Investigation of the impact of hydrodynamic conditions on sediment resuspension in shallow lakes  

作　　者：Wenguang Luo Jing Lu Senlin Zhu Yao Yue Lingjun Xiao 

机构地区：[1]State Key Laboratory of Water Resources and Hydropower Engineering Science,Wuhan University,Wuhan,People’s Republic of China [2]College of Hydraulic Science and Engineering,Yangzhou University,Yangzhou,People’s Republic of China [3]Wuhan Yuchi Testing Technology Co.,Ltd,Wuhan,People’s Republic of China

出　　处：《International Journal of Digital Earth》2022年第1期1676-1691,共16页国际数字地球学报（英文）

基　　金：supported by the National Natural Science Foundation of China [grant numbers 52109099,52079094].

摘　　要：In this study,we sampled the original sediment columns from three points located in the eastern,central,and western areas of Chaohu Lake,and then investigated sediment resuspension under hydraulic disturbances in the laboratory. The results showed that when the hydraulic disturbance is weak and sediment surface shear stress is small (<0.02 N/m²),sediment surface layer moves alone. When the hydraulic disturbance is moderate and sediment surface shear stress is within a threshold (3.7 N/m²),only a small proportion of the surface sediments begins to move. However,when the hydraulic disturbance is further strengthened and sediment surface shear stress is larger than the threshold value,surface sediments move smoothly. By the experimental results,we found that the plankton layer is about 1 mm (1.56% of the maximum content of suspended matter (SSCmax)),which is the major contribution of individual sediment initiation. The new sediment layer is about 19–22 mm (20.9% of the SSCmax),which considerably affects sediment resuspension in shallow lakes. The consolidated layer is about 22 mm below the bed surface,which requires high shear stress and is hard to be transferred to the water column. The quantified experimental observation results are further verified with the theoretical results.

关 键 词：Sediment resuspension suspended solids shear stress HYDRODYNAMIC Lake Chaohu 

分 类 号：TV142[水利工程—水力学及河流动力学]