The Recent Microrelief Features of the Yangtze Estuary

Based on the bedforms date were made in the Yangtze estuary, China, during January 2010 and July 2015 with the acoustic multi-beam bathymetric and shallow sediment profiler and surface sediment samples collected recently, the microrelief features of the Yangtze Estuary under the human interference recently is studied. Results show that in addition to four types of common microrelief (smooth bedfloors , sandwaves, hollow and gully), but also there are two types of microrelief under the human interference (sand and dredging mark).Restricted by the nature of sediment, sand waves exist only in the local region of the South Channel, the North Channel、the South Passage and the Hengsha passage whose main types of the surface sediment was fine sand. Under the combined effect of a series of large-scale engineering with watershed and estuary, the upper reach of North Channel, the Hengsha passage, the upper reach of south Channel and the upper reach of the South passage are subject to different degrees of erosion recently, so there are varying degrees of erosive microrelief (hollow and gully). Due to dredging engineering and artificial disordered mining, there are a huge range of dredging mark in the lower reach of South Channel, Yuanyuansha channel and North passage and there are a degree of sand in the main channel of south side of Ruifengsha.