Spatio-temporal patterns and drivers of CH4 and CO2 fluxes from rivers and lakes in highly urbanized areas

被引:5
|
作者
Fan, Longfeng [1 ,2 ]
Cheng, Junxiang [1 ,3 ,10 ]
Xie, Yangcun [4 ]
Xu, Ligang [1 ,5 ]
Buttler, Alexandre [6 ,7 ]
Wu, Yuexia [8 ]
Fan, Hongxiang [1 ]
Wu, Yakun [1 ,9 ]
机构
[1] Chinese Acad Sci, Key Lab Watershed Geog Sci, Nanjing Inst Geog & Limnol, Nanjing 210008, Peoples R China
[2] Univ Chinese Acad Sci, Beijing 100049, Peoples R China
[3] Jiangxi Res Acad Ecol Civilizat, Nanchang 330036, Peoples R China
[4] Chinese Acad Environm Planning, Beijing 100043, Peoples R China
[5] Univ Chinese Acad Sci Nanjing, Nanjing 211135, Peoples R China
[6] Ecole Polytech Fed Lausanne EPFL, Sch Architecture Civil & Environm Engn ENAC, Stn 2, CH-1015 Lausanne, Switzerland
[7] Swiss Fed Inst Forest Snow & Landscape Res WSL, Site Lausanne,Stn 2, CH-1015 Lausanne, Switzerland
[8] Nanjing Univ Finance & Econ, Sch Business Adm, Nanjing 210023, Peoples R China
[9] Anhui Univ Technol, Sch Energy & Environm, Maanshan 243002, Peoples R China
[10] Chinese Acad Sci, Nanjing Inst Geog & Limnol, Nanjing 210008, Peoples R China
关键词
Carbon cycle; Carbon dioxide; Controlling factor; Gas exchange; Methane; Urban landscape; GREENHOUSE GASES CO2; NITROUS-OXIDE EMISSIONS; CARBON-DIOXIDE; REGIONAL-SCALE; WATER-QUALITY; METHANE; DYNAMICS; N2O; NETWORK; SUPERSATURATION;
D O I
10.1016/j.scitotenv.2024.170689
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Gaseous carbon exchange at the water-air interface of rivers and lakes is an essential process for regional and global carbon cycle assessments. Many studies have shown that rivers surrounding urban landscapes can be hotspots for greenhouse gas (GHG) emissions. Here we investigated the variability of diffusive GHG (methane [CH4] and carbon dioxide [CO2]) emissions from rivers in different landscapes (i.e., urban, agricultural and mixed) and from lakes in Suzhou, a highly urbanized region in eastern China. GHG emissions in the Suzhou metropolitan water network followed a typical seasonal pattern, with the highest fluxes in summer, and were primarily influenced by temperature and dissolved oxygen concentration. Surprisingly, lakes were emission hotspots, with mean CH4 and CO2 fluxes of 2.80 and 128.89 mg m- 2 h-1, respectively, translating to a total CO2- equivalent flux of 0.21 g CO2-eq m- 2 d-1. The global warming potential of urban and mixed rivers (0.19 g CO2- eq m- 2 d-1) was comparable to that for lakes, but about twice the value for agricultural rivers (0.10 g CO2-eq m- 2 d-1). Factors related to the high GHG emissions in lakes included hypoxic water conditions and an adequate nutrient supply. Riverine CH4 emissions were primarily associated with the concentrations of total dissolved solids (TDS), ammonia-nitrogen and chlorophyll a. CO2 emissions in rivers were mainly closely related to TDS, with suitable conditions allowing rapid organic matter decomposition. Compared with other types of rivers, urban rivers had more available organic matter and therefore higher CO2 emissions. Overall, this study em- phasizes the need for a deeper understanding of the impact of GHG emissions from different water types on global warming in rapidly urbanizing regions. Flexible management measures are urgently needed to mitigate CO2 and CH4 emissions more effectively in the context of the shrinking gap between urban and rural areas with growing socio-economic development.
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页数:12
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