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FORMATION MECHANISM AND DEVELOPMENTAL CONDITIONS OF TIDAL CURRENT RIDGES
作者姓名:夏东兴  刘振夏
作者单位:First Institute of Oceanography, State Oceanic Administration, Qingdao;First Institute of Oceanography, State Oceanic Administration, Qingdao
摘    要:This paper discusses mainly the formation mechanism and developmental conditions of tidal current ridges. The tidal current velocities of 1-3.5 knots and the supply of abundant loose sediments are the prerequisites for the formation of the tidal current ridges. The hydrodynamic mechanism is similar to that of straight rivers. In the trough between two ridges the tidal current moves forward in the form of two helical flows. The two flows converge and sink in the centre of the trough, and erode the trough deeply; they diverge and rise on the two sides of the trough, and accumulate the ridges. When the supply material and relief come to the dynamic equilibrium, the development of ridges keeps steady.

收稿时间:1984/8/29 0:00:00
修稿时间:8/4/1985 12:00:00 AM

FORMATION MECHANISM AND DEVELOPMENTAL CONDITIONS OF TIDAL CURRENT RIDGES
XIA DONGXING and LIU ZHENXIA.FORMATION MECHANISM AND DEVELOPMENTAL CONDITIONS OF TIDAL CURRENT RIDGES[J].Acta Oceanologica Sinica,1986,5(2):247-255.
Authors:XIA DONGXING and LIU ZHENXIA
Institution:First Institute of Oceanography, State Oceanic Administration, Qingdao
Abstract:This paper discusses mainly the formation mechanism and developmental conditions of tidal current ridges.The tidal current velocities of 1-3.5 knots and the supply of abundant loose sediments are the prerequisites for the formation of the tidal current ridges.The hydrodynamic mechanism is similar to that of straight rivers.In the trough between two ridges the tidal current moves forward in the form of two helical flows.The two flows converge and sink in the centre of the trough,and erode the trough deeply; they diverge and rise on the two sides of the trough,and accumulate the ridges.When the supply material and relief come to the dynamic equilibrium,the development of ridges keeps steady.
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