Naturally deposited sand in its undisturbed intact state exhibits distinct mechanical properties compared to reconstituted sand owing to the initial fabric generated during sedimentation. In this study, hollow cylinder torsional shear (HCTS) tests were conducted on an intact sand obtained from a river–lake sedimentation area and its air-pluviated reconstituted counterpart to compare their macro-scale mechanical behavior. In parallel, X-ray tomography scans were performed on corresponding mini-samples at an initial state to compare their fabric characteristics. The results indicate that, at the macro-scale, intact sand exhibits greater initial shear modulus and more pronounced dilation, with these differences gradually diminishing as loading progresses. At the micro-scale, the particle orientation of intact sand exhibits concentration within an inclined plane, whereas reconstituted sand particles tend to orient in the horizontal plane. Intact sand displays a more uniform contact normal orientation distribution, greater coordination number, and especially, greater contact area and volume compared to reconstituted sand. These disparities are more pronounced in the coarse particles within the samples. Based on the microstructure characteristics, an interlocking variable I is proposed. I is hypothesized to evolve during shearing and ultimately converge to a unique critical state and is introduced in a dilatancy state parameter to form the Critical State Theory incorporating Interlocking (CST-I). The simulation results highlight that with the incorporation of I in CST-I, the greater shear modulus and more pronounced dilation of intact sand can be well captured. CST-I provides a framework to unify the modeling of uncemented structured and reconstituted sand.
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