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Table 3 Difference between wave-induced liquefaction and seismic liquefaction (modified from Zen and Yamazaki 1990a; Sumer et al. 2007)

From: Susceptibility of typical marine geological disasters: an overview

Difference

Earthquake-induced liquefaction

Wave-induced liquefaction

External forces

Earthquake

Wave

Loading

Cyclic shear stress

Oscillatory water pressure

Input

Base

Surface

period

Order of 1 s

Order of 10 s

Duration

Several minutes

A couple of days or weeks

Drainage condition

Undrained

Partially drained

Excess pore pressure

Positive, gradual increase

Positive and negative, oscillatory

Effective stress

Decrease

Decrease and increase alternately

Liquefaction phenomena

Occur at once

Occur transiently and repeatedly