Research Progress and Prospects of Geohazard Mechanism and Risk Prevention Related to Seabed Fluid Migration

Tian, Z. Q.; Jia, Yonggang; Zhu, Chaoqi; Lü, Lin; Xu, Guangli; Xia, Feng; Wang, Hui; Wang, Hongwei; He, Manchao; Peng, Jianbing

doi:10.15302/j-sscae-2023.03.012

Chinese Journal of Engineering Science

2023

DOI: 10.15302/j-sscae-2023.03.012

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Research Progress and Prospects of Geohazard Mechanism and Risk Prevention Related to Seabed Fluid Migration

Z. Q. Tian¹,

Yonggang Jia²,

Chaoqi Zhu³

et al.

Abstract: Seabed fluid migration is a critical process that involves the transport and movement of liquids, gases, and seawater within and outside the seabed, which has significant impacts on the genesis, development, and evolution of seabed geological disasters.

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2024

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Cited by 2 publications

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Interaction between internal solitary waves and the seafloor in the deep sea

Tian,

Huang,

Xiang

et al. 2024

Deep Underground Science and Engineering

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Internal solitary wave (ISW), as a typical marine dynamic process in the deep sea, widely exists in oceans and marginal seas worldwide. The interaction between ISW and the seafloor mainly occurs in the bottom boundary layer. For the seabed boundary layer of the deep sea, ISW is the most important dynamic process. This study analyzed the current status, hotspots, and frontiers of research on the interaction between ISW and the seafloor by CiteSpace. Focusing on the action of ISW on the seabed, such as transformation and reaction, a large amount of research work and results were systematically analyzed and summarized. On this basis, this study analyzed the wave–wave interaction and interaction between ISW and the bedform or slope of the seabed, which provided a new perspective for an in‐depth understanding of the interaction between ISW and the seafloor. Finally, the latest research results of the bottom boundary layer and marine engineering stability by ISW were introduced, and the unresolved problems in the current research work were summarized. This study provides a valuable reference for further research on the hazards of ISW to marine engineering geology.

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Interaction between internal solitary waves and the seafloor in the deep sea

Tian,

Huang,

Xiang

et al. 2024

Deep Underground Science and Engineering

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Microseismic observations reveal that internal waves intensify seabed methane release

Tian,

Jia,

Zhu

et al. 2024

Sci. China Earth Sci.

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scite is a Brooklyn-based organization that helps researchers better discover and understand research articles through Smart Citations–citations that display the context of the citation and describe whether the article provides supporting or contrasting evidence. scite is used by students and researchers from around the world and is funded in part by the National Science Foundation and the National Institute on Drug Abuse of the National Institutes of Health.

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Research Progress and Prospects of Geohazard Mechanism and Risk Prevention Related to Seabed Fluid Migration

Abstract: Seabed fluid migration is a critical process that involves the transport and movement of liquids, gases, and seawater within and outside the seabed, which has significant impacts on the genesis, development, and evolution of seabed geological disasters.

Cited by 2 publications

References 9 publications

Interaction between internal solitary waves and the seafloor in the deep sea

Interaction between internal solitary waves and the seafloor in the deep sea

Microseismic observations reveal that internal waves intensify seabed methane release

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