“…Because the slope material had to be under an unsaturated condition from the surface to a certain depth, the authors suspected that unsaturated soil had made a phase transformation from a static condition, as a solid phase, to a ‰uid-like phase after shaking. In order to clarify the mechanism, fundamental research on unsaturated volcanic soils after subjecting them to cyclic shear has been carried out by the authors (Unno et al, 2006a; Kazama et al, 2006). In these studies, it was shown that a shaking disturbance aŠects the moisture state of soil, and that the liquefaction potential of unsaturated soil can be evaluated by taking the volume compressibility of the soil particle structure, the degree of saturation and the conˆning pressure into account.…”