Modeling nitrogen export from 2539 lowland artificial watersheds in Lake Taihu Basin, China: Insights from process-based modeling

被引:19
作者
Huang, Jiacong [1 ,2 ]
Cui, Zhen [1 ,3 ]
Tian, Feng [1 ,3 ]
Huang, Qi [4 ]
Gao, Junfeng [1 ]
Wang, Xuesong [5 ]
Li, Jun [5 ]
机构
[1] Chinese Acad Sci, Nanjing Inst Geog & Limnol, Key Lab Watershed Geog Sci, 73 East Beijing Rd, Nanjing 210008, Peoples R China
[2] Nanjing Hydraul Res Inst, Ctr Ecoenvironm Res, Nanjing 210098, Peoples R China
[3] Univ Chinese Acad Sci, Beijing 100049, Peoples R China
[4] Jiangxi Normal Univ, Minist Educ, Key Lab Poyang Lake Wetland & Watershed Res, Nanchang 330022, Jiangxi, Peoples R China
[5] Changzhou Hydrol & Water Resources Invest Bur, 1 Xingye Rd, Changshou 213022, Peoples R China
基金
中国国家自然科学基金; 中国博士后科学基金;
关键词
Polder; Global climate change; Nitrogen; Taihu; CLIMATE SYSTEM MODEL; COASTAL WATERS; PHOSPHORUS; PRECIPITATION; CATCHMENTS; NUTRIENTS; CMIP5; EUTROPHICATION; TEMPERATURE; ADAPTATION;
D O I
10.1016/j.jhydrol.2019.124428
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
Excess nitrogen (N) poses a risk of aquatic eutrophication and ecosystem degradation to downstream areas. However, it is poorly investigated in lowland artificial watersheds (polders) due to their complex hydrological processes. This study investigated the N export and retention at all 2539 polders in Lake Taihu Basin, China using a nitrogen dynamic model (NDP), specially developed for polders. The response of N export to global climate change (air temperature and precipitation) and human activities (N fertilization) in the future (2014-2049) were quantified through scenario simulations. The simulation results revealed that these polders have a larger N export coefficient (a spatially-averaged value of 15.3 kg N/ha/yr) than that of non-polder areas (similar to 6.7 kg N/ha/yr) mainly due to their intensive agricultural activities and high population density. However, these polders also showed considerable N retention with estimated retention rates of 52.7-54.6%. In model results from the future (2014-2049), human activities (N fertilization) determined the magnitude of polder N export, while global climate change determined the fluctuation of polder N export. The estimation of polder N sources, sinks and retention capacity at a watershed scale can be used to identify the hotspot of N loss, and thus guide decision-making to control N loss.
引用
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页数:9
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