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《Acta Sedimentologica Sinica》 2006-04
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Mechanism of Silt-mud Couplet of Mud Tidal Flat and Discrimination Criteria of Storm Surge Sedimentation in the Middle Jiangsu Province

WANG Jian~(1) BAI Chun-guang~(1,2) ~() Xu Yong-hui~(1,3)(1.College of Geographical Sciences,Nanjing Normal University,Nanjing 210097; 2.Transportation College,Southeast University,Nanjing 210096;3.Department of Urban and Resource Sciences,Nanjing University,Nanjing 210093)  
Field observation on the formation and development process of silt-mud couplets is carried out on tidal flat of the middle Jiangsu province.Combined the observation result with the calculation of sedimentation quantity and the analysis of grain-size and roundness of sedimentary particles,the mechanism of silt-mud couplets is revealed in this area.One thin silt-mud couplet with the thickness of millimeters is formed during a flood-ebb tidal cycle,and one thick couplet with the thickness of centimeters is formed during a springneap tidal cycle.In addition to the research on the formation of silt-mud couplets,the field observation on the tidal flat is carried out before and after the storm surge for typhoon No.9711.The result shows that even during storm surge period,high tidal flat can still be in sedimentation over some places,no erosion occurred.Compared with the normal tidal flat sedimentation,the storm sedimentation has the characteristics of coarse particle,bad sorting,relatively high roundness,obviously graded bedding,typical parallel bedding,cross bedding.
【Fund】: 国家自然科学基金项目(批准号:49601019);; 国家重点基础和发展规划项目(2003CB415201-8);; 国家教育振兴计划教育部青年教师奖励基金(批准号:2001JBC12)资助
【CateGory Index】: P512.2
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