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The role of fluid drag force in the dynamic process of two-phase flow-like landslides

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Abstract

During the landslide mobility process, there is a dynamic interaction between the sliding main body and the different surrounding media. This affects the mobility characteristics of the landslide, particularly the friction force and contact force, which play the significant roles of dissipating and transferring energy in the sliding main body, respectively. In order to analyze the dynamic characteristics of rapid and long-runout landslides, the discrete element method solver of EDEM software and the computational fluid dynamics code of ANSYS-Fluent solver for a two-phase flow-like landslide, combined with flume tests and a field case, were used to research the following points: (1) When the liquid volume fraction is large enough during the mobility process of a two-phase flow-like landslide, the liquid phase provides a certain drag force relative to the solid phase. (2) The drag force was determined from the volume fraction of the liquid, the solid–liquid velocity difference, and the viscosity coefficient of the liquid, which together affect the characteristics of the landslide’s mobility and accumulation. (3) According to the back analysis of the Xianchi Reservoir landslide, fluid drag force plays an important role in the actual landslide mobility process. Therefore, it is necessary to consider the influence of the fluid drag force in hazard zoning and the post-failure mobility process analysis of large-scale flow-like landslides.

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Funding

This study was financially supported by the National Natural Science Foundation of China (42177172 and 41907257), the Institute of Geo-Mechanics (DZLXJK201901), and the National Key Research and Development Program of China “The Disaster Pattern and Risk Prevention Technology of Large Landslides in the Karst Mountain Area” (2018YFC1504806).

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Correspondence to Yueping Yin.

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I certify that this manuscript is original and has not been published elsewhere while being considered, and that the study has not been split into several parts to increase the quantity of submissions and submitted to various journals or to one journal over time. No data have been fabricated or manipulated (including images) to support our conclusions. No data, text, or theories by others are presented as if they were our own. The submission has been received explicitly from all co-authors and authors whose names appear on the submission, and all have contributed sufficiently to the scientific work and therefore share collective responsibility and accountability for the results.

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Gao, Y., Yin, Y., Li, B. et al. The role of fluid drag force in the dynamic process of two-phase flow-like landslides. Landslides 19, 1791–1805 (2022). https://doi.org/10.1007/s10346-022-01858-y

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