Spatiotemporal variations and dominated environmental parameters of nitrous oxide (N2O) concentrations from cascade reservoirs in southwest China

Chiquan He; Rui Qi; Haiyue Feng; Zhenzhen Zhao; Fushun Wang; Daoyuan Wang; Feifei Wang; Xueping Chen; Pu Zhang; Siliang Li; Yuanbi Yi

doi:10.1007/s11356-023-29502-9

Spatiotemporal variations and dominated environmental parameters of nitrous oxide (N₂O) concentrations from cascade reservoirs in southwest China

Environ Sci Pollut Res Int. 2023 Oct;30(46):102547-102559. doi: 10.1007/s11356-023-29502-9. Epub 2023 Sep 5.

Authors

Chiquan He¹, Rui Qi¹, Haiyue Feng¹, Zhenzhen Zhao², Fushun Wang¹, Daoyuan Wang¹, Feifei Wang¹, Xueping Chen¹, Pu Zhang¹, Siliang Li³, Yuanbi Yi³

Affiliations

¹ School of Environmental and Chemical Engineering, Shanghai University, 150#, 99 Shangda Road, Shanghai, 200444, China.
² School of Environmental and Chemical Engineering, Shanghai University, 150#, 99 Shangda Road, Shanghai, 200444, China. zhaozhen0828@126.com.
³ Institute of Surface-Earth System Science, Tianjin University, Tianjin, 300072, China.

PMID: 37668782
DOI: 10.1007/s11356-023-29502-9

Abstract

Anthropogenic activity has caused rivers and reservoirs to become sources of nitrous oxide (N₂O), which is thought to play an important role in global climate change. There are thermal and DO stratification in deep-water reservoirs with long hydraulic retention time, which change N₂O production mechanism compared with shallow-water reservoirs. To promote our understanding of the relationship of N₂O production in reservoirs at different depths, spatiotemporal variations in water environmental factors and N₂O from cascade reservoirs of Chaishitan (CST), Longtan (LT), Yantan (YT) and Dahua (DH) reservoirs in the Zhujiang River were detected, and the LT and YT reservoirs were compared as representatives of deep-water and shallow-water reservoirs in April and July 2019. The average N₂O concentrations in the LT and YT reservoirs were 22.82 ± 2.21 and 21.55 ± 1.65 nmol L^-1, respectively. During spring and summer, the WT (water temperature) and DO (dissolved oxygen) concentrations in the YT reservoir were well mixed. In contrast, the LT reservoir, as a deep-water reservoir, had thermal and DO stratifications in both the shallow and middle water, especially in the summer when the solar radiation intensity was high. During summer stratification, the DO concentration in the LT reservoir showed obvious spatial variation, ranging from 1.23 to 9.84 mg L^-1, while the DO concentration in the YT reservoir showed very little variation, ranging from 6.45 to 7.09 mg L^-1. Structural equation modeling results showed that NH₄⁺ was the main determinant of the N₂O concentration in the YT reservoir, and DO was the most influential factor of the N₂O concentration in the LT reservoir. These results suggest significant variations in the factors influencing N₂O concentration among reservoirs. Additionally, the mechanisms of N₂O production differ between deep-water and shallow-water reservoirs. This study highlights the spatio-temporal variations and influential factors contributing to N₂O concentration. Furthermore, it discusses the production mechanisms of N₂O in different types of reservoirs. These findings contribute to our understanding of N₂O distribution in hydropower systems and provide valuable data for the management of hydropower facilities and research on greenhouse gas emissions.

Keywords: Deep-water reservoir; Denitrification; Nitrification; Nitrous oxide (N2O); Reservoirs; Shallow-water reservoir.

Abstract

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