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Updated: May 31, 2026

Measuring Dissolved Methane in Aquatic Ecosystems Using An Optical Spectroscopy Gas Analyzer
Published on: July 26, 2024
Contrasting greenhouse gas fluxes in a city river-lake continuum: CH4 diffusive emissions offset by N2O sequestration
Xiaokang Tian1, Menglin Liu1, Y Jun Xu2
1School of Environmental Ecology and Biological Engineering, Hubei Key Laboratory of Microbial Transformation and Regulation of Biogenic Elements in the Middle Reaches of the Yangtze River, State Key Laboratory of Green and Efficient Development of Phosphorus Resources, Wuhan Institute of Technology, Wuhan, 430205, China.
Abstract:
Urban aquatic systems are critical yet poorly constrained contributors to global greenhouse gas (GHG) budgets. This is particularly true for semi-natural river-lake continuum undergoing rapid urbanization. This study investigated the spatiotemporal variations and influencing factors of methane (CH4) and nitrous oxide (N2O) diffusive fluxes across water-atmosphere boundary in an urban river-lake system of China. Dissolved CH4 and N2O were collected using a headspace equilibrium method, and the patterns and governing factors of these gases were then unraveled through partial least squares path modeling. We found significant spatiotemporal heterogeneity in CH4 and N2O fluxes. CH4 fluxes were 3.2-fold higher in the river Qingshangang (QSG) (32.81 ± 34.84 μmol m-2 d-1) than in the river Lihu (LH) (10.15 ± 8.15 μmol m-2 d-1), while N2O fluxes demonstrated a clear source-sink transition, with QSG acting as a net source (3.23 ± 4.14 μmol m-2 d-1), and LH as a net sink (-2.66 ± 1.99 μmol m-2 d-1). CH4 flux was significantly higher in the rainy season (QSG: 42.34 ± 37.61 μmol m-2 d-1; LH: 17.39 ± 8.48 μmol m-2 d-1) than in the dry season (QSG: 21.28 ± 55.93 μmol m-2 d-1; LH: 2.47 ± 1.39 μmol m-2 d-1). N2O flux was also higher in the rainy season (4.22 ± 4.70 μmol m-2 d-1) than in the dry season (2.23 ± 3.57 μmol m-2 d-1) in QSG, in contrast, an opposite pattern occurred in LH, where rainy season flux (-4.09 ± 2.86 μmol m-2 d-1) was significantly more negative than dry season flux (-1.24 ± 0.52 μmol m-2 d-1). CH4 flux was mainly regulated by nutrient species, whereas N2O flux was more strongly influenced by basic water quality parameters. Aquatic vegetation significantly reduced CH4 emissions, however, had negligible effects on N2O flux. The study shows an overall net carbon sink for the studied urban landscape lake over a 100-year global warming potential timeframe. These findings underscore the importance of high-resolution, site-specific assessments for accurate GHG accounting and effective mitigation strategy.
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