“…It basically asserts that any pre-existing UGL stresses that control R M (treating moisture-change effects as marginal) are essentially timewise constant as long as the temperature level does not change. This assumption is deemed very realistic for densely packed particulate materials, as demonstrated in discrete element models [50,51], in laboratory compaction experiments on sand [52], in laboratory thermal cycling experiments on dense sand [34], in large-scale laboratory experiments on UGM compaction [53], in field investigations on compactioninduced stresses on retaining walls [54,55], and in application of geophysical exploration techniques to assess the in situ modulus of UGLs [56]. Finally, it is noted that there exists some experimental evidence that well-compacted UGMs under constant temperature exhibit time-dependent mechanical behavior, e.g., creep under constant level of load, and stress-relaxation under constant level of deformation [57].…”