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Field observation of the wave-induced pore pressure response in a silty soil seabed

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Abstract

Liquefaction of seabed sediments under the action of storm waves is an important form of seabed instability, which may cause damage to submarine structures such as pipelines and cables. A commonly used parameter to identify sediment liquefaction is pore pressure. The pressure response of the pore water at different depths of a silty soil seabed under storm waves was monitored by a probe rod in the Yellow River delta. The probe is made of a steel pipe with a length of 8 m and an outer diameter of 10 cm, which is equipped with 10 pore pressure sensors. According to the collected data, under a water depth of 8 m, silty soil seabed liquefaction starts when the significant wave height reaches 0.5 m, and the liquefaction depth is between 3.3 and 3.8 m under waves with a significant wave height of 3.65 m. Seabed liquefaction develops in a top-down manner, and the average development rate of the liquefaction depth is approximately 0.17 m/min.

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Abbreviations

d :

grain size

h :

water depth

H :

wave height

\( \overline{H} \) :

average wave height

H max :

maximum wave height

H 1/3 :

significant wave height

K :

coefficient of permeability

K P :

pressure coefficient

k 0 :

lateral earth pressure coefficient at rest

P :

magnitude of the pressure change at the water bottom

P e :

excess pore pressure

\( {\overline{P}}_e \),:

residual excess pore pressure

P m :

measured pore pressure

P z :

magnitude of the pressure change at burial depth z

P 0 :

static pore pressure

T :

wave period

\( \overline{T} \) :

average wave period

T 1/3 :

significant wave period

v :

development rate of liquefaction depth

W g :

water content

z :

burial depth of the sensor

γ :

unit weight

γ s :

effective unit weight of soil

γ w :

effective unit weight of sea water

σ :

effective stress

σ v0 :

initial vertical effective stress

σ 0 :

initial effective stress

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Funding

This study was funded by the National Natural Science Foundation of China (Grant No. 41576039).

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Correspondence to Guohui Xu.

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Xu, X., Xu, G., Yang, J. et al. Field observation of the wave-induced pore pressure response in a silty soil seabed. Geo-Mar Lett 41, 13 (2021). https://doi.org/10.1007/s00367-020-00680-6

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