INITIATION OF RIPPLE MARKS UNDER OSCILLATING WATER

被引:14
作者
KANEKO, A [1 ]
HONJI, H [1 ]
机构
[1] KYUSHU UNIV, APPL MECH RES INST, FUKUOKA 8168580, JAPAN
关键词
D O I
10.1111/j.1365-3091.1979.tb00340.x
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
It was observed that a monolayer of glass beads which were scattered sparsely on a rigid plane floor grew into regular waves of particles under oscillatory water flow. The relative displacement of two nearby particles due to viscous fluid forces seems to be responsible for the initiation of these particle waves. It was also observed that the similar particle waves were formed on the initially flat surface of a thick sand bed and subsequently developed into oscillatory sand ripples of a common type. On the basis of these observations, it is suggested that the particle waves may be the basic cause of the initiation of general ripple marks under oscillatory flow. Copyright © 1979, Wiley Blackwell. All rights reserved
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页码:101 / 113
页数:13
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