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Enhanced mobility of polydisperse granular flows in a small flume
Abstract Background A series of laboratory tests was conducted to investigate the influence of the interaction between coarse and fine particles on the mobility of granular flows in a small flume. Methods The angle of the upper slope was fixed at 45°, and the lower slope was inclined at angles of 0°, 5°, 10°, and 15° in different cases. Three monodisperse materials (gravel, coarse sand, and fine sand) were mixed, and the proportion of each material in each test was varied but maintained the same total mass of 3.0 kg. Results Test results show that the proportion of fine sand strongly influenced the run-out of polydisperse materials. With increasing proportion of fine sand, the run-outs of granular flows increased until its peak. However, the run-outs decreased with further more fine sand. Discussion The reason might be that a thin layer of fine sand acted as rollers for the rolling of the gravel, leading to the reduction of effective friction resistance during the movement; when excessive amount of fine sand was involved, these rollers were thrown into disarray so that the particles were either blocked or forced into sliding. Conclusion This implies that an appropriate proportion of fine particles were partly responsible for the long run-out of rock avalanches.
Enhanced mobility of polydisperse granular flows in a small flume
Abstract Background A series of laboratory tests was conducted to investigate the influence of the interaction between coarse and fine particles on the mobility of granular flows in a small flume. Methods The angle of the upper slope was fixed at 45°, and the lower slope was inclined at angles of 0°, 5°, 10°, and 15° in different cases. Three monodisperse materials (gravel, coarse sand, and fine sand) were mixed, and the proportion of each material in each test was varied but maintained the same total mass of 3.0 kg. Results Test results show that the proportion of fine sand strongly influenced the run-out of polydisperse materials. With increasing proportion of fine sand, the run-outs of granular flows increased until its peak. However, the run-outs decreased with further more fine sand. Discussion The reason might be that a thin layer of fine sand acted as rollers for the rolling of the gravel, leading to the reduction of effective friction resistance during the movement; when excessive amount of fine sand was involved, these rollers were thrown into disarray so that the particles were either blocked or forced into sliding. Conclusion This implies that an appropriate proportion of fine particles were partly responsible for the long run-out of rock avalanches.
Enhanced mobility of polydisperse granular flows in a small flume
Yang, Qingqing (author) / Su, Zhiman (author) / Cai, Fei (author) / Ugai, Keizo (author)
Geoenvironmental Disasters ; 2 ; 1-9
2015-04-25
9 pages
Article (Journal)
Electronic Resource
English
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