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Titel A research of phase velocity of roll waves for debris flow
VerfasserIn M. Arai
Konferenz EGU General Assembly 2012
Medientyp Artikel
Sprache Englisch
Digitales Dokument PDF
Erschienen In: GRA - Volume 14 (2012)
Datensatznummer 250064567
 
Zusammenfassung
This research is phase velocity of roll waves on debris flows. Phase velocity of roll waves has different characteristics with mean velocity. Using the momentum and mass conservation equations in a coordinate system moving with velocity c for a homogeneous fluid are as follows c-ˆ‚U– βU -ˆ‚U-+ c(1 - β )U--ˆ‚A--ˆ‚H = - g sinθ + g cosθ-ˆ‚H + f′U-2 -ˆ‚ξ -ˆ‚ξ A -ˆ‚H -ˆ‚ ξ -ˆ‚ξ 2 R ( ) -ˆ‚A--ˆ‚H- -ˆ‚U- U - c -ˆ‚H -ˆ‚ξ + A -ˆ‚ξ = 0 here, v(x,t) = U(x - ct) = U(ξ), h(x,t) = H(x - ct) = H(ξ), ξ = x - ct, v : cross-sectional mean velocity, h : depth of flow, A : cross-sectional flow area, g : acceleration due to gravity, θ : slope angle of the channel, R : hydraulic radius, β : momentum correction factor, f′ : friction factor, x : coordinate axis of flow direction, t : time, the occurrence condition of roll waves is obtained. From other way to obtain the occorrence condition, the ratio U -0c which U0 is mean velocity at control section and c phase velocity (velocity of a coordinate system moving) is obtained, and under the condition that the channel is rectanglar and the width B of channel is much wider than the depth (B -‰« H), the ratio of U c0 is led as follows, ° –––––––– ( ) S–1- U0- β––β-β–-1-+-B-Fr2- c = S 1 β - B-F-2 r here, Fr = –U–– -ˆšgHcosθ : Froude number, S : wetted perimeter. Experiments have been conducted in an experimental flume of 28m in length, 10cm in width and 10cm in depth. In a circulation system the tested material is pumped from the extit of the flume back to the inlet, providing a constant discharge upstream. The material used consisted of non-cohesive coal particles with a d50 of 0.67mm, a density Ïă of 1.41g/cm3 and polypropylene particles with a d50 of 2.9mm, a density Ïă of 1.06g/cm3. The experimental results and theoretical result (equation (3)) are correspondig well on β = 1.02.