Abstract
Rock avalanches have become a hot spot in the field of geological hazards due to their flow features and long run-out distance. These features are closely related to the mass ratio parameter mr (the proportion of fine particles to the total mass). To explore the influence on the kinetic parameters and deposit morphology of rock avalanches by mr, a tabletop apparatus was developed to conduct sand avalanche experiments. Direct shear tests were performed to provide strength parameters of sand and sand–plate interface systematically. The results show that with the decrease of mean particle size D50, the internal friction angle increases first and then decreases, but the opposite trend has been observed for the friction angle of sand–plate interface. The addition of fine particles smaller than 0.075 mm makes the motion behavior of the sliding mass different. With the increase of mr, the motion of sand avalanches changes from frictional flows to viscous flows. In addition, a critical mass ratio parameter is proposed. The critical mass ratio parameter increases with the increased range of particle sizes. This research supports the study of avalanche events.
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This study would not have been possible without the financial support from the National Natural Science Foundation of China under Grant Nos. 42177155, 41790442, 41702298, and 41602359 as well as the fellowship of China Postdoctoral Science Foundation Nos. 2020M683676XB. We thank Professor Alice Crossland, Professor Ke Gao, and the Team of Native English Editing (https: www.nativeee.com) for an English language editing.
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Conceptualisation: ZD and Y-BW, Funding acquisition: ZD, Conducting experiments and analysis: ZD, Y-BW, J-BP, and S-ZX; Writing: ZD and Y-BW.
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Duan, Z., Wu, YB., Peng, JB. et al. Characteristics of sand avalanche motion and deposition influenced by proportion of fine particles. Acta Geotech. 18, 1353–1372 (2023). https://doi.org/10.1007/s11440-022-01653-y
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DOI: https://doi.org/10.1007/s11440-022-01653-y