scholarly journals Review on Seismic Liquefaction of Seabed Soil

Author(s):  
ChangXian Zhou ◽  
ShaoPeng Zheng ◽  
YouQuan Ye ◽  
Hao Wang
2021 ◽  
Vol 12 (1) ◽  
pp. 12-21
Author(s):  
Azad Kumar Mehta ◽  
Deepak Kumar ◽  
Pijush Samui

Liquefaction susceptibility of soil is a complex problem due to non-linear behaviour of soil and its physical attributes. The assessment of liquefaction potential is commonly assessed by the in-situ testing methods. The classification problem of liquefaction is non-linear in nature and difficult to model considering all independent variables (seismic and soil properties) using traditional techniques. In this study, four different classification techniques, namely Fast k-NN (F-kNN), Naïve Bayes Classifier (NBC), Decision Forest Classifier (DFC), and Group Method of Data Handling (GMDH), were used. The SPT-based case record was used to train and validate the models. The performance of these models was assessed using different indexes, namely sensitivity, specificity, type-I error, type-II error, and accuracy rate. Additionally, receiver operating characteristic (ROC) curve were plotted for comparative study. The results show that the F-kNN models perform far better than other models and can be used as a reliable technique for analysis of liquefaction susceptibility of soil.


2021 ◽  
Vol 11 (24) ◽  
pp. 11631
Author(s):  
Xiuwei Chai ◽  
Jingyuan Liu ◽  
Yu Zhou

This study is aimed at numerically investigating the cnoidal wave-induced dynamics characteristics and the liquefaction process in a loosely deposited seabed floor in a shallow water environment. To achieve this goal, the integrated model FSSI-CAS 2D is taken as the computational platform, and the advanced soil model Pastor–Zienkiewicz Mark III is utilized to describe the complicated mechanical behavior of loose seabed soil. The computational results show that a significant lateral spreading and vertical subsidence could be observed in the loosely deposited seabed floor due to the gradual loss of soil skeleton stiffness caused by the accumulation of pore pressure. The accumulation of pore pressure in the loose seabed is not infinite but limited by the liquefaction resistance line. The seabed soil at some locations could be reached to the full liquefaction state, becoming a type of heavy fluid with great viscosity. Residual liquefaction is a progressive process that is initiated at the upper part of the seabed floor and then enlarges downward. For waves with great height in shallow water, the depth of the liquefaction zone will be greatly overestimated if the Stokes wave theory is used. This study can enhance the understanding of the characteristics of the liquefaction process in a loosely deposited seabed under coastal shallow water and provide a reference for engineering activities.


Author(s):  
Nick J. Traylen ◽  
Frederick J. Wentz ◽  
Sjoerd Van Ballegooy ◽  
Liam M. Wotherspoon ◽  
Theo Hnat ◽  
...  

2002 ◽  
Vol 42 (1) ◽  
pp. 35-52 ◽  
Author(s):  
YOSHIHISA SHIMIZU ◽  
SUSUMU YASUDA ◽  
IWAO MORIMOTO ◽  
ROLANDO ORENSE
Keyword(s):  

Poromechanics ◽  
2020 ◽  
pp. 505-510
Author(s):  
T. Shiomi ◽  
S. Tsukuni ◽  
O.C. Zienkiewicz

2014 ◽  
Vol 24 (3) ◽  
pp. 249-266 ◽  
Author(s):  
Vijay Kumar ◽  
Kumar Venkatesh ◽  
R. P. Tiwari

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