Granular and particle-laden flows: from laboratory experiments to field observations

被引:160
|
作者
Delannay, R. [1 ]
Valance, A. [1 ]
Mangeney, A. [2 ,3 ]
Roche, O. [4 ]
Richard, P. [5 ]
机构
[1] Univ Rennes 1, UMR CNRS 6251, Inst Phys Rennes, Campus Beaulieu Batiment 11A,263 Av Gen Leclerc, F-35042 Rennes, France
[2] Univ Paris Diderot, Sorbonne Paris Cite, Inst Phys Globe Paris, Seismol Grp, 1 Rue Jussieu, F-75005 Paris, France
[3] INRIA, CEREMA, ANGE Team, Lab J Louis Lions, Paris, France
[4] Univ Blaise Pascal, Lab Magmas & Volcans, OPGC, CNRS IRD, Campus Univ Cezeaux,6 Ave Blaise Pascal, F-63178 Aubiere, France
[5] LUNAM Univ, IFSTTAR, MAST, GPEM, Site Nantes,Route Bouaye, F-44344 Bouguenais, France
关键词
granular flows; geophysics; particle laden flows; SAVAGE-HUTTER TYPE; IRREGULAR 3-DIMENSIONAL TERRAIN; DEPTH-AVERAGED MU(I)-RHEOLOGY; 2-PHASE SEDIMENT TRANSPORT; SAINT VENANT EQUATIONS; DENSE INCLINED FLOWS; FREE-SURFACE FLOWS; MOUNT ST-HELENS; PYROCLASTIC FLOWS; SNOW AVALANCHE;
D O I
10.1088/1361-6463/50/5/053001
中图分类号
O59 [应用物理学];
学科分类号
摘要
This review article provides an overview of dry granular flows and particle fluid mixtures, including experimental and numerical modeling at the laboratory scale, large scale hydrodynamics approaches and field observations. Over the past ten years, the theoretical and numerical approaches have made such significant progress that they are capable of providing qualitative and quantitative estimates of particle concentration and particle velocity profiles in steady and fully developed particulate flows. The next step which is currently developed is the extension of these approaches to unsteady and inhomogeneous flow configurations relevant to most of geophysical flows. We also emphasize that the up-scaling from laboratory experiments to large scale geophysical flows still poses some theoretical physical challenges. For example, the reduction of the dissipation that is responsible for the unexpected long run-out of large scale granular avalanches is not observed at the laboratory scale and its physical origin is still a matter of debate. However, we believe that the theoretical approaches have reached a mature state and that it is now reasonable to tackle complex particulate flows that incorporate more and more degrees of complexity of natural flows.
引用
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页数:40
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