TIME-DEPENDENT TRIAXIAL RELAXATION BEHAVIOR OF A RESEDIMENTED CLAY

The paper describes the results of K-0 consolidated-undrained triaxial compression relaxation tests on resedimented Boston Blue Clay (BBC) u sing a computer-automated triaxial apparatus. Specimens were either no rmally consolidated (overconsolidation ratio, OCR = 1) or had an OCR = 4, and they were sheared at different axial strain rates to axial str ains (epsilon(a)) from 0.1 to 15%. Each strain level was maintained un til the monitored shear stress and pore pressure reached equilibrium l evels. The results show that a single specimen can be used reliably fo r multiple relaxation tests. During relaxation, the rate of normalized shear stress decay with log time, (-Delta q/sigma'(vm))/Delta logt, i s approximately constant, regardless of epsilon(a) or OCR. Changes in shear-induced pore pressure during relaxation were negligible except w hen specimens were rapidly sheared. Independent of OCR, end-of-relaxat ion equilibrium stress states for relaxation strains epsilon, less tha n or equal to 1.5% lie on a line of obliquity defined by K = sigma'(h) /sigma'(v) = 0.50, compared to K-0 = 0.49 for OCR = 1 BBC; whereas, fo r epsilon(a) greater than or equal to 2.5%, the equilibrium states lie on a steeper obliquity line defined by K = 0.40.