2012
DOI: 10.1016/j.margeo.2011.01.001
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The sand ridge field of the South Yellow Sea: Origin by river–sea interaction

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Cited by 89 publications
(79 citation statements)
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“…These results indicate that: 1) before the sand ridges were generated, the sediments were carried by residual currents; 2) the original source of the sediment could be either the ancient Yellow River estuary or Yangtze River estuary. This hydrodynamic finding is consistent with the environmental magnetism results [16] and the sediment composition results [17]. Once the sand ridges had been formed, the Lagrangian residual current varied (shown in Figure 8(b)).…”
Section: Lagrange Residual Currentsupporting
confidence: 88%
“…These results indicate that: 1) before the sand ridges were generated, the sediments were carried by residual currents; 2) the original source of the sediment could be either the ancient Yellow River estuary or Yangtze River estuary. This hydrodynamic finding is consistent with the environmental magnetism results [16] and the sediment composition results [17]. Once the sand ridges had been formed, the Lagrangian residual current varied (shown in Figure 8(b)).…”
Section: Lagrange Residual Currentsupporting
confidence: 88%
“…These sand shoals are about 200 km long and 100 km wide, and feature a pinwheel shape. These sand shoals are hypothesized to have formed from the high sediment discharges by the Yellow and Yangtze Rivers (Wang et al, 2012). The unique radial geomorphology of the sand shoals affects tidal current and result in eddies forming in the deep channels between sand shoals (Du, 2012) (Fig.…”
Section: Conjectures About the Original Sources Of Propagules For Grementioning
confidence: 99%
“…In our case, the average erosion risk-index above 0. 5 shows a strong hydraulic regime with tidal ridge existence. In the previous study, the tidal sand ridges existing in the zone A, B, C, E, F have been widely cited ( Figure 1, Chough et al, 2002;Li et al, 2001;Liu et al, 1998;Park & Lee, 1994;Wang et al, 2012) . The recent discovered sand ridges in the Bohai Sea ( Wang et al, 2006;Wang et al, 2015 ) which are in the corresponding zone D and G in the research domain give a good proof that erosion risk might be a good clue in looking for the potential location of sand ridge.…”
Section: Discussionmentioning
confidence: 94%
“…More and more coastal engineering projects like offshore construction or seabed pipeline routing request to estimate the potential of erosion on the seafloor bottom surface, to investigate the occurrence of special bottom morphology, e. g. tidal sand ridge distribution and development along Chinese coasts ( Liu et al, 1998;Swift, 1975;Wang et al, 2012;Yang, 1989) . Considering the variety of bottom sediment types and specific sediment distribution patterns, a methodology of assessing and quantifying the status of bottom dynamics is required, studying the natural dynamics of surface sediment and its interaction with human activities.…”
Section: Introductionmentioning
confidence: 99%