Pressure characteristics of two-dimensional topography in wave-induced seabed liquefaction

被引：0
|
作者：
Wang, Youqi [1 ]
Wang, Qixiang [1 ]
Cao, Ruichen [2 ,3 ,7 ]
Gao, Guandong [4 ,5 ,6 ,7 ,8 ]
Feng, Xingru [4 ,5 ,6 ,7 ,8 ]
Yin, Baoshu [4 ,5 ,6 ,8 ]
Ren, Huanping [9 ]
Guo, Junting [10 ]
Lv, Xianqing [1 ]
机构：
[1] Ocean Univ China, Frontier Sci Ctr Deep Ocean Multispheres & Earth S, Phys Oceanog Lab, Qingdao 266100, Peoples R China
[2] Shandong Key Lab Marine Ecol Environm & Disaster P, Qingdao 266061, Peoples R China
[3] Minist Nat Resources, North China Sea Marine Forecasting Ctr, Qingdao 266590, Peoples R China
[4] Chinese Acad Sci, Inst Oceanol, Key Lab Ocean Observat & Forecasting, Key Lab Ocean Circulat & Waves, Qingdao 266071, Peoples R China
[5] Chinese Acad Sci, CAS Key Lab Ocean Circulat & Waves, Inst Oceanol, Qingdao 266071, Peoples R China
[6] Laoshan Lab, Qingdao 266071, Peoples R China
[7] Chinese Acad Sci, Inst Oceanol, CAS Engn Lab Marine Ranching, Qingdao 266071, Peoples R China
[8] Univ Chinese Acad Sci, Beijing 100029, Peoples R China
[9] Chinese Acad Sci, Inst Oceanol, Oceanog Data Ctr, Qingdao 266071, Peoples R China
[10] Jimei Univ, Polar & Marine Res Inst, Coll Harbor & Coastal Engn, Xiamen 361021, Peoples R China
来源：
PHYSICS OF FLUIDS | 2025年 / 37卷 / 01期
基金：
国家重点研发计划; 中国国家自然科学基金;
关键词：
INDUCED PROGRESSIVE LIQUEFACTION;
D O I：
10.1063/5.0250813
中图分类号：
O3 [力学];
学科分类号：
08 ; 0801 ;
摘要：
This study used the Massachusetts Institute of Technology general circulation model (MITgcm) to simulate the seabed liquefaction process in the Chengdao area. The liquefied soil and the overlying water are considered as a two-layer fluid system in the model. By constructing various topographies using Gaussian functions, it is possible to achieve an agreement between simulation and measurement. The simulation results reveal the characteristics of pore pressure in different topographies. The main findings include the following: (1) The expansion of liquefaction zone leads to an accelerated attenuation of pore pressure amplitude. (2) A decrease in topographic slope diminishes the wave group characteristics of pore pressure due to the sensitivity of certain wave components with specific frequencies to topographic slope.
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收藏
页数：11
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