“…The laboratory and analytical investigations into the release of trapped particles from the pores of geological formations (Beresnev and Johnson, 1994;Kouznetsov et al, 1998;Roberts et al, 2001;Kostrov and Wooden, 2002;Vogler and Chrysikopoulos, 2002;Iassonov and Beresnev, 2003;Pride et al, 2008;Roberts and Abdel-Fattah, 2009;Beresnev and Deng, 2010;Beresnev et al, 2000;Manga et al, 2012;Lo et al, 2012;Deng and Cardenas, 2013) suggest that an estimate of the fluid motion in the target formation can lead to a better assessment of the particle mobilization phenomenon. In order to estimate the fluid motion generated due to the applied stress wave stimulation, in this section, we consider the case of a poroelastic target inclusion (Ω a , Fig.…”