Rapid changes of sediment dynamic processes in Yalu River Estuary under anthropogenic impacts  

作　　者：Jian-hua GAO Jun LI Harry WANG Fen-long BAI Yan CHENG Ya-ping WANG 

机构地区：[1]Key Laboratory for Coast and Island Development of Ministry of Education,Nanjing University [2]Qingdao Institute of Marine Geology [3]Virginia Institute of Marine Science,Gloucester Point,VA 23062,United States Prof. [4]School of Urban Construction,East Liaoning University [5]Key Laboratory for Coast and Island Development,Ministry of Education,Nanjing University

出　　处：《International Journal of Sediment Research》2012年第1期37-49,共13页国际泥沙研究（英文版）

基　　金：supported by Natural Science Foundation of China(No.40976051,40506022,40976036, 40871019);the Project Funded by the Priority Academic Program Development of Jiangsu Higher Education Institutions

摘　　要：The response of the Yalu River Estuary to human activities was investigated. Changes of sediment dynamics during the past 10 years were explored through hydrodynamic calculation, as well as heavy mineral and grain size analysis. In addition, the characteristics of estuarine geomorphological evolution were compared with historical data. The long-term sediment dynamic process and geomorphological evolution were primarily affected by the decrease of water discharge and sediment supply resulting from human activities. The entire estuarine system of Yalu River Estuary has also undergone significant changes since 1941 that are associated with water reduction and sediment discharge affected by construction reservoirs. The estuary eventually formed the current patterns in the 1980s. Compared with variations of water and sediment discharge, sand dredging directly affected the estuarine sediment dynamics in the past 10 years. Data from six hydrodynamic stations measured in 2009 indicated that the bedload transport flux has substantially decreased during a tidal cycle compared with that surveyed in 1996. The bedload transport direction also changed from seaward in 1996 to landward in 2009. In addition, the estuarine bed load movement changes were： （a） sediment from areas with water depth being less than 5 m was transported from the sea towards the land; （b） sediment transport from areas with water depth between 5 to 20 m was oriented towards the sea; and （c） sediment from areas with water depth greater than 20 m was conveyed from the sea towards the land.The response of the Yalu River Estuary to human activities was investigated. Changes of sediment dynamics during the past 10 years were explored through hydrodynamic calculation, as well as heavy mineral and grain size analysis. In addition, the characteristics of estuarine geomorphological evolution were compared with historical data. The long-term sediment dynamic process and geomorphological evolution were primarily affected by the decrease of water discharge and sediment supply resulting from human activities. The entire estuarine system of Yalu River Estuary has also undergone significant changes since 1941 that are associated with water reduction and sediment discharge affected by construction reservoirs. The estuary eventually formed the current patterns in the 1980s. Compared with variations of water and sediment discharge, sand dredging directly affected the estuarine sediment dynamics in the past 10 years. Data from six hydrodynamic stations measured in 2009 indicated that the bedload transport flux has substantially decreased during a tidal cycle compared with that surveyed in 1996. The bedload transport direction also changed from seaward in 1996 to landward in 2009. In addition, the estuarine bed load movement changes were： （a） sediment from areas with water depth being less than 5 m was transported from the sea towards the land; （b） sediment transport from areas with water depth between 5 to 20 m was oriented towards the sea; and （c） sediment from areas with water depth greater than 20 m was conveyed from the sea towards the land.

关 键 词：Sediment dynamics GEOMORPHOLOGY Human activities Yalu River Estuary 

分 类 号：TV148[水利工程—水力学及河流动力学]