Influence analysis of spatially variable cohesion on flow process and run-out distance of landslides
Author:
Funder
National Natural Science Foundation of China
Natural Science Foundation of Jiangsu Province
Publisher
Springer Science and Business Media LLC
Link
https://link.springer.com/content/pdf/10.1007/s11069-024-06443-1.pdf
Reference47 articles.
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2. Bao Y, Huang Y, Liu G, Wang G (2020a) SPH simulation of high-volume rapid landslides triggered by earthquakes based on a unified constitutive model part I initiation process and slope failure. Int J Comp Meth-Sing 17(4):1850150. https://doi.org/10.1142/S0219876218501505
3. Bao Y, Huang Y, Liu G, Zeng W (2020b) SPH simulation of high-volume rapid landslides triggered by earthquakes based on a unified constitutive model. part II: solid–liquid-like phase transition and flow-like landslides. Int J Comp Meth-Sing 17(4):1850149. https://doi.org/10.1142/S0219876218501499
4. Braun A, Cuomo S, Petrosino S, Wang X, Zhang L (2018) Numerical SPH analysis of debris flow run-out and related river damming scenarios for a local case study in SW China. Landslides 15(3):535–550. https://doi.org/10.1007/s10346-017-0885-9
5. Cheng H, Huang Y, Zhang W, Xu Q (2022) Physical process-based runout modeling and hazard assessment of catastrophic debris flow using SPH incorporated with ArcGIS: A case study of the Hongchun gully. CATENA 212:106052. https://doi.org/10.1016/j.catena.2022.106052
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