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ZHANG Chun-sheng, LIU Zhong-bao, SHI Dong, CHENG Qi-gui, ZHANG Rong-bing, GAO Chun-ning, LI Jian-xiong. The Simulation Experiment of Surge-Type Turbidity Current Formation and Development[J]. Acta Sedimentologica Sinica, 2002, 20(1): 25-29.
Citation: ZHANG Chun-sheng, LIU Zhong-bao, SHI Dong, CHENG Qi-gui, ZHANG Rong-bing, GAO Chun-ning, LI Jian-xiong. The Simulation Experiment of Surge-Type Turbidity Current Formation and Development[J]. Acta Sedimentologica Sinica, 2002, 20(1): 25-29.

The Simulation Experiment of Surge-Type Turbidity Current Formation and Development

  • Received Date: 2001-07-04
  • The momentum equation of underflows-type turbidity and surge-type turbidity current is compared in this paper,and the result indicates that the surge-type turbidity current entrains water not only through its upper surface but also through its front. At the slope of 0°,5°,10°, surge-type turbidity current experiments reveals that the head of the turbidity current is overhanging and is divided transversely into roughly periodic buttock-shaped lobes and clefts, on account of the mixing, the body of a turbidity current in deep water flows about 25% faster than the head, the moment process of the surge-type turbidity current shows the characteristics of wave, and back-wave transcendental front-wave. the turbidity current consumes itself in the process of mixing into the ambient medium. The flow height and velocity of surge-type turbidity current is proportional to the motion distance and under slope. Close to the bottom of the turbidity current, there is a considerable increase in density and there may even be a thin layer with bed-load flow. There is not such characteristic in the underflow-type turbidity current.
  • [1] Middleton G V.Small-scale models of turbidity currents and criterion for autosuspension[J].J.Sedim.Petrol.1966a,36:202~208
    [2] Middleton G V.Experiments on density and turbidity currents,I.Motion of the head[J].Can.J.Earth.Sci.1966b,3:523~546
    [3] Middleton G V.Experiments on density and turbidity currents,II.Uniform flow of density currents[J].Can.J.Earth.Sci.1966c,3:627~637
    [4] Kuenen P H.Estimated size of the Grand Banks turbidity current[J].Am.J.Sci.1952.250:874~884
    [5] Luthi S.Experiments on non-channelized turbidity currents and their deposits[J].Mar.Geol.1981a,40:59~68
    [6] Luthi S.Some new aspects of two-dimensional turbidity currents[J].Sedimentology,1981b,28:97~105
    [7] Leeder M R.On the dynamics of sediment suspension by residual Reynolds stresses-confirmation of Bagnold's theory[J].Sedimentology.1983,30:91~485
    [8] Keyu L.Submarine of features of modern open-sea fan deltas,Huon peninsula,Papua new Gwined[J].Sedimentary Geology,1995,98(1):63~77
    [9] Sumer B M,Deigaard R.Particle motions near the bottom in turbulent flow in an open channel[J].J.Fluid Mech.1981,109:38~311
    [10] Mctigue D F.Mixture theory for suspended sediment transport[J].J.Hydraul.Div.Am.Soc.Civ.Engrs,1981,107:73~659
    [11] Kersey D G,Hsu K J.Energy relations of density-current flows:an experimental investigation[J] Sedimentology,1976,23:761~789
    [12] Southard J B,Mackintosh M E.Experimental test of autosuspension[J].Earth Surf.Proc.Landforms,1981,6:11~103
    [13] 张春生,刘忠保,施东等.扇三角洲形成过程及演变规律[J].沉积学报,2000,18(4):521~526
    [14] Tochon-Danguy J C,Hopfinger E J.Simulation of powder-snow avalanches[J].Proc.Grindel-wald Symp.,Snow Mech.Symp.,IAHS-AIHS Publ.,1975,14:369~380
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  • Received:  2001-07-04

The Simulation Experiment of Surge-Type Turbidity Current Formation and Development

Abstract: The momentum equation of underflows-type turbidity and surge-type turbidity current is compared in this paper,and the result indicates that the surge-type turbidity current entrains water not only through its upper surface but also through its front. At the slope of 0°,5°,10°, surge-type turbidity current experiments reveals that the head of the turbidity current is overhanging and is divided transversely into roughly periodic buttock-shaped lobes and clefts, on account of the mixing, the body of a turbidity current in deep water flows about 25% faster than the head, the moment process of the surge-type turbidity current shows the characteristics of wave, and back-wave transcendental front-wave. the turbidity current consumes itself in the process of mixing into the ambient medium. The flow height and velocity of surge-type turbidity current is proportional to the motion distance and under slope. Close to the bottom of the turbidity current, there is a considerable increase in density and there may even be a thin layer with bed-load flow. There is not such characteristic in the underflow-type turbidity current.

ZHANG Chun-sheng, LIU Zhong-bao, SHI Dong, CHENG Qi-gui, ZHANG Rong-bing, GAO Chun-ning, LI Jian-xiong. The Simulation Experiment of Surge-Type Turbidity Current Formation and Development[J]. Acta Sedimentologica Sinica, 2002, 20(1): 25-29.
Citation: ZHANG Chun-sheng, LIU Zhong-bao, SHI Dong, CHENG Qi-gui, ZHANG Rong-bing, GAO Chun-ning, LI Jian-xiong. The Simulation Experiment of Surge-Type Turbidity Current Formation and Development[J]. Acta Sedimentologica Sinica, 2002, 20(1): 25-29.
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