Reflection of Plane Waves at Free Surface of an Initially Stressed Dissipative Medium

The paper discuses the effect of initial stresses on the reflection coefficients of plane waves in a dissipative medium. Basic governing equations are formulated in context of Biot's incremental deformation theory. These governing equations are solved analytically to obtain the dimensional phase velocities of plane waves propagating in plane of symmetry. Closed-form expressions for the reflection coefficients of P and SV waves- incident at the free surface of an initially stressed dissipative medium are obtained. Numerical computations, using these expressions, are carried out for a particular model. Computations made with the results predicted in presence and absence of the initial stresses and the results have been shown graphically. The study shows that the presence of compressive initial stresses increases the velocity of longitudinal wave (P-wave) but diminishes that of transverse wave (SV-wave). Also the numerical results presented indicate that initial stresses and dissipation might affect the reflection coefficients significantly.


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References:
[1] S. B Sinha.," Transmission of elastic waves through a homogenous layer
sandwiched in homogenous media". J. Phys. Earth, 12, 1999, pp 1-4
[2] R. D Tooly., T. W. Spencer and H. F. Sagoci ," Reflection and
Transmission of plane compressional waves," Geophysics, 30, 1965, pp
552-570.
[3] R. N. Gupta," Reflection of plane waves from a linear transition layer in
liquid media," Geophysics, 30, 1965, pp 122-131.
[4] R. N. Gupta," Reflection of elastic waves from a linear transition layer,"
Bull. Seism. Soc. Am.56, 1966, pp 511-526.
[5] R. N. Gupta," Propagation of SH-waves in inhomogeneous media," J.
Acoust. Soc. Am., 41, 1967, pp 1328-1329.
[6] H., K . Acharya" Reflection from the free surface of inhomogeneous
media," Bull. Seism. Soc. Am.60, 1970, pp 1101-1104.
[7] V. Cerveny," Reflection and Transmission coefficients for transition
layers," Studia Geophys. Geod., 171974, pp 59-68.
[8] B. M. Singh. , S. J. Singh and S. D. Chopra," Reflection and refraction
of SH-waves and the plane boundary between two laterally and
vertically heterogeneous solids," Act Geophys. Pol., 26, 1978, pp 209-
216.
[9] S. L. Saini," Reflection and refraction of SH-waves in anisotropic
inhomogeneous media," PhD. Thesis Kurukshetra Univ., India, 1979.
[10] B. Singh, A. Kumar and J. Singh," Reflection of generalized
thermoelastic wave from a solid half-space under hydrostatic initial
stress," Appl. Math. Comput., 177, 2006, pp 170-177.
[11] S. K. Tomar and J. Singh," Transmission of longitudinal waves through
a plane interface between two dissimilar porous elastic solid halfspaces,"
Appl. Math. Comput., 169, 2005, pp 671-688.
[12] M. D. Sharma, "Effect of initial stress on reflection at the free surfaces
of anisotropic elastic medium," J. Earth Syst. Sci. 116, No. 6, 2007, pp
537-551.
[13] M. A. Biot," Mechanics of Incremental Deformation,", John Wiley and
Sons Inc., New York, 1965.
[14] Y. C. Fung, "Foundation of solid mechanics," Prentice Hall of India,
New Delhi, 1965.
[15] M. M Selim and M. K. Ahmed," Propagation and attenuation of seismic
body waves in dissipative medium under initial and couple stresses,"
Appl. Math. Comput., 182, 2006, pp 1064-1074.
[16] R. M Kebeasy A. I Bayoumy and A. A. Gharib, "Crustal structure
modeling for the northern part of the Aswan Lake area using seismic
waves generated by explosions and local earthquake," J.
Geodynamics,14, Nos 1-4,1991, pp159-182.
[17] S. Dey and D. Dutta," Propagation and attenuation of seismic body
waves in initially stressed dissipative medium," Acta Geophys. Pol.,
XLVI, No.3, 1998, pp. 351- 365.