Patterns of internal nitrogen and phosphorus loadings in a cascade reservoir with a large water level gradient: Effects of reservoir operation and water depth. (15th October 2022)

• Record Type: Journal Article
• Authors: Zhang, Min; Wen, Shuailong; Wu, Tao; Wang, Shaoming; Li, Xin; Gong, Wanqing; Wang, Hongwei; Liu, Cheng; Zhong, Jicheng
• Is Part Of: Journal of environmental management. Volume 320(2022)
• Publication Date: 2022-10-15
• Subjects: Eutrophication -- Internal loading -- N and P fluxes -- Reservoir -- Seasonal thermal stratification; Environmental policy -- Periodicals; Environmental management -- Periodicals; Environment -- Periodicals; Ecology -- Periodicals; 363.705
• DOI: 10.1016/j.jenvman.2022.115884
• Languages: English
• ISSNs: 0301-4797

Abstract

Abstract: Internal nutrient loadings pose a high risk of being an additional N and P source, exacerbating eutrophication and deteriorating water quality. In this study, we selected the Daheiting Reservoir (DHTR) in North China, with a pronounced water level gradient, to investigate internal N and P loadings, estimate N and P fluxes across the sediment‒water interface based on the pore water profiles, and reveal the potential effects of water discharge from an upstream reservoir and high-intensity cage aquaculture on the risks of internal N and P release. The results indicated that DHTR presented with severe internal nutrient loadings, and the N and P fluxes showed significant spatiotemporal variations. N H 4 + − N and soluble reactive phosphorus (SRP) fluxes were higher in deep areas (averages of 26.14 and 9.9 m g m − 2 d − 1, respectively) than in shallow areas near inflows (averages of 5.0 and 1.24 m g m − 2 d − 1, respectively). Unexpectedly, the estimated N H 4 + − N and SRP fluxes were the lowest in summer (averages of 3.94 and 0.33 m g m − 2 d − 1, respectively), which may have been influenced by seasonal thermal stratification and copious discharge from the hypolimnion of the upstream reservoir (Panjiakou Reservoir). Comparison of annual internal and external N and P loadings revealed that water discharge from the upstream Panjiakou Reservoir was the dominant source of N and P to the reservoir, contributing up to 83.6% of N input and 55.4% of P input. The internal P loading also contributed to water eutrophication to a great extent, accounting for 34.7% of the total P input. Our results highlight the impact of upstream reservoir discharge operation on downstream reservoir water quality and the importance of controlling the internal nutrient loading in cascade reservoirs, and further provide theoretical and practical foundations for the development of policies and strategies to conserve reservoir ecosystems. Graphical abstract: Image 1 Highlights: Internal N and P loadings and contributions were evaluated in a cascade reservoir. N and P fluxes showed large spatiotemporal variability. N and P fluxes showed a similar spatial pattern and different temporal pattern. Discharge water from upstream reservoir was the dominant source of N and P. Internal P loading accounted for one-third of the total P loading.