“…(1992), Abousleiman et al (1998), Ghassemi and Diek (2002), Tod (2003). Eringen (1970) and Nowacki (1966)developed the linear theory of micropolar thermoelasticity which are known as micropolar coupled thermoelasticity to include thermal effects. Goodman and Cowin (1972) 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.).…”