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MOE KLCID. Nanjing University. Estuary flocculation and sediment dynamics in Jiulong River mouth. Yang Yang (杨 旸) yangy@nju.edu.cn MOE Key Laboratory for Coast and Island Development School of Geography and Ocean Science Nanjing University Nov., 2013. MOE KLCID. Nanjing University.
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MOE KLCID Nanjing University Estuary flocculation and sediment dynamics in Jiulong River mouth Yang Yang (杨 旸) yangy@nju.edu.cn MOE Key Laboratory for Coast and Island Development School of Geography and Ocean Science Nanjing University Nov., 2013
MOE KLCID Nanjing University Contents • Introduction & Study Area • Data collection and processing • Results • Hydrodynamics • Floc size, settling velocity and turbulence • Summary
Study Area Jiulong River Estuary Jiulong River has a total length of 1,148 km. Annual water discharge is 12×109 m3, with 70% occurring between April to September (wet season) . Max. tidal range ~ 5.6m
MOE KLCID Nanjing University Previous finding Survey line Coarse sediment in the upper layer? Floc? Relative distance (km)
MOE KLCID Nanjing University Floc Survey line Dyer & Manning (1999)
MOE KLCID Nanjing University Winterwerp (1998) Survey line Buonassissi&Dierssen(2010) Wolanski et al.(1992) Floc size ~ Ws SSC Hydro.
Study Area Anchor Station
MOE KLCID Nanjing University Field data collection SBE26 EMCM OBS ADV ADV OBS ADV OBS
MOE KLCID Nanjing University • Tripod Diver
MOE KLCID Nanjing University • CTD • LISST • water samples • ADCP
MOE KLCID Nanjing University OBS SSC calibration ADCP
MOE KLCID Nanjing University ADV SSC calibration ADV
Settling velocity MOE KLCID Nanjing University (1) Rouse-type equation (2) sediment flux method (Fugate & Friedrichs, 2002)
Tides MOE KLCID Nanjing University
Spring Neap MOE KLCID Nanjing University Current velocity and SSC profiles
Spring Neap MOE KLCID Nanjing University Salinity and sus. sed. size profiles
Spring Neap MOE KLCID Nanjing University Current velocity and SSC profiles
Spring Neap MOE KLCID Nanjing University Salinity and sus. sed. size profiles
MOE KLCID Nanjing University
MOE KLCID Nanjing University
Spring Time relative to middle low water level(hour)
Neap Time relative to middle low water level(hour)
MOE KLCID Nanjing University constant shear
MOE KLCID Nanjing University
MOE KLCID Nanjing University suspended sediment size 215 LISST profiles 139 water samples
MOE KLCID Nanjing University
MOE KLCID Nanjing University
MOE KLCID Nanjing University
MOE KLCID Nanjing University
MOE KLCID Nanjing University Summary • Multiple methods provided results with similar general patterns on the shear velocity and settling velocity estimations. • The SPM concentration variation was found to be similar as that of the shear velocity, which is dominated by resuspension within the bottom boundary layer. • The floc size variations are limited by the turbulent eddy evolution during a tidal cycle. The status of turbulent shear determines the aggregates and deflocculating processes, including the settling velocity. • JOURNAL OF GEOPHYSICAL RESEARCH: OCEANS, VOL. 118, 1–18, doi:10.1002/jgrc.20340, 2013
MOE KLCID Nanjing University Thank you!