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pro vyhledávání: '"P. K. Triantafyllos"'
Publikováno v:
Acta Geotechnica. 15:197-221
The conditions that trigger the unrestrained flow deformation of loose anisotropic sand are investigated. An instability surface (IS) is defined in the deviatoric plane. It comprises the transient-peak states at which flow instability is triggered wh