ROLL WAVES ON A LAYER OF A MUDDY FLUID FLOWING DOWN A GENTLE SLOPE - A BINGHAM MODEL

被引:76
作者
LIU, KF [1 ]
MEI, CC [1 ]
机构
[1] MIT,DEPT CIVIL & ENVIRONM ENGN,CAMBRIDGE,MA 02139
关键词
D O I
10.1063/1.868148
中图分类号
O3 [力学];
学科分类号
08 ; 0801 ;
摘要
To study rapid and laminar flow of a mud layer down a gentle slope, a shallow layer of Bingham fluid is considered. Attention is focused on long waves of finite amplitude. Convective inertia is kept in the approximate equations which are simplified by Karman's momentum integral approach with an assumed velocity profile. A linearized instability analysis is first carried out for periodic disturbances. The nonlinear development of unstable disturbances is computed numerically to study the formation of periodic shocks, or roll waves. Nonlinear motion caused by external influx to an otherwise steadily flowing mud layer is also investigated.
引用
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页码:2577 / 2590
页数:14
相关论文
共 30 条
[1]  
ALEXEENKOV SV, 1985, AICHE J, V31, P1446
[2]  
Anderson D. A., 2020, COMPUTATIONAL FLUID, VFourth
[3]   THE YIELD STRESS MYTH [J].
BARNES, HA ;
WALTERS, K .
RHEOLOGICA ACTA, 1985, 24 (04) :323-326
[4]   WAVE FORMATION IN LAMINAR FLOW DOWN AN INCLINED PLANE [J].
BENJAMIN, TB .
JOURNAL OF FLUID MECHANICS, 1957, 2 (06) :554-574
[5]  
Bolt B. A., 1977, GEOLOGICAL HAZARDS
[6]  
Brock R.R., 1969, J HYDRAUL DIV, V95, P1401, DOI [10.1061/JYCEAJ.0002132, DOI 10.1061/JYCEAJ.0002132]
[7]  
Burden R.L., 1978, NUMERICAL ANAL
[8]   LARGE DEBRIS FLOWS - A MACRO-VISCOUS PHENOMENON [J].
DAVIES, TRH .
ACTA MECHANICA, 1986, 63 (1-4) :161-178
[9]  
Dent J. D., 1983, Annals of Glaciology, V4, P42