Punjabi University, Patiala, Punjab, India. International Journal of Theoretical and Applied Mechanics. ISSN 973-685 Volume 12, Number 3 (217) pp. 435-443 Research India Publications http://www.ripublication.com Linearly Distributed Time Harmonic

More information

Propagation of Plane Waves in Micro-stretch Elastic Solid in Special Case

Propagation of Plane Waves in Micro-stretch Elastic Solid in Special Case Global Journal of Pure and Applied Mathematics. ISSN 973-768 Volume 3, Number 6 (7), pp. 43-5 Research India Publications http://www.ripublication.com Propagation of Plane Waves in Micro-stretch Elastic

More information

PEAT SEISMOLOGY Lecture 2: Continuum mechanics

PEAT SEISMOLOGY Lecture 2: Continuum mechanics PEAT8002 - SEISMOLOGY Lecture 2: Continuum mechanics Nick Rawlinson Research School of Earth Sciences Australian National University Strain Strain is the formal description of the change in shape of a

More information

Research Article Dispersion of Love Waves in a Composite Layer Resting on Monoclinic Half-Space

Research Article Dispersion of Love Waves in a Composite Layer Resting on Monoclinic Half-Space Applied Mathematics Volume 011, Article ID 71349, 9 pages doi:10.1155/011/71349 Research Article Dispersion of Love Waves in a Composite Layer Resting on Monoclinic Half-Space Sukumar Saha BAS Division,

More information

INITIAL STRESS AT THE EARTH S CORE-MANTLE BOUNDARY

INITIAL STRESS AT THE EARTH S CORE-MANTLE BOUNDARY I nternat. J. Math. & Math. Si. Vol. 3 No. 3 (1980) 591-598 591 REFLECTION AND TRANSMISSION OF SEISMIC WAVES UNDER INITIAL STRESS AT THE EARTH S CORE-MANTLE BOUNDARY SUKHENDU DEY and SUSHIL KUMAR ADDY

More information

Effect of Rotation and Initial Magnetic Field in Fibre-Reinforced Anisotropic Elastic Media

Effect of Rotation and Initial Magnetic Field in Fibre-Reinforced Anisotropic Elastic Media Applied Mathematics, 05, 6, 877-898 Published Online May 05 in SciRes. http://www.scirp.org/journal/am http://dx.doi.org/0.436/am.05.6508 Effect of Rotation and Initial Magnetic Field in Fibre-Reinforced

More information

Thermal Effects on Propagation of Transverse Waves in Anisotropic Incompressible Dissipative Pre-Stressed Plate

Thermal Effects on Propagation of Transverse Waves in Anisotropic Incompressible Dissipative Pre-Stressed Plate Appl. Math. Inf. Sci. 0, No. 3, 09-095 (206) 09 Applied Mathematics & Information Sciences An International Journal http://dx.doi.org/0.8576/amis/00327 Thermal Effects on Propagation of Transverse Waves

More information

PEAT SEISMOLOGY Lecture 12: Earthquake source mechanisms and radiation patterns II

PEAT SEISMOLOGY Lecture 12: Earthquake source mechanisms and radiation patterns II PEAT8002 - SEISMOLOGY Lecture 12: Earthquake source mechanisms and radiation patterns II Nick Rawlinson Research School of Earth Sciences Australian National University Waveform modelling P-wave first-motions

More information

The effect of a laser pulse and gravity field on a thermoelastic medium under Green Naghdi theory

The effect of a laser pulse and gravity field on a thermoelastic medium under Green Naghdi theory Acta Mech 7, 3571 3583 016 DOI 10.1007/s00707-016-1683-5 ORIGINAL PAPER Mohamed I. A. Othman Ramadan S. Tantawi The effect of a laser pulse and gravity field on a thermoelastic medium under Green Naghdi

More information

(a) Show that the amplitudes of the reflected and transmitted waves, corrrect to first order

(a) Show that the amplitudes of the reflected and transmitted waves, corrrect to first order Problem 1. A conducting slab A plane polarized electromagnetic wave E = E I e ikz ωt is incident normally on a flat uniform sheet of an excellent conductor (σ ω) having thickness D. Assume that in space

More information

Modeling of Variable Lamé s Modulii for a FGM Generalized Thermoelastic Half Space

Modeling of Variable Lamé s Modulii for a FGM Generalized Thermoelastic Half Space 75 Modeling of Variable Lamé s Modulii for a FGM Generalized Thermoelastic Half Space Abstract In this work we consider a problem in the contet of the generalized theory of thermoelasticity for a half

More information

Mathematical modelling of Stoneley wave in a transversely isotropic thermoelastic media

Mathematical modelling of Stoneley wave in a transversely isotropic thermoelastic media Available at http://pvamu.edu/aam Appl. Appl. Math. ISSN: 1932-9466 Vol. 12, Issue 1 (June 2017), pp. 319-336 Applications and Applied Mathematics: An International Journal (AAM) Mathematical modelling

More information

EFFECT OF COUPLE-STRESS ON THE REFLECTION AND TRANSMISSION OF PLANE WAVES AT AN INTERFACE

EFFECT OF COUPLE-STRESS ON THE REFLECTION AND TRANSMISSION OF PLANE WAVES AT AN INTERFACE International Journal of Modern Engineering Research (IJMER) www.ijmer.com Vol., Issue, pp-5-8 ISSN: 9-665 EFFET OF OUPLE-STRESS ON THE REFLETION AND TRANSMISSION OF PLANE WAVES AT AN INTERFAE Mahabir

More information

7.2.1 Seismic waves. Waves in a mass- spring system

7.2.1 Seismic waves. Waves in a mass- spring system 7..1 Seismic waves Waves in a mass- spring system Acoustic waves in a liquid or gas Seismic waves in a solid Surface waves Wavefronts, rays and geometrical attenuation Amplitude and energy Waves in a mass-

More information

COPYRIGHTED MATERIAL. Index

COPYRIGHTED MATERIAL. Index Index A Admissible function, 163 Amplification factor, 36 Amplitude, 1, 22 Amplitude-modulated carrier, 630 Amplitude ratio, 36 Antinodes, 612 Approximate analytical methods, 647 Assumed modes method,

More information

Plane waves in a rotating generalized thermo-elastic solid with voids

Plane waves in a rotating generalized thermo-elastic solid with voids MultiCraft International Journal of Engineering, Science and Technology Vol. 3, No. 2, 2011, pp. 34-41 INTERNATIONAL JOURNAL OF ENGINEERING, SCIENCE AND TECHNOLOGY www.ijest-ng.com 2011 MultiCraft Limited.

More information

The Effect of Heat Laser Pulse on Generalized Thermoelasticity for Micropolar Medium

The Effect of Heat Laser Pulse on Generalized Thermoelasticity for Micropolar Medium Mechanics and Mechanical Engineering Vol. 21, No. 4 (2017) 797 811 c Lodz University of Technology The Effect of Heat Laser Pulse on Generalized Thermoelasticity for Micropolar Medium Mohamed I. A. Othman

More information

Propagation of Rayleigh Wave in Two Temperature Dual Phase Lag Thermoelasticity

Propagation of Rayleigh Wave in Two Temperature Dual Phase Lag Thermoelasticity Mechanics and Mechanical Engineering Vol. 21, No. 1 (2017) 105 116 c Lodz University of Technology Propagation of Rayleigh Wave in Two Temperature Dual Phase Lag Thermoelasticity Baljeet Singh Department

More information

Sound Propagation through Media. Nachiketa Tiwari Indian Institute of Technology Kanpur

Sound Propagation through Media. Nachiketa Tiwari Indian Institute of Technology Kanpur Sound Propagation through Media Nachiketa Tiwari Indian Institute of Technology Kanpur LECTURE-13 WAVE PROPAGATION IN SOLIDS Longitudinal Vibrations In Thin Plates Unlike 3-D solids, thin plates have surfaces

More information

Time Harmonic Inclined Load in Micropolar Thermoelastic Medium Possesing Cubic Symmetry with One Relaxation Time

Time Harmonic Inclined Load in Micropolar Thermoelastic Medium Possesing Cubic Symmetry with One Relaxation Time Tamkang Journal of Science and Engineering, Vol. 13, No. 2, pp. 117 126 (2010) 117 Time Harmonic Inclined Load in Micropolar Thermoelastic Medium Possesing Cubic Symmetry with One Relaxation Time Praveen

More information

Mechanics of Earthquakes and Faulting

Mechanics of Earthquakes and Faulting Mechanics of Earthquakes and Faulting www.geosc.psu.edu/courses/geosc508 Standard Solids and Fracture Fluids: Mechanical, Chemical Effects Effective Stress Dilatancy Hardening and Stability Mead, 1925

More information

Model tests and FE-modelling of dynamic soil-structure interaction

Model tests and FE-modelling of dynamic soil-structure interaction Shock and Vibration 19 (2012) 1061 1069 1061 DOI 10.3233/SAV-2012-0712 IOS Press Model tests and FE-modelling of dynamic soil-structure interaction N. Kodama a, * and K. Komiya b a Waseda Institute for

More information

Elements of Rock Mechanics

Elements of Rock Mechanics Elements of Rock Mechanics Stress and strain Creep Constitutive equation Hooke's law Empirical relations Effects of porosity and fluids Anelasticity and viscoelasticity Reading: Shearer, 3 Stress Consider

More information

Reflection of quasi-p and quasi-sv waves at the free and rigid boundaries of a fibre-reinforced medium

Reflection of quasi-p and quasi-sv waves at the free and rigid boundaries of a fibre-reinforced medium Sādhan ā Vol. 7 Part 6 December 00 pp. 63 630. Printed in India Reflection of quasi-p and quasi-sv waves at the free and rigid boundaries of a fibre-reinforced medium A CHATTOPADHYAYRLKVENKATESWARLU and

More information

Electromagnetic fields and waves

Electromagnetic fields and waves Electromagnetic fields and waves Maxwell s rainbow Outline Maxwell s equations Plane waves Pulses and group velocity Polarization of light Transmission and reflection at an interface Macroscopic Maxwell

More information

Thermoelastic Interactions without Energy Dissipation Due to Inclined Load

Thermoelastic Interactions without Energy Dissipation Due to Inclined Load Tamkang Journal of Science and Engineering, Vol. 11, No. 2, pp. 109 118 (2008) 109 Thermoelastic Interactions without Energy Dissipation Due to Inclined Load Rajneesh Kumar 1 * and Leena Rani 2 1 Department

More information

PLEASE SCROLL DOWN FOR ARTICLE

PLEASE SCROLL DOWN FOR ARTICLE This article was downloaded by:[youssef, Hamdy M.] On: 22 February 2008 Access Details: [subscription number 790771681] Publisher: Taylor & Francis Informa Ltd Registered in England and Wales Registered

More information

Available online at ScienceDirect. Procedia Engineering 144 (2016 )

Available online at  ScienceDirect. Procedia Engineering 144 (2016 ) Available online at www.sciencedirect.com ScienceDirect Procedia Engineering 144 (016 ) 170 177 1th International Conference on Vibration Problems, ICOVP 015 Propagation of Torsional Surface Wave in Anisotropic

More information

On the study of elastic wave scattering and Rayleigh wave velocity measurement of concrete with steel bar

On the study of elastic wave scattering and Rayleigh wave velocity measurement of concrete with steel bar NDT&E International 33 (2000) 401 407 www.elsevier.com/locate/ndteint On the study of elastic wave scattering and Rayleigh wave velocity measurement of concrete with steel bar T.-T. Wu*, J.-H. Sun, J.-H.

More information

Comparison between the visco-elastic dampers And Magnetorheological dampers and study the Effect of temperature on the damping properties

Comparison between the visco-elastic dampers And Magnetorheological dampers and study the Effect of temperature on the damping properties Comparison between the visco-elastic dampers And Magnetorheological dampers and study the Effect of temperature on the damping properties A.Q. Bhatti National University of Sciences and Technology (NUST),

More information

Wave Propagation in Anisotropic, Anelastic, Porous and Electromagnetic Media

Wave Propagation in Anisotropic, Anelastic, Porous and Electromagnetic Media SECTION I. SEISMIC EXPLORATION Volume 38 WAVE FIELDS IN REAL MEDIA: Wave Propagation in Anisotropic, Anelastic, Porous and Electromagnetic Media (SECOND EDITION, REVISED AND EXTENDED) by Jose M. CARCIONE

More information

Conversion coefficients at a liquid/solid interface

Conversion coefficients at a liquid/solid interface Conversion coefficients at a liquid/solid interface P.F. aley Conversion coefficients ABSTACT When upward-propagating rays transporting seismic energy are recorded at the earth s surface, the vertical

More information

Wave Propagation in Uniaxial Media. Reflection and Transmission at Interfaces

Wave Propagation in Uniaxial Media. Reflection and Transmission at Interfaces Lecture 5: Crystal Optics Outline 1 Homogeneous, Anisotropic Media 2 Crystals 3 Plane Waves in Anisotropic Media 4 Wave Propagation in Uniaxial Media 5 Reflection and Transmission at Interfaces Christoph

More information

The effect of rotation on plane waves in generalized thermo-microstretch elastic solid with one relaxation time for a mode-i crack problem

The effect of rotation on plane waves in generalized thermo-microstretch elastic solid with one relaxation time for a mode-i crack problem The effect of rotation on plane waves in generalized thermo-microstretch elastic solid with one relaxation time for a mode-i crack problem Kh. Lotfy a)b) and Mohamed I. A. Othman a) a) Department of Mathematics,

More information

J10M.1 - Rod on a Rail (M93M.2)

J10M.1 - Rod on a Rail (M93M.2) Part I - Mechanics J10M.1 - Rod on a Rail (M93M.2) J10M.1 - Rod on a Rail (M93M.2) s α l θ g z x A uniform rod of length l and mass m moves in the x-z plane. One end of the rod is suspended from a straight

More information

We briefly discuss two examples for solving wave propagation type problems with finite differences, the acoustic and the seismic problem.

We briefly discuss two examples for solving wave propagation type problems with finite differences, the acoustic and the seismic problem. Excerpt from GEOL557 Numerical Modeling of Earth Systems by Becker and Kaus 2016 1 Wave propagation Figure 1: Finite difference discretization of the 2D acoustic problem. We briefly discuss two examples

More information

The effect of rigidity on torsional vibrations in a two layered poroelastic cylinder

The effect of rigidity on torsional vibrations in a two layered poroelastic cylinder Int. J. Adv. Appl. Math. and Mech. 3(1) (2015) 116 121 (ISSN: 2347-2529) Journal homepage: www.ijaamm.com International Journal of Advances in Applied Mathematics and Mechanics The effect of rigidity on

More information

NDT&E Methods: UT. VJ Technologies CAVITY INSPECTION. Nondestructive Testing & Evaluation TPU Lecture Course 2015/16.

NDT&E Methods: UT. VJ Technologies CAVITY INSPECTION. Nondestructive Testing & Evaluation TPU Lecture Course 2015/16. CAVITY INSPECTION NDT&E Methods: UT VJ Technologies NDT&E Methods: UT 6. NDT&E: Introduction to Methods 6.1. Ultrasonic Testing: Basics of Elasto-Dynamics 6.2. Principles of Measurement 6.3. The Pulse-Echo

More information

Basic Equations of Elasticity

Basic Equations of Elasticity A Basic Equations of Elasticity A.1 STRESS The state of stress at any point in a loaded bo is defined completely in terms of the nine components of stress: σ xx,σ yy,σ zz,σ xy,σ yx,σ yz,σ zy,σ zx,andσ

More information

WINTER 16 EXAMINATION

WINTER 16 EXAMINATION Model ject Code: Important Instructions to examiners: ) The answers should be examined by key words and not as word-to-word as given in the model answer scheme. ) The model answer and the answer written

More information

Physics and Chemistry of the Earth and Terrestrial Planets

Physics and Chemistry of the Earth and Terrestrial Planets MIT OpenCourseWare http://ocw.mit.edu 12.002 Physics and Chemistry of the Earth and Terrestrial Planets Fall 2008 For information about citing these materials or our Terms of Use, visit: http://ocw.mit.edu/terms.

More information

Soil Damping Ratio: Theoretical Aspect and Measurement

Soil Damping Ratio: Theoretical Aspect and Measurement Ratio: Theoretical Aspect and Measurement Sri Atmaja P. Rosyidi, Ph.D. Assistant Professor, Universitas Muhammadiyah Yogyakarta A Two Day Workshop on SASW for Practicing Engineer 17-18 February 2011, Faculty

More information

ERTH2020 Introduction to Geophysics The Seismic Method. 1. Basic Concepts in Seismology. 1.1 Seismic Wave Types

ERTH2020 Introduction to Geophysics The Seismic Method. 1. Basic Concepts in Seismology. 1.1 Seismic Wave Types ERTH2020 Introduction to Geophysics The Seismic Method 1. Basic Concepts in Seismology 1.1 Seismic Wave Types Existence of different wave types The existence of different seismic wave types can be understood

More information

REFLECTIONOFPLANEWAVESFROMAFREESURFACEOF A GENERALIZED MAGNETO-THERMOELASTIC SOLID HALF-SPACE WITH DIFFUSION

REFLECTIONOFPLANEWAVESFROMAFREESURFACEOF A GENERALIZED MAGNETO-THERMOELASTIC SOLID HALF-SPACE WITH DIFFUSION JOURNAL OF THEORETICAL AND APPLIED MECHANICS 52, 2, pp. 385-394, Warsaw 2014 REFLECTIONOFPLANEWAVESFROMAFREESURFACEOF A GENERALIZED MAGNETO-THERMOELASTIC SOLID HALF-SPACE WITH DIFFUSION Baljeet Singh Post

More information

SURFACE WAVE MODELLING USING SEISMIC GROUND RESPONSE ANALYSIS

SURFACE WAVE MODELLING USING SEISMIC GROUND RESPONSE ANALYSIS 43 SURFACE WAVE MODELLING USING SEISMIC GROUND RESPONSE ANALYSIS E John MARSH And Tam J LARKIN SUMMARY This paper presents a study of surface wave characteristics using a two dimensional nonlinear seismic

More information

Dispersion of Love Wave in a Fiber-Reinforced Medium Lying Over a Heterogeneous Half-Space with Rectangular Irregularity

Dispersion of Love Wave in a Fiber-Reinforced Medium Lying Over a Heterogeneous Half-Space with Rectangular Irregularity Journal of Solid Mechanics Vol. 10, No. 3 (018) pp. 591-60 Dispersion of ove Wave in a Fiber-Reinforced Medium ying Over a Heterogeneous Half-Space with Rectangular Irregularity R.M. Prasad 1,*, S. Kundu

More information

Main Menu. Summary. Introduction

Main Menu. Summary. Introduction Kyosuke Okamoto *, JSPS Research Fellow, Kyoto University; Ru-shan Wu, University of California, Santa Cruz; Hitoshi Mikada, Tada-nori Goto, Junichi Takekawa, Kyoto University Summary Coda-Q is a stochastic

More information

Lecture 21 Reminder/Introduction to Wave Optics

Lecture 21 Reminder/Introduction to Wave Optics Lecture 1 Reminder/Introduction to Wave Optics Program: 1. Maxwell s Equations.. Magnetic induction and electric displacement. 3. Origins of the electric permittivity and magnetic permeability. 4. Wave

More information

D scattering of obliquely incident Rayleigh waves by a saturated alluvial valley in a layered half-space

D scattering of obliquely incident Rayleigh waves by a saturated alluvial valley in a layered half-space 1842. 3-D scattering of obliquely incident Rayleigh waves by a saturated alluvial valley in a layered half-space Zhenning Ba 1, Jianwen Liang 2 Department of Civil Engineering, Tianjin University, Tianjin

More information

CHAPTER 9 ELECTROMAGNETIC WAVES

CHAPTER 9 ELECTROMAGNETIC WAVES CHAPTER 9 ELECTROMAGNETIC WAVES Outlines 1. Waves in one dimension 2. Electromagnetic Waves in Vacuum 3. Electromagnetic waves in Matter 4. Absorption and Dispersion 5. Guided Waves 2 Skip 9.1.1 and 9.1.2

More information

Wave Propagation in Fractured Poroelastic Media

Wave Propagation in Fractured Poroelastic Media Wave Propagation in Fractured Poroelastic Media WCCM, MS170: Advanced Computational Techniques in Geophysical Sciences, Barcelona, Spain, July 2014 Juan E. Santos Instituto del Gas y del Petróleo (IGPUBA),

More information

3D Elasticity Theory

3D Elasticity Theory 3D lasticity Theory Many structural analysis problems are analysed using the theory of elasticity in which Hooke s law is used to enforce proportionality between stress and strain at any deformation level.

More information

Introduction to Polarization

Introduction to Polarization Phone: Ext 659, E-mail: hcchui@mail.ncku.edu.tw Fall/007 Introduction to Polarization Text Book: A Yariv and P Yeh, Photonics, Oxford (007) 1.6 Polarization States and Representations (Stokes Parameters

More information

LASER GENERATED THERMOELASTIC WAVES IN AN ANISOTROPIC INFINITE PLATE

LASER GENERATED THERMOELASTIC WAVES IN AN ANISOTROPIC INFINITE PLATE LASER GENERATED THERMOELASTIC WAVES IN AN ANISOTROPIC INFINITE PLATE H. M. Al-Qahtani and S. K. Datta University of Colorado Boulder CO 839-7 ABSTRACT. An analysis of the propagation of thermoelastic waves

More information

TWO DIMENSIONAL DISLOCATION SOURCES IN FIBER COMPOSITE LAMINATES

TWO DIMENSIONAL DISLOCATION SOURCES IN FIBER COMPOSITE LAMINATES TWO DIMENSIONAL DISLOCATION SOURCES IN FIBER COMPOSITE LAMINATES E. Rhian Green Department of Engineering Leicester University Leicester LEI 7RH U.K. INTRODUCTION The method which is frequently adopted

More information

ON THE MODELING AND SIMULATION OF AN ACOUSTIC CLOAK

ON THE MODELING AND SIMULATION OF AN ACOUSTIC CLOAK 5 th International Conference Advanced Composite Materials Engineering COMAT 014 16-17 October 014, Braşov, Romania ON THE MODELING AND SIMULATION OF AN ACOUSTIC CLOAK Veturia Chiroiu 1, Rodica Ioan 1,,

More information

6.730 Physics for Solid State Applications

6.730 Physics for Solid State Applications 6.730 Physics for Solid State Applications Lecture 5: Specific Heat of Lattice Waves Outline Review Lecture 4 3-D Elastic Continuum 3-D Lattice Waves Lattice Density of Modes Specific Heat of Lattice Specific

More information

NYS STANDARD/KEY IDEA/PERFORMANCE INDICATOR 5.1 a-e. 5.1a Measured quantities can be classified as either vector or scalar.

NYS STANDARD/KEY IDEA/PERFORMANCE INDICATOR 5.1 a-e. 5.1a Measured quantities can be classified as either vector or scalar. INDICATOR 5.1 a-e September Unit 1 Units and Scientific Notation SI System of Units Unit Conversion Scientific Notation Significant Figures Graphical Analysis Unit Kinematics Scalar vs. vector Displacement/dis

More information

EE485 Introduction to Photonics. Introduction

EE485 Introduction to Photonics. Introduction EE485 Introduction to Photonics Introduction Nature of Light They could but make the best of it and went around with woebegone faces, sadly complaining that on Mondays, Wednesdays, and Fridays, they must

More information

Grade XI. Physics Exam Preparation Booklet. Chapter-wise Important Questions. #GrowWithGreen

Grade XI. Physics Exam Preparation Booklet. Chapter-wise Important Questions. #GrowWithGreen Grade XI Physics Exam Preparation Booklet Chapter-wise Important Questions #GrowWithGreen Units and Measurements Q1. After reading the physics book, Anamika recalled and noted down the expression for the

More information

Surface Waves and Free Oscillations. Surface Waves and Free Oscillations

Surface Waves and Free Oscillations. Surface Waves and Free Oscillations Surface waves in in an an elastic half spaces: Rayleigh waves -Potentials - Free surface boundary conditions - Solutions propagating along the surface, decaying with depth - Lamb s problem Surface waves

More information

Speed of Light in Glass

Speed of Light in Glass Experiment (1) Speed of Light in Glass Objective:- This experiment is used to determine the speed of propagation of light waves in glass. Apparatus:- Prism, spectrometer, Halogen lamp source. Theory:-

More information

Reflection of plane micropolar viscoelastic waves at a loosely bonded solid solid interface

Reflection of plane micropolar viscoelastic waves at a loosely bonded solid solid interface Sādhan ā Vol. 27, Part 5, October 22, pp. 493 56. Printed in India Reflection of plane micropolar viscoelastic waves at a loosely bonded solid solid interface BALJEET SINGH Mathematics Department, Jat

More information

Generalized Magneto-thermo-microstretch Response of a Half-space with Temperature-dependent Properties During Thermal Shock

Generalized Magneto-thermo-microstretch Response of a Half-space with Temperature-dependent Properties During Thermal Shock 2562 Generalized Magneto-thermo-microstretch Response of a Half-space with Temperature-dependent Properties During Thermal Shock Abstract The generalized magneto-thermoelastic problem of an infinite homogeneous

More information

Source Free Surface x

Source Free Surface x Finite-dierence time-domain model for elastic waves in the ground Christoph T. Schroeder and Waymond R. Scott, Jr. School of Electrical and Computer Engineering Georgia Institute of Technology Atlanta,

More information

Saturation Effects of Soils on Ground Motion at Free Surface Due to Incident SV Waves

Saturation Effects of Soils on Ground Motion at Free Surface Due to Incident SV Waves Saturation Effects of Soils on Ground Motion at Free Surface Due to Incident SV Waves Jun Yang, M.ASCE 1 Abstract: A study is presented of saturation effects of subsoil on seismic motions at the free surface

More information

Add-on unidirectional elastic metamaterial plate cloak

Add-on unidirectional elastic metamaterial plate cloak Add-on unidirectional elastic metamaterial plate cloak Min Kyung Lee *a and Yoon Young Kim **a,b a Department of Mechanical and Aerospace Engineering, Seoul National University, Gwanak-ro, Gwanak-gu, Seoul,

More information

Research Article Propagation of Plane Waves in a Thermally Conducting Mixture

Research Article Propagation of Plane Waves in a Thermally Conducting Mixture International Scholarly Research Network ISRN Applied Mathematics Volume 211, Article ID 31816, 12 pages doi:1.542/211/31816 Research Article Propagation of Plane Waves in a Thermally Conducting Mixture

More information

Mechanics PhD Preliminary Spring 2017

Mechanics PhD Preliminary Spring 2017 Mechanics PhD Preliminary Spring 2017 1. (10 points) Consider a body Ω that is assembled by gluing together two separate bodies along a flat interface. The normal vector to the interface is given by n

More information

Iranian Journal of Mathematical Sciences and Informatics Vol.2, No.2 (2007), pp 1-16

Iranian Journal of Mathematical Sciences and Informatics Vol.2, No.2 (2007), pp 1-16 Iranian Journal of Mathematical Sciences and Informatics Vol.2, No.2 (2007), pp 1-16 THE EFFECT OF PURE SHEAR ON THE REFLECTION OF PLANE WAVES AT THE BOUNDARY OF AN ELASTIC HALF-SPACE W. HUSSAIN DEPARTMENT

More information

Electromagnetic Waves Across Interfaces

Electromagnetic Waves Across Interfaces Lecture 1: Foundations of Optics Outline 1 Electromagnetic Waves 2 Material Properties 3 Electromagnetic Waves Across Interfaces 4 Fresnel Equations 5 Brewster Angle 6 Total Internal Reflection Christoph

More information

Application of fractional order theory of thermoelasticity to a 1D problem for a cylindrical cavity

Application of fractional order theory of thermoelasticity to a 1D problem for a cylindrical cavity Arch. Mech., 66, 4, pp. 257 267, Warszawa 2014 Application of fractional order theory of thermoelasticity to a 1D problem for a cylindrical cavity W. E. RASLAN Department of Mathematics and Engineering

More information

where d is the vibration direction of the displacement and c is the wave velocity. For a fixed time t,

where d is the vibration direction of the displacement and c is the wave velocity. For a fixed time t, 3 Plane waves 3.1 Plane waves in unbounded solid Consider a plane wave propagating in the direction with the unit vector p. The displacement of the plane wave is assumed to have the form ( u i (x, t) =

More information

Chapter 15. Mechanical Waves

Chapter 15. Mechanical Waves Chapter 15 Mechanical Waves A wave is any disturbance from an equilibrium condition, which travels or propagates with time from one region of space to another. A harmonic wave is a periodic wave in which

More information

Understanding hydraulic fracture variability through a penny shaped crack model for pre-rupture faults

Understanding hydraulic fracture variability through a penny shaped crack model for pre-rupture faults Penny shaped crack model for pre-rupture faults Understanding hydraulic fracture variability through a penny shaped crack model for pre-rupture faults David Cho, Gary F. Margrave, Shawn Maxwell and Mark

More information

Simulation of Geometrical Cross-Section for Practical Purposes

Simulation of Geometrical Cross-Section for Practical Purposes Simulation of Geometrical Cross-Section for Practical Purposes Bhasker R.S. 1, Prasad R. K. 2, Kumar V. 3, Prasad P. 4 123 Department of Mechanical Engineering, R.D. Engineering College, Ghaziabad, UP,

More information

Reflection of Plane Waves from Electro-magneto-thermoelastic Half-space with a Dual-Phase-Lag Model

Reflection of Plane Waves from Electro-magneto-thermoelastic Half-space with a Dual-Phase-Lag Model Copyright 2016 Tech Science Press CMC, vol.51, no.2, pp.63-79, 2016 Reflection of Plane Waves from Electro-magneto-thermoelastic Half-space with a Dual-Phase-Lag Model A. M. Abd-Alla 1,2,3, Mohamed I.

More information

DISPLACEMENTS AND STRESSES IN AN ANISOTROPIC MEDIUM DUE TO NON-UNIFORM SLIP ALONG A VERY LONG STRIKE-SLIP FAULT

DISPLACEMENTS AND STRESSES IN AN ANISOTROPIC MEDIUM DUE TO NON-UNIFORM SLIP ALONG A VERY LONG STRIKE-SLIP FAULT ISET Journal of Earthquake Technology, Paper No. 45, Vol. 4, No. 1, March 005, pp. 1-11 DISPLACEMENTS AND STRESSES IN AN ANISOTROPIC MEDIUM DUE TO NON-UNIFORM SLIP ALONG A VERY LONG STRIKE-SLIP FAULT Dinesh

More information