TY - JOUR

T1 - Modeling of non-hydroplaning mudflows on continental slopes

AU - Huang, Xin

AU - García, Marcelo H.

N1 - Funding Information:
The financial support of the Geology and Geophysics Program (Grant N0014-93-1-0044) in the US Office of Naval Research with J. Kravitz as program director is gratefully acknowledged. Critical reviews of an early draft by C.A. Nittrouer, A.J. Mehta, K.X. Whipple and two anonymous reviewers significantly improved the manuscript. The authors are grateful to all of them.

PY - 1999/2/2

Y1 - 1999/2/2

N2 - An analytical model is proposed for two-dimensional, laminar, non-hydroplaning mudflows resulting from submarine slides that occur in deep waters, have substantial runout distances, and can be approximated as Bingham fluids. Length-scale analysis indicates that the dynamics of the mudflows can be treated in two regions: the outer region away from the flow front and the inner region near the flow front. The model, obtained by a matched-asymptotic method, can predict the asymptotic runout characteristics of submarine, non-hydroplaning mudflows as well as subaerial mudflows. A critical condition for hydroplaning to occur is found with the help of the model. The model can be used to predict the evolution of submarine slides such as velocities and time scales, and to interpret the deposits generated by them. As an example, a hypothetical submarine slide on a slope of 2°is considered. The initial sediment mass has a maximum thickness of 7.25 m, a maximum length of 207.6 m, and a volume of 752.6 m3/m. For a bulk density of 2.0 t/m3, a kinematic viscosity of 0.005 m2/s, and a yield stress of 200 N/m2, the propagating velocity of the flow front is predicted to be 2.3 m/s after about 30 S, and then to decrease along the flow path, producing a deposit 0.58 m thick and 1.3 km long. The final stage of the slide is similar to a creeping motion.

AB - An analytical model is proposed for two-dimensional, laminar, non-hydroplaning mudflows resulting from submarine slides that occur in deep waters, have substantial runout distances, and can be approximated as Bingham fluids. Length-scale analysis indicates that the dynamics of the mudflows can be treated in two regions: the outer region away from the flow front and the inner region near the flow front. The model, obtained by a matched-asymptotic method, can predict the asymptotic runout characteristics of submarine, non-hydroplaning mudflows as well as subaerial mudflows. A critical condition for hydroplaning to occur is found with the help of the model. The model can be used to predict the evolution of submarine slides such as velocities and time scales, and to interpret the deposits generated by them. As an example, a hypothetical submarine slide on a slope of 2°is considered. The initial sediment mass has a maximum thickness of 7.25 m, a maximum length of 207.6 m, and a volume of 752.6 m3/m. For a bulk density of 2.0 t/m3, a kinematic viscosity of 0.005 m2/s, and a yield stress of 200 N/m2, the propagating velocity of the flow front is predicted to be 2.3 m/s after about 30 S, and then to decrease along the flow path, producing a deposit 0.58 m thick and 1.3 km long. The final stage of the slide is similar to a creeping motion.

KW - Bingham plastic fluid

KW - Continental slope

KW - Gravity flow

KW - Modeling

KW - Mudflow

KW - Submarine slide

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U2 - 10.1016/S0025-3227(98)00108-X

DO - 10.1016/S0025-3227(98)00108-X

M3 - Article

AN - SCOPUS:0033514332

VL - 154

SP - 131

EP - 142

JO - Marine Geology

JF - Marine Geology

SN - 0025-3227

IS - 1-4

ER -