The perfect debris flow? Aggregated results from 28 large-scale experiments

Aggregation of data collected in 28 controlled experiments reveals reproducible debris‐flow behavior that provides a clear target for model tests. In each experiment ∼10 m3 of unsorted, water‐saturated sediment composed mostly of sand and gravel discharged from behind a gate, descended a steep, 95‐m...

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Vydáno v:	Journal of Geophysical Research. F. Earth Surface Ročník 115; číslo F3
Hlavní autoři:	Iverson, Richard M., Logan, Matthew, LaHusen, Richard G., Berti, Matteo
Médium:	Journal Article
Jazyk:	angličtina
Vydáno:	Washington, DC Blackwell Publishing Ltd 01.09.2010 American Geophysical Union
Témata:	Boundary conditions Debris Debris flow Detritus Dispersions Earth sciences Earth, ocean, space Exact sciences and technology experiments Flow resistance Fractals Geomorphology Geophysics Gravel Hydrology Landslides & mudslides Levees Mathematics Mud Nonlinear systems Particle size pore pressure Porosity Rheology Roughness Sediments Segregations Time series experimental studies models mobility thickness pore fluid debris flows aggregation friction grains gravel sand grain size Normal stress fluid pressure pore pressure roughness debris Flow velocity Height flumes segregation mud boundary conditions flow
ISSN:	0148-0227, 2169-9003, 2156-2202, 2169-9011
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