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Guo Xingjie, Cheng Heqin, Mo Ruoyu, Yang Zhongyong. Statistical characteristics and transport law of sand waves in the Yangtze Estuary[J]. Haiyang Xuebao, 2015, 37(5): 148-158. doi: 10.3969/j.issn.0253-4193.2015.05.014
Citation: Guo Xingjie, Cheng Heqin, Mo Ruoyu, Yang Zhongyong. Statistical characteristics and transport law of sand waves in the Yangtze Estuary[J]. Haiyang Xuebao, 2015, 37(5): 148-158. doi: 10.3969/j.issn.0253-4193.2015.05.014

Statistical characteristics and transport law of sand waves in the Yangtze Estuary

doi: 10.3969/j.issn.0253-4193.2015.05.014
  • Received Date: 2014-05-18
  • Rev Recd Date: 2014-10-18
  • The underwater topography at the South Channel,North Passage,Channel of Hengsha and North Channel of the Yangtze Estuary were surveyed by using multibeam echo-sounding system,wave height,wavelength,inflow angle,the dorsal stream angle and sediment characteristics of sand waves in these areas were calculated statistically,and the net displacement of sand waves in one tidal period was estimated on the basis of data for flow rate,grain sizes of sediments and water depths. The results showed that the sand waves in the Yangtze Estuary were basically large,and there took on a proportional relationship between wavelengths with sediment particle sizes. The symmetry of sand waves is different among all surveyed area in the Yangtze Estuary. The more obvious the ebb flow is,the worse the symmetry of sand wave and the more net displacement is. The symmetry of sand waves can reflect the power of water and net displacement of sand waves.
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