Abstract: | The results of experimental investigations of the compressibility of argillaceous soils (loess loams, loams, and clays) subjected to underground explosions are discussed. The data concerning the deformation at the shock-wave front, and their comparison with data concerning residual deformations indicate that the viscoplastic soil properties strongly influence the soil compressibility for short-term loads originating from underground explosions. The conclusions which were previously drawn in [1] are qualitatively and quantitatively confirmed. |