Pan Liu
Current Organizations / Institutes
The organizations/institutes from the scholar's latest article
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Pan Liu has a total of 5 co-authors. Here are the top co-authors by number of shared publications:
- Jingping Xu
Department of Ocean Science and Engineering, Southern University of Science and Technology, Shenzhen 518055, China
1 shared publication - Jinwen Zhang
Guangdong Provincial Key Laboratory of Green Construction and Intelligent Operation & Maintenance for Offshore Infrastructure, School of Future Transportation, Guangzhou Maritime University/Guangzhou Jiaotong University (Under Construction), Guangzhou 510725, China
1 shared publication - Shufeng Bao
Guangdong Provincial Key Laboratory of Green Construction and Intelligent Operation & Maintenance for Offshore Infrastructure, School of Future Transportation, Guangzhou Maritime University/Guangzhou Jiaotong University (Under Construction), Guangzhou 510725, China
1 shared publication - Xuesheng Qian
Guangdong Provincial Key Laboratory of Green Construction and Intelligent Operation & Maintenance for Offshore Infrastructure, School of Future Transportation, Guangzhou Maritime University/Guangzhou Jiaotong University (Under Construction), Guangzhou 510725, China
1 shared publication - Yuping Yang
National Engineering Research Center of Port Hydraulic Construction Technology, Tianjin Research Institute for Water Transport Engineering, Ministry of Transport, Tianjin 300456, China
1 shared publication
Latest Publications
- Open Access
- 22 February 2026
- Published by MDPI AG in Journal of Marine Science and Engineering
- Vol. 14 (4) , 400
Analysis of Seepage Effects on Seabed Slope Stability Under Earthquake Loading
To find out the combined effect of seismic action, seepage, and sandy and argillaceous interlayers on the seabed slope stability, the safety factors of seabed slopes, which include sandy and argillaceous interlayers, under different hydraulic gradients and seismic loads, were calculated using the geotechnical simulation software Geo-Studio 2012. Results demonstrate that both seismic action and seepage exert significant impacts on seabed slope stability: seismic loads play a dominant role in governing slope stability, while seepage acts as a key triggering factor for slope failure. With the gradual increase in seismic load magnitude, the influence of seepage hydraulic gradient on slope safety factor decreases progressively. For homogeneous segregated slopes, which consist of silty clay, a higher seepage hydraulic gradient reduces the magnitude of critical seismic load that induces slope instability. Under identical seismic load and hydraulic gradient conditions, seabed slopes with sandy interlayers exhibit higher stability compared to homogeneous soil slopes, whereas slopes with argillaceous interlayers show reduced stability.
- 22 February 2026
- Published by MDPI AG in Journal of Marine Science and Engineering
- Vol. 14 (4) , 400
Open AccessAnalysis of Seepage Effects on Seabed Slope Stability Under Earthquake Loading
To find out the combined effect of seismic action, seepage, and sandy and argillaceous interlayers on the seabed slope stability, the safety factors of seabed slopes, which include sandy and argillaceous interlayers, under different hydraulic gradients and seismic loads, were calculated using the geotechnical simulation software Geo-Studio 2012. Results demonstrate that both seismic action and seepage exert significant impacts on seabed slope stability: seismic loads play a dominant role in governing slope stability, while seepage acts as a key triggering factor for slope failure. With the gradual increase in seismic load magnitude, the influence of seepage hydraulic gradient on slope safety factor decreases progressively. For homogeneous segregated slopes, which consist of silty clay, a higher seepage hydraulic gradient reduces the magnitude of critical seismic load that induces slope instability. Under identical seismic load and hydraulic gradient conditions, seabed slopes with sandy interlayers exhibit higher stability compared to homogeneous soil slopes, whereas slopes with argillaceous interlayers show reduced stability.