A simple lumped mass model to describe velocity of granular flows in a large flume
文献类型:期刊论文
作者 | Yang Qingqing1; Cai Fei1; Ugai, Keizo1; Su Zhiman2![]() ![]() ![]() |
刊名 | JOURNAL OF MOUNTAIN SCIENCE
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出版日期 | 2012-04-01 |
卷号 | 9期号:2页码:221-231 |
关键词 | Granular flow Large-scale flume test Mass-front velocity Deposit characteristic |
ISSN号 | 1672-6316 |
通讯作者 | CAI Fei |
英文摘要 | This paper presents a lumped mass model to describe the run-out and velocity of a series of large flume tests, which was carried out to investigate some propagation mechanisms involved in rapid, dry, dense granular flows and energy transformation when the flows encountered obstacles and reoriented their movement directions. Comparisons between predicted and measured results show that the trend of predicted velocities was basically matched with that of measured ones. Careful scrutiny of test videos reveals that subsequent particles with a higher velocity collided with slowed fronts to make them accelerate. However, this simple model cannot reflect collisions between particles because it treated released materials as a rigid block. Thus, the predicted velocity was somewhat lower than the measured velocity in most cases. When the flow changed its direction due to the variation in slope inclination, the model predicted a decrease in velocity. The predicted decrease in velocity was less than the measured one within a reasonable range of 10% or less. For some cases in which a convexity was introduced, the model also predicted the same trend of velocities as measured in the tests. The velocity increased greatly after the materials took a ballistic trajectory from the vertex of the convexity, and reduced dramatically when they finally made contact with the base of the lower slope. The difference between prediced and measured decrease in velocity was estimated to be about 5% due to the landing. Therefore, the simple lumped mass model based on the energy approach could roughly predict the run-out and velocity of granular flows, although it neglected internal deformation, intergranular collision and friction. |
WOS标题词 | Science & Technology ; Life Sciences & Biomedicine |
类目[WOS] | Environmental Sciences |
研究领域[WOS] | Environmental Sciences & Ecology |
关键词[WOS] | 5.12 WENCHUAN EARTHQUAKE ; INDUCED SLOPE FAILURE ; ROCK AVALANCHES ; ENERGY APPROACH ; LANDSLIDES ; TESTS ; PREDICTIONS ; GRAVEL ; SCALE |
收录类别 | SCI |
语种 | 英语 |
WOS记录号 | WOS:000301788100009 |
公开日期 | 2013-04-15 |
源URL | [http://192.168.143.20:8080/handle/131551/5082] ![]() |
专题 | 成都山地灾害与环境研究所_Journal of Mountain Science _Journal of Mountain Science-2012_Vol9 No.2 成都山地灾害与环境研究所_山地灾害与地表过程重点实验室 |
作者单位 | 1.Gunma Univ, Dept Civil & Environm Engn, Kiryu, Gumma 3768515, Japan 2.Chinese Acad Sci, Inst Mt Hazards & Environm, Chengdu 610041, Peoples R China 3.Chengdu Univ Technol, State Key Lab Geohazard Prevent & Geoenvironm Pro, Chengdu 610059, Peoples R China |
推荐引用方式 GB/T 7714 | Yang Qingqing,Cai Fei,Ugai, Keizo,et al. A simple lumped mass model to describe velocity of granular flows in a large flume[J]. JOURNAL OF MOUNTAIN SCIENCE,2012,9(2):221-231. |
APA | Yang Qingqing,Cai Fei,Ugai, Keizo,Su Zhiman,Huang Runqiu,&Xu Qiang.(2012).A simple lumped mass model to describe velocity of granular flows in a large flume.JOURNAL OF MOUNTAIN SCIENCE,9(2),221-231. |
MLA | Yang Qingqing,et al."A simple lumped mass model to describe velocity of granular flows in a large flume".JOURNAL OF MOUNTAIN SCIENCE 9.2(2012):221-231. |
入库方式: OAI收割
来源:成都山地灾害与环境研究所
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