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- W2125324684 abstract "Debris flow is generally composed of a wide range of solid particles and viscous pore fluid. It flows at a high velocity down a slope channel. Interactions between solid and fluid phases affected by multiple parameters govern the rheological properties of debris flows. A dimensional analysis for a systematic study of the governing parameters is presented. Multiple dimensionless numbers with clear physical meanings are critically reviewed. The applications of field data to the studying of natural debris flows are demonstrated. Specific values of dimensionless numbers for classifying flow regimes of large-scale natural debris flows are obtained. Compared with previous small-scale physical model tests, this study shows that the contact friction between particles dominates in natural debris flows. In addition, the solid inertial stress due to particle collisions and the pore-fluid viscous shearing stress play key roles in governing the dynamic properties of debris flows. The channel width as a confinement to the flows can affect the solids discharge per unit width significantly. A dimensionless number related to pore-fluid pressure dissipation is also found that can satisfactorily distinguish between surge flows and continuous flows in the field." @default.
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- W2125324684 date "2010-07-01" @default.
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- W2125324684 title "Dimensional analysis of natural debris flows" @default.
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- W2125324684 doi "https://doi.org/10.1139/t09-134" @default.
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