Wencan Guan, Youliang Chen, Rafig Azzam
Traditional liquefaction criteria based on pore water pressure ratio fail to characterize cumulative plastic deformation prior to liquefaction onset. This study presents a Gaussian process-transformer (GT) diffusion model enabling end-to-end mapping from tidal loading to seabed plastic volumetric strain increments. The GT model embeds cyclic loading history into Gaussian Process covariance structures through a stress path dynamic factor matrix, capturing memory effects absent in conventional methods. Physics constraints are enforced via multi-task learning with cross-attention mechanisms for seamless physics-deep learning integration. Primary validation at Crissy Field achieves R2 = 0.94, outperforming Modified Cam Clay models by 47%–61%. Cross-domain validation using Tokyo Bay CPT data from the 2011 Tohoku earthquake (Mw 9.1) confirms frequency-independence (R2 = 0.82–0.95). Validation at Sheringham Shoal (101 CPT soundings) establishes generalizability across seabed types. The research reveals a 60° phase lag, identifying mid-flood and early ebb as critical risk phases. Uncertainty quantification achieves expected calibration error = 0.0337 and prediction interval coverage probability = 98.7%. The GT framework enables continuous-field real-time liquefaction risk monitoring for offshore infrastructure.