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《Oceanologia Et Limnologia Sinica》 1992-01
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THE DYNAMICAL PROCESS OF SEDIMENTATION IN LEQING BAY

Xu Weiyi, Chen Gengxin and Li Bogen(Second Institute of Oceanography, SOA, Hangzhou, 310012)  
A two-dimensional numerical simulation is made for the tide and the path of sedimental transportation in Leqing Bay. It presents the processes of the transportation, siltafion of the sediment quantitatively.The results show that the 10 m isobath is the demarcation line. In the eastern area off this line, the flood current comes mainly from the waterway between the Yuhuan Island and the Henzhi Island. The trajectory of the flow in one spring tidal day is a narrow belt. For the net transportation of sediment from north to south it is the dynamical condition of maintaining the deep waterway off the Damaiyu Port. In the western area off 10 m isobath the trajectory of flow is for the transportation of sediment to west and north-west, the trajectory of flow near the Huaqi Flat is for the transportation of sediment to north and west, both contributing to the development of the Huaqi Flat.Before building the Xuanmen Dam, the standing wave of tide and funnel-type topography are the main condition for the formation of the characteristic Chumen Flat.
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