Initial Stress and Gravity on P-Wave Reflection from Electromagneto-Thermo-Microstretch Medium in the Context of Three-Phase Lag Model

)e present paper studied the reflection of thermo-microstretch waves under the generalized thermoelasticity theory which is employed to study the reflection of plane harmonic waves from a semi-infinite elastic solid under the effect of the electromagnetic field, initial stress, and gravity. )e formulation is applied under the thermoelasticity theory with three-phase lag, and the reflection coefficient ratio variations with the angle of incidence under different conditions are obtained. Numerical results obtained from the present study are presented graphically and discussed. It is observed that the initial stress, gravitation, and electromagnetic field exert some influence in the thermo-microstretch medium due to reflection of P-waves.


Introduction
In recent decades, the influences of electromagnetic field, initial stress, gravitation, and thermal field have been much pronounced in diverse fields, especially, engineering, geophysics, geology, acoustics, plasma, and physics because of its utilitarian aspects in these fields. e generalized theories of thermoelasticity, which admit the finite speed of a thermal signal, have been the center of interest of active research. Allam et al. [1] discussed the Green-Lindsay model of reflection of P and SV waves from the free surface of thermoelastic diffusion, solid under influence of the electromagnetic field, and initial stress. Abo-Dahab and Kilicman [2] illustrated the reflection and transmission of Pand SV-wave phenomena at the interface between solid and liquid media with magnetic field and two thermal relaxation times. Othman and Song [3] developed the reflection of plane waves from an elastic solid half-space under hydrostatic initial stress without energy dissipation. Abd-Alla et al. [4] studied SV wave's incidence at the interface between solid and liquid media under electromagnetic field and initial stress in the context of three thermoelastic theories. Aboueregal and Abo-Dahab [5] discussed the dual-phase model on magneto-thermoelasticity infinite nonhomogeneous solid having a spherical cavity. Zhou et al. [6] developed the reflection and transmission of plane waves at the interface of pyroelectric bimaterials. Singh [7] illustrated the reflection of P and SV waves from the free surface of an elastic solid with generalized thermodiffusion. Sinha and Sinha [8][9][10] studied the reflection of thermoelastic waves at a solid half-space with thermal relaxation. Angel and Achenbach [11] discussed the reflection and transmission of elastic waves by a periodic array of crack. Kilany et al. [12] developed photothermal and void effect of a semiconductor rotational medium based on the Lord-Shulman theory. Quintanilla and Racke [13] studied a note on stability of three-phase lag heat conduction. Kothari et al. [14] developed the fundamental solutions of generalized thermoelasticity with three-phase lags. Banik and Kanoria [15] illustrated generalized thermoelastic interaction in a functionally graded isotropic unbounded medium due to varying heat source with three-phase lag effect. Chou and Yang [16] developed two-dimensional dual-phase lag thermal behavior in single-/multilayer structures using the space-time conservation element and solution element (CESE) method. Liu [17] studied numerical analysis of dualphase lag and heat transfer in a layered cylinder with nonlinear interface boundary conditions. Marzougui et al. [18] used a computational analysis of heat transport irreversibility phenomenon in a magnetized porous channel. Abo-Dahab et al. [19] developed MHD Casson nanofluid flow over nonlinearly heated porous medium in the presence of extending surface effect with suction/injection. Zaim et al. [20] used Galerkin finite element analysis of magneto-hydrodynamic natural convection of Cu-water-nanoliquid in a baffled U-shaped enclosure. Mebarek-Oudina et al. [21] illustrated magneto-thermal convection stability in an inclined cylindrical annulus filled with a molten metal. Ezzat and Othman [22] investigated the plane waves in an electromagneto-thermoelastic perfect conductivity medium with two relaxation times. e objective of the present investigation is to determine the reflection of P waves from the thermo-electro-magnetomicrostretch medium in the context of three-phase lag model under the effect of rotation, electromagnetic field, and gravity with initial stress. e reflection coefficient ratios of various reflected waves with the angle of incidence have been obtained from the 3PHL model and LS theory. Also, the effect of the electromagnetic field and gravity is discussed numerically and illustrated graphically. e physical quantities are obtained and tested by a numerical study using the parameters of Cu as a target and presented graphically. e distribution of these quantities is represented graphically in the presence and absence of electromagnetic field, initial stress, and gravity field.

Formulation of the Problem
e equations of generalized thermo-microstretch in a rectangular coordinate system (x, y, z) with z− axis directed in the media are used. Constant magnetic field intensity H � (0, H 0 , 0) is taken as the direction of the y-axis. We begin our consideration with linearized equations of electrodynamics of slowly moving media.
(1) e constitutive equation in the presence of gravitational and electromagnetic field is From the above equations, we can obtain From equations (3) and (4), we obtain So, the displacement vector u has the components u x � u(x, z, t), u y � 0, and u z � w(x, z, t). where In component form, the basic governing equations become μ + k − P 2 2 Complexity such that τ * ] � K + K * τ ] , ∇ 2 � (z 2 /zx 2 ) + (z 2 /zz 2 ). e constitutive relation can be written as To facilitate the solution, the following dimensionless quantities are introduced: Using equation (18), the governing equations (7)- (16) recast in the following form (after suppressing the primes): Complexity where e displacement components u(x, z, t) and w(x, z, t) may be written in terms of potential functions Φ(x, z, t) and Using equation (31) in equations (19)- (23), we obtain where

Solution of the problem
We assume now that the solution of equations (32)-(36) takes the following form: Substituting equation (38) into equations (32)-(36), we get which tends to where A, B, C, D, E, and F in equation (45) are given in Appendix A From equation (45), there are five waves with five different velocities.

e Boundary Conditions.
e boundary conditions for the problem be taken as From equations (55)-(60), we get

Numerical Results and Discussion
e physical constants used are [3] i � (60) Figure 2 shows the variation of the amplitude of reflected P 1 wave |Z 1 |, amplitude of reflected P 2 wave |Z 2 |, amplitude of reflected P 3 wave |Z 3 |, amplitude of reflected P 4 wave |Z 4 |, and amplitude of reflected P 5 wave |Z 5 | with respect to the angle of incidence θ for different values of the initial stress. e amplitude of the reflected wave increases with increasing of the angle of incidence until it reaches a maximum value at θ about 90. e amplitude of reflected P 2 wave |Z 2 |, the amplitude of reflected P 3 wave |Z 3 |, the amplitude of reflected P 4 wave |Z 4 |, and the amplitude of reflected P 5 wave |Z 5 | each of them decrease with increasing of the angle of incidence until it becomes a minimum value at θ � 90. In addition, all lines begin to coincide when the horizontal angle of incidence θ increases to the maximum. ese results obey physical reality for the behavior of reflection of P waves [3]. Figure 3 shows the variation of the amplitude of reflected P 1 wave |Z 1 |, amplitude of reflected P 2 wave |Z 2 |, amplitude of reflected P 3 wave |Z 3 |, amplitude of reflected P 4 wave |Z 4 |, and amplitude of reflected P 5 wave |Z 5 | with respect to the angle of incidence θ for different values of the gravitation. e amplitude of reflected P 1 wave |Z 1 |, the amplitude of the reflected wave |Z 2 |, and the amplitude of reflected P 5 wave |Z 5 | increases with increasing angle of incidence until it reaches a maximum value at θ about 90. e amplitude of reflected P 3 wave |Z 3 | and the amplitude of reflected P 4 wave z-axis Complexity |Z 4 | decreases with increasing angle of incidence until it becomes a minimum value at θ � 90. It is noticed that the reflection of P waves is strongly affected by the presence of gravity [23]. Figures 4 and 5: show the variation of the amplitude of reflected P 1 wave |Z 1 |, amplitude of reflected P 2 wave |Z 2 |, amplitude of reflected P 3 wave |Z 3 |, amplitude of reflected P 4 wave |Z 4 |, and amplitude of reflected P 5 wave |Z 5 | with respect to the angle of incidence θ for different values of the electric field and magnetic field, respectively. e amplitude of reflected P 1 wave |Z 1 |, amplitude of reflected P 2 wave |Z 2 |, amplitude of reflected P 3 wave |Z 3 |, amplitude of reflected P 4 wave |Z 4 |, and amplitude of reflected P 5 wave |Z 5 | increase with increasing electric field and magnetic field. e electric field and magnetic field increase the magnitude of reflection of P waves. is is mainly due to the fact that the electric field and magnetic field correspond to a term signifying a positive force that tends to accelerate the charge carries [2]. Figure 6 shows the variation of the amplitude of reflected P 1 wave |Z 1 |, amplitude of reflected P 2 wave |Z 2 |, amplitude of reflected P 3 wave |Z 3 |, amplitude of reflected P 4 wave |Z 4 |, and amplitude of reflected P 5 wave |Z 5 | with respect to the angle of incidence θ. e change of amplitude of reflected to wave appeared in this figure, where we notice gravitation, electric field, magnetic field, and initial stress. ese figures are very important to study the dependence of these physical quantities on the vertical amplitude of reflected of distance. e curves obtained are highly depending on the vertical distance from origin, and all the physical quantities satisfy boundary condition and are moving in P waves [24].

Conclusion
We obtain the following conclusions based on the above analysis: (1) e reflected P waves and amplitude of the reflected P waves depend on the angle of incidence, rotation, initial stress, gravity field, and magnetic field, and the nature of this dependence is different for different reflected P waves.
(2) e rotation, initial stress, gravity field, and electromagnetic field play a significant role, and the effects have the inverse trend for the reflected P waves and amplitude of the reflected P waves.
(3) e rotation, initial stress, gravity field, and electromagnetic field have a strong effect on the reflected P waves and amplitude of the reflected P waves.
(4) e result provides a motivation to investigate the reflection of P waves from thermo-magneto-microstretch materials as a new class of applications thermoelectric solids. e results presented in this paper should prove to be useful for researchers in material science, designers of new materials, microsystem technologies, physicists, as well as for those working on the development of thermo-electro-magneto-microstretch and in practical situations as in geophysics, optics, acoustics, and geomagnetic and oil prospecting.
(5) e equations were solved by using the wave function assumption which is the basis of the normal mode method and the features of this system. We can find the amplitude of the primary wave under the influence of different variables, whether gravity, primary gain, and electric and magnetic fields, by varying relaxation time.
It is observed that the amplitudes of reflected P waves change in the presence of rotation, initial stress, gravity field, and magnetic field. Hence, the presence of rotation, initial stress, gravity field, and electromagnetic field significantly affected the reflection phenomena. Electric current density vector K, K * : ermal conduction coefficients m ij :