High resolution records of flood deposition in the mud area off the Changjiang River mouth during the past century

• Published in: Chinese journal of oceanology and limnology 2014-07, Vol.32 (4), p.909-920
• Main Authors: Hu, Gang, Li, Anchun, Liu, Jian, Xu, Gang, Mei, Xi, Kong, Xianghuai
• Format: Article
• Language: English
• Subjects: Clay; drainage; Drainage area; Earth and Environmental Science; Earth Sciences; Extreme values; Flood forecasting; Flood frequency; Floods; Fluvial deposits; Frequency analysis; Geochemistry; Geology; Grain size; High resolution; Lead isotopes; Magnetic permeability; Magnetic susceptibility; Marine; Oceanography; Paleoecology; Parameter identification; Parameter sensitivity; Parameters; Particle size; Physical properties; river deltas; River discharge; River mouth; River mouths; Rivers; Seasonal variation; Seasonal variations; Sediment; sediment yield; Sediments; Silt; Water discharge; winter; Zirconium
• ISSN: 0254-4059; 2096-5508; 1993-5005; 2523-3521
• DOI: 10.1007/s00343-014-3244-x

This paper presents a paleoflood study to determine the flood frequency of the Changjiang River, based on core cj0702, taken from the Changjiang River subaqueous delta. We identified flood deposits by means of high-resolution grain-size variation, sensitive population, geochemical indexes and magnetic susceptibility. The core covers a time span of 120 years by ²¹⁰Pb dating and was sampled at 1–2 cm intervals. Grain size, geochemical elements, and physical parameters were analyzed. The results indicate that the sediment of the core is mainly composed of silt and clay, as well as groups of interbedded silt, clay silt, and clay. Vertically, the grain size pattern was controlled by seasonal variations in water discharge and by the sediment input in winter from the abandoned Huanghe River delta. River flooding caused extreme values in all our measured parameters. We identified more than 20 flood events that occurred since 1887 using the physical parameter analysis method. The environmentally sensitive component of sediment grain size (14.32–96.39 μm) contribution>30%, Zr/Rb ratio>1.5, and magnetic susceptibility>16 were selected as the criteria for flood identification generally. We also found that floods that had taken place in the upstream, midstream, or downstream parts of the river were clearly identified by these indexes while the large-scale floods that covered the whole drainage area did not leave clear indications in the sediment record. This study for identification of flood events is of great significance for understanding hyperpycnal current sedimentation as well as for forecasting of floods.