Understanding the mechanical response of silt–clay transitional soils is increasingly important for underground transportation infrastructure, where complex stress paths and one-dimensional (K0) consolidation histories are common. However, most existing studies rely on isotropic consolidation, leaving the effects of K0 consolidation on transitional behavior insufficiently understood. This study presents a systematic series of undrained triaxial tests on reconstituted silty clay consolidated under isotropic and K0 conditions across a range of overconsolidation ratios (OCRs). The results show that phase transformation—a hallmark of transitional soil behavior—appears only in isotropically consolidated specimens at low OCRs, whereas it does not occur in K0-consolidated specimens tested under comparable OCRs. K0-consolidated specimens exhibit a counter-intuitive non-monotonic relationship between void ratio and mean effective stress at the end of shearing, reflecting persistent anisotropic structural effects consistent with anisotropic critical state theory. While K0 consolidation produces more complex stress–strain responses, the stress-ratio evolution remains broadly comparable to isotropically consolidated cases. Overall, the findings demonstrate that consolidation history critically governs the undrained behavior of silt–clay transitional soils and underscore the importance of incorporating realistic K0 consolidation conditions in laboratory characterization and geotechnical design for transportation applications.
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