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This document examines differences between three seismic soil liquefaction triggering relationships: (1) Seed et al. (1985), (2) Boulanger and Idriss (2012), and (3) Cetin et al. (2018). The relationships are plotted on the same scale to compare boundary curves defining liquefaction triggering. Significant differences are seen between the curves at probability levels of 50% and 20% liquefaction. While boundary curves alone do not fully characterize hazard levels, the differences indicate varying levels of c

Author

Youven Duraisamy

Language

EN