引江济太不是太湖磷负荷上升的原因  

Water Diversion is Not to Blame for Phosphorus Enrichment in Taihu Lake

作　　者：Zhiyuan Wang Qiuwen Chen Jianyun Zhang Hanlu Yan 

机构地区：[1]State Key Laboratory of Hydrology–Water Resources and Hydraulic Engineering,Nanjing Hydraulic Research Institute,Nanjing 210098,China [2]Center for Eco-Environment Research,Nanjing Hydraulic Research Institute,Nanjing 210098,China [3]Yangtze Institute for Conservation and Green Development,Hohai University,Nanjing 210098,China

出　　处：《Engineering》2024年第4期10-14,共5页工程（英文）

基　　金：funded by the National Natural Science Foundation of China(52121006,52070132,and U2040209);the Outstanding Youth Fund of Jiangsu Province(BK20200053).

摘　　要：Despite frequent cyanobacterial blooms increasing in magnitude and duration,Taihu Lake remains one of the most important water sources in the Yangtze River Delta of China.To meet the rising water demand from social–economic development and secure water source during cyanobacterial blooms,the Water Diversion Project from the Yangtze River to Taihu Lake(WDYT)through the Wangyuhe(WYH)River channel was initiated in 2002 and has been in operation since 2007.

关 键 词：YANGTZE China initiated 

分 类 号：X524[环境科学与工程—环境工程] TV67[水利工程—水利水电工程]