Patterns and Drivers of CO2 and CH4 Fluxes in an Urbanized River Network and Their Response to Restoration

IF 3.7 3区 环境科学与生态学 Q2 ENVIRONMENTAL SCIENCES
Lingling Li, Renhua Yan
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Abstract

Carbon evasion from urban river networks becomes increasingly significant as urbanization accelerates. However, there remains a limited understanding of the overall carbon emission impact integrating CO2 and CH4 dynamics, particularly in response to ecological restoration efforts. In this study, we investigated patterns of fluvial CO2 and CH4 diffusive fluxes across an urban river network in Wuxi, China. Our results reveal that water quality variables, especially dissolved oxygen (DO) and phosphorus content, predominantly influence the variability of carbon emissions. These factors exhibit a stronger correlation with CO2 emissions compared to CH4, indicating a net increase in carbon emissions as water quality deteriorates. Seasonally, higher water temperatures, phosphate levels, and lower DO concentrations lead to increased carbon emissions during summer months. Spatially, areas with lower carbon emissions (averaged 86 mmol m−2 d−1 CO2 and 0.13 mmol m−2 d−1 CH4) are primarily situated near the lake and in river sections where significant water quality improvements have been achieved through ecological restoration efforts. Cluster analysis shows that over 60% of high-carbon emission (averaged 162 mmol m−2 d−1 CO2 and 1.21 mmol m−2 d−1 CH4) sites in the study area have undergone ecological restoration, suggesting potential for further carbon emission reduction through enhanced restoration practices. Our findings underscore the importance of implementing carbon reduction strategies such as nutrient removal and aeration for oxygenation within water ecological restoration initiatives. Effective matching of restoration strategies holds further potential for mitigating carbon emissions from urban river networks.

城市化河网中二氧化碳和甲烷通量的模式和驱动因素及其对恢复的响应
随着城市化进程的加快,城市河网的碳逃逸变得越来越重要。然而,人们对二氧化碳和甲烷动态综合碳排放影响的了解仍然有限,尤其是在生态恢复工作中。在这项研究中,我们调查了中国无锡城市河网中流体二氧化碳和甲烷扩散通量的模式。研究结果表明,水质变量,尤其是溶解氧(DO)和磷含量,主要影响碳排放的变化。与甲烷(CH4)相比,这些因素与二氧化碳排放量的相关性更大,表明随着水质恶化,碳排放量会出现净增长。从季节上看,较高的水温、磷酸盐含量和较低的溶解氧浓度会导致夏季碳排放量增加。从空间上看,碳排放量较低的区域(平均为 86 mmol m-2 d-1 CO2 和 0.13 mmol m-2 d-1 CH4)主要位于湖泊附近以及通过生态修复工作显著改善水质的河段。聚类分析显示,研究区域内超过 60% 的高碳排放(平均为 162 mmol m-2 d-1 CO2 和 1.21 mmol m-2 d-1 CH4)地点进行了生态修复,这表明通过加强修复实践有可能进一步减少碳排放。我们的研究结果强调了在水生态修复措施中实施碳减排策略(如去除营养物质和通气增氧)的重要性。修复策略的有效匹配为减少城市河网的碳排放带来了更多潜力。
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来源期刊
Journal of Geophysical Research: Biogeosciences
Journal of Geophysical Research: Biogeosciences Earth and Planetary Sciences-Paleontology
CiteScore
6.60
自引率
5.40%
发文量
242
期刊介绍: JGR-Biogeosciences focuses on biogeosciences of the Earth system in the past, present, and future and the extension of this research to planetary studies. The emerging field of biogeosciences spans the intellectual interface between biology and the geosciences and attempts to understand the functions of the Earth system across multiple spatial and temporal scales. Studies in biogeosciences may use multiple lines of evidence drawn from diverse fields to gain a holistic understanding of terrestrial, freshwater, and marine ecosystems and extreme environments. Specific topics within the scope of the section include process-based theoretical, experimental, and field studies of biogeochemistry, biogeophysics, atmosphere-, land-, and ocean-ecosystem interactions, biomineralization, life in extreme environments, astrobiology, microbial processes, geomicrobiology, and evolutionary geobiology
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