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《OCEANOLOGIA ET LIMNOLOGIA SINICA》 1997-04
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THE ACCRETION PROCESS OF THE HAIZHOU BAY MUD FLAT PROFILE

Fan Shejun; Yu Zhiying; Jin Liu+(State Key Laborator of Coastal & Estuarine Research, East China Normal University, Shanghai 200062)+(Headquarter of Lianyungang port Construction,Lian Yungang 222240)  
This paper reports results of studes on the mud flat of data obtained inHaizhou Bay. On the basis of field surveys of wave and sediment in December, 1986,and from March lst 1985 to March 1st 1987, and on the characteristics of hydrology,morphology in this area, a two-dimension model describing the ascretion of theHaizhou Bay, was established by combining knowledge of hydraulics, sedimentologyand sediment kinematics. The results showed that tide crrrent played a dominant rolein changes of the accretion mud flat; that waves are weakened sharply by the nearbottom suspended mud; and that its contribution to the shore is weak. In the accretionprocess of the mud flat,two convex points appeared : which one at the bottom of themean high water the other near the mean low water. The accretion of the former wasfaster than that of the latter. The subtidal zone accretion process was much slower.
【Fund】: 高等学校博士点基金!9426902
【CateGory Index】: P737
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