Three-dimensional dynamic simulation of waves produced by landslides: an analysis of the Mogangling landslide caused by the Moxi earthquake in 1786.
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| Title: | Three-dimensional dynamic simulation of waves produced by landslides: an analysis of the Mogangling landslide caused by the Moxi earthquake in 1786. |
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| Authors: | Ge, Yunfeng1,2 (AUTHOR) geyunfeng@cug.edu.cn, Shao, Xianyun1 (AUTHOR) shaoxianyun@cug.edu.cn, Fu, Xiaodong3 (AUTHOR) xdfu@whrsm.ac.cn, Zhu, Lei4 (AUTHOR) zhul@imde.ac.cn, Hu, Bin1 (AUTHOR) hubin2023@cug.edu.cn, Tang, Huiming1,5 (AUTHOR) tanghm@cug.edu.cn |
| Source: | Quarterly Journal of Engineering Geology & Hydrogeology. May2026, Vol. 59 Issue 2, p1-13. 13p. |
| Subjects: | Landslides, Water waves, Theory of wave motion, Computer simulation, Earthquakes, Granular flow, Landslide hazard analysis, Rockslides |
| Abstract: | Surge waves generated by landslides can lead to catastrophic consequences, including severe economic losses and loss of life. This study investigates the surge waves induced by the Mogangling landslide triggered by the 1786 Moxi earthquake through a combination of numerical simulations and field surveys. A detailed field investigation was conducted to characterize the engineering geological features of the Mogangling landslide. Based on the point cloud data, a 3D landslide model was constructed and used for numerical simulations. The landslide motion was simulated using a granular flow model, and wave propagation was modelled using the renormalization group turbulence model. These two models were coupled to analyse the generation and evolution of the landslide-induced surge waves. The simulation results indicate that the peak sliding velocity of the landslide approached 20 m s−1. As the landslide mass entered the Dadu River, a large landslide-dam formed, temporarily blocking the river and generating intense surge waves. The peak water velocity increased to 30 m s−1, and the maximum wave height reached 81.78 m, which is consistent with the historical record of roughly 80 m. The surge waves propagated in a circular pattern toward the opposite riverbank. The findings provide insights for the risk assessment of landslide-induced surge waves. [ABSTRACT FROM AUTHOR] |
| Copyright of Quarterly Journal of Engineering Geology & Hydrogeology is the property of Geological Society Publishing House and its content may not be copied or emailed to multiple sites without the copyright holder's express written permission. Additionally, content may not be used with any artificial intelligence tools or machine learning technologies. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.) | |
| Database: | Engineering Source |
| FullText | Text: Availability: 0 |
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| Header | DbId: egs DbLabel: Engineering Source An: 193492224 AccessLevel: 6 PubType: Academic Journal PubTypeId: academicJournal PreciseRelevancyScore: 0 |
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| Items | – Name: Title Label: Title Group: Ti Data: Three-dimensional dynamic simulation of waves produced by landslides: an analysis of the Mogangling landslide caused by the Moxi earthquake in 1786. – Name: Author Label: Authors Group: Au Data: <searchLink fieldCode="AR" term="%22Ge%2C+Yunfeng%22">Ge, Yunfeng</searchLink><relatesTo>1,2</relatesTo> (AUTHOR)<i> geyunfeng@cug.edu.cn</i><br /><searchLink fieldCode="AR" term="%22Shao%2C+Xianyun%22">Shao, Xianyun</searchLink><relatesTo>1</relatesTo> (AUTHOR)<i> shaoxianyun@cug.edu.cn</i><br /><searchLink fieldCode="AR" term="%22Fu%2C+Xiaodong%22">Fu, Xiaodong</searchLink><relatesTo>3</relatesTo> (AUTHOR)<i> xdfu@whrsm.ac.cn</i><br /><searchLink fieldCode="AR" term="%22Zhu%2C+Lei%22">Zhu, Lei</searchLink><relatesTo>4</relatesTo> (AUTHOR)<i> zhul@imde.ac.cn</i><br /><searchLink fieldCode="AR" term="%22Hu%2C+Bin%22">Hu, Bin</searchLink><relatesTo>1</relatesTo> (AUTHOR)<i> hubin2023@cug.edu.cn</i><br /><searchLink fieldCode="AR" term="%22Tang%2C+Huiming%22">Tang, Huiming</searchLink><relatesTo>1,5</relatesTo> (AUTHOR)<i> tanghm@cug.edu.cn</i> – Name: TitleSource Label: Source Group: Src Data: <searchLink fieldCode="JN" term="%22Quarterly+Journal+of+Engineering+Geology+%26+Hydrogeology%22">Quarterly Journal of Engineering Geology & Hydrogeology</searchLink>. May2026, Vol. 59 Issue 2, p1-13. 13p. – Name: Subject Label: Subjects Group: Su Data: <searchLink fieldCode="DE" term="%22Landslides%22">Landslides</searchLink><br /><searchLink fieldCode="DE" term="%22Water+waves%22">Water waves</searchLink><br /><searchLink fieldCode="DE" term="%22Theory+of+wave+motion%22">Theory of wave motion</searchLink><br /><searchLink fieldCode="DE" term="%22Computer+simulation%22">Computer simulation</searchLink><br /><searchLink fieldCode="DE" term="%22Earthquakes%22">Earthquakes</searchLink><br /><searchLink fieldCode="DE" term="%22Granular+flow%22">Granular flow</searchLink><br /><searchLink fieldCode="DE" term="%22Landslide+hazard+analysis%22">Landslide hazard analysis</searchLink><br /><searchLink fieldCode="DE" term="%22Rockslides%22">Rockslides</searchLink> – Name: Abstract Label: Abstract Group: Ab Data: Surge waves generated by landslides can lead to catastrophic consequences, including severe economic losses and loss of life. This study investigates the surge waves induced by the Mogangling landslide triggered by the 1786 Moxi earthquake through a combination of numerical simulations and field surveys. A detailed field investigation was conducted to characterize the engineering geological features of the Mogangling landslide. Based on the point cloud data, a 3D landslide model was constructed and used for numerical simulations. The landslide motion was simulated using a granular flow model, and wave propagation was modelled using the renormalization group turbulence model. These two models were coupled to analyse the generation and evolution of the landslide-induced surge waves. The simulation results indicate that the peak sliding velocity of the landslide approached 20 m s−1. As the landslide mass entered the Dadu River, a large landslide-dam formed, temporarily blocking the river and generating intense surge waves. The peak water velocity increased to 30 m s−1, and the maximum wave height reached 81.78 m, which is consistent with the historical record of roughly 80 m. The surge waves propagated in a circular pattern toward the opposite riverbank. The findings provide insights for the risk assessment of landslide-induced surge waves. [ABSTRACT FROM AUTHOR] – Name: AbstractSuppliedCopyright Label: Group: Ab Data: <i>Copyright of Quarterly Journal of Engineering Geology & Hydrogeology is the property of Geological Society Publishing House and its content may not be copied or emailed to multiple sites without the copyright holder's express written permission. Additionally, content may not be used with any artificial intelligence tools or machine learning technologies. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract.</i> (Copyright applies to all Abstracts.) |
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| RecordInfo | BibRecord: BibEntity: Identifiers: – Type: doi Value: 10.1144/qjegh2025-147 Languages: – Code: eng Text: English PhysicalDescription: Pagination: PageCount: 13 StartPage: 1 Subjects: – SubjectFull: Landslides Type: general – SubjectFull: Water waves Type: general – SubjectFull: Theory of wave motion Type: general – SubjectFull: Computer simulation Type: general – SubjectFull: Earthquakes Type: general – SubjectFull: Granular flow Type: general – SubjectFull: Landslide hazard analysis Type: general – SubjectFull: Rockslides Type: general Titles: – TitleFull: Three-dimensional dynamic simulation of waves produced by landslides: an analysis of the Mogangling landslide caused by the Moxi earthquake in 1786. Type: main BibRelationships: HasContributorRelationships: – PersonEntity: Name: NameFull: Ge, Yunfeng – PersonEntity: Name: NameFull: Shao, Xianyun – PersonEntity: Name: NameFull: Fu, Xiaodong – PersonEntity: Name: NameFull: Zhu, Lei – PersonEntity: Name: NameFull: Hu, Bin – PersonEntity: Name: NameFull: Tang, Huiming IsPartOfRelationships: – BibEntity: Dates: – D: 01 M: 05 Text: May2026 Type: published Y: 2026 Identifiers: – Type: issn-print Value: 14709236 Numbering: – Type: volume Value: 59 – Type: issue Value: 2 Titles: – TitleFull: Quarterly Journal of Engineering Geology & Hydrogeology Type: main |
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