Sediment resuspension in the Lake Taihu, China  

作　　者：HU Chunhua HU Weiping ZHANG Fabing HU Zhixin LI Xianghua CHEN Yonggen 

机构地区：[1]Nanjing Institute of Geography and Linmology, Chinese Academy ofSciences, Nanjing 210008, China [2]Graduate School of the Chinese Academy of Sciences, Beijing 100049,China [3]Hehai University, Naniing 210008 China

出　　处：《Chinese Science Bulletin》2006年第6期731-737,共7页

摘　　要：In order to examine the intensity of surfi-cial sediment resuspension in Lake Taihu, a large shallow lake in eastern China, suspended sediment concentrations (SSCs) were measured on the basis of analysis of water samples collected using an in-novative multi-level water sampler. The results show that under calm weather conditions, the SSC is rela-tively homogenous through the entire water column. However, when strong winds occur, the SSC in the bottom layer is 1-2 orders of magnitude greater than in the surface layer; thus, in this case, the amount of total suspended matter in the water column cannot be estimated using the SSC values of the surface layer alone. Furthermore, the depth of disturbance, or the thickness of the sediment layer that is set in mo-tion by wind-wave induced currents, is of the order of 100 mm.In order to examine the intensity of surficial sediment resuspension in Lake Taihu, a large shallow lake in eastern China, suspended sediment concentrations （SSCs） were measured on the basis of analysis of water samples collected using an innovative multi-level water sampler. The results show that under calm weather conditions, the SSC is relatively homogenous through the entire water column. However, when strong winds occur, the SSC in the bottom layer is 1-2 orders of magnitude greater than in the surface layer; thus, in this case, the amount of total suspended matter in the water column cannot be estimated using the SSC values of the surface layer alone. Furthermore, the depth of disturbance, or the thickness of the sediment layer that is set in motion by wind-wave induced currents, is of the order of 10^0 mm.

关 键 词：中国 太湖 沉淀物 再悬浮作用 沉积物迁移 

分 类 号：P512.32[天文地球—地质学]