A constitutive model, based on the concept of scaled memory (SM), is p
resented to describe the undrained behavior of anisotropic clays subje
cted to generalized loadings. The SM capabilities that were previously
established for one-dimensional cyclic responses are extended to six-
dimensional monotonic loadings. SM is simpler than multiyield surface
plasticity, and just as capable in modeling anisotropic behavior. The
performance of the SM model is illustrated by simulating the stress-st
rain responses of K-0-consolidated clays during combined triaxial-tors
ional tests.