Space-for-time substitution leads to carbon emission overestimation in eutrophic lakes

被引:14
|
作者
Zhou, Muchun [1 ,3 ]
Zhou, Chuanqiao [1 ,2 ]
Peng, Yu [1 ]
Jia, Ruoyu [1 ]
Zhao, Wenpeng [4 ]
Liang, Shuoyuan [2 ]
Xu, Xiaoguang [1 ,5 ]
Terada, Akihiko [3 ]
Wang, Guoxiang [1 ]
机构
[1] Nanjing Normal Univ, Jiangsu Ctr Collaborat Innovat Geog Informat Resou, Sch Environm, Jiangsu Key Lab Environm Change & Ecol Constructio, Nanjing 210023, Peoples R China
[2] Tokyo Inst Technol, Dept Transdisciplinary Sci & Engn, Tokyo 1528550, Japan
[3] Tokyo Univ Agr & Technol, Dept Chem Engn, Tokyo 1848588, Japan
[4] Natl Univ Singapore, Dept Civil & Environm Engn, Singapore City 119077, Singapore
[5] Xianlin Univ, 1 Wenyuan Rd, Nanjing 210023, Peoples R China
基金
中国国家自然科学基金;
关键词
Eutrophication; Cyanobacteria; Greenhouse gas; Space-for-time substitution; Emission potential; CYANOBACTERIA BLOOMS; METHANE DYNAMICS; WATER; RESERVOIRS; CH4; PHOSPHORUS; COMMUNITY;
D O I
10.1016/j.envres.2022.115175
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Lacustrine eutrophication is generally considered as an important contributor of carbon emissions to the at-mosphere; however, there is still a huge challenge in accuracy estimating carbon emissions from lakes. To test the effect of widely used space-for-time substitution on lake carbon emissions, this study monitored different pro-cesses of carbon emissions, including the carbon production potential, dissolved carbon concentrations, and carbon release fluxes in eight lakes along the trophic gradients on a spatial scale and the typical eutrophic Lake Taihu for one year on a temporal scale. Eutrophication promoted carbon production potential, dissolved carbon concentrations, and carbon release fluxes, especially for CH4. Trophic lake index (TLI) showed positive corre-lations with the CH4 production potential, dissolved CH4 concentrations, and CH4 release fluxes, and also pos-itive correlations with the CO2 production potential, dissolved CO2 concentrations, and CO2 release fluxes. The space-for-time substitution led to an overestimation for the influence of eutrophication on carbon emissions, especially the further intensification of lake eutrophication. On the spatial scale, the average CH4 production potential, dissolved CH4 concentrations and CH4 release fluxes in eutrophic lakes were 268.6, 0.96 mu mol/L, and 587.6 mu mol m - 2 center dot h- 1,respectively, while they were 215.8, 0.79 mu mol/L, and 548.6 mu mol m - 2 center dot h- 1on the temporal scale. Obviously, CH4 and CO2 emissions on the spatial scale were significantly higher than those on the temporal scale in eutrophic lakes. The primary influencing factors were the seasonal changes in the physicochemical environments of lake water, including dissolved oxygen (DO) and temperature. The CH4 and CO2 release fluxes showed negative correlations with DO, while temperature displayed positive correlations, respectively. These results suggest that the effects of DO and temperature on lake carbon emissions should be considered, which may be ignored during the accurate assessment of lake carbon budget via space-for-time substitution in eutrophic lakes.
引用
收藏
页数:11
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