A quasi single-phase model for debris flows and its comparison with a two-phase model
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摘要:
A depth-averaged quasi single-phase mixture model is proposed for debris flows over inclined bed slopes based on the shallow water hydrosediment-morphodynamic theory with multi grain sizes.The stresses due to fluctuations are incorporated based on analogy to turbulent flows,as estimated using the depth-averaged k-ε turbulence model and a modification component.A fully conservative numerical algorithm,using well-balanced slope limited centred scheme,is deployed to solve the governing equations.The present quasi single-phase model using four closure relationships for the bed shear stresses is evaluated against USGS experimental debris flow and compared with traditional quasi single-phase models and a recent physically enhanced two-phase model.It is found that the present quasi single-phase model performs much better than the traditional models,and is attractive in terms of computational cost while the two-phase model performs even better appreciably.