Effects of Seasonal Thermal Stratification on Nitrogen Transformation and Diffusion at the Sediment-Water Interface in a Deep Canyon Artificial Reservoir of Wujiang River Basin

Watershed-scale nitrogen pollution in aquatic systems has become a worldwide concern due to its continuous impact on water quality deterioration, while the knowledge of key influencing factors dominating nitrogen transportation and transformation at the sediment-water interface (SWI) remains limited...

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Autores principales: Yongmei Hou, Xiaolong Liu, Sainan Chen, Jie Ren, Li Bai, Jun Li, Yongbo Gu, Lai Wei
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Publicado: MDPI AG 2021
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spelling oai:doaj.org-article:5ffad47f45f949a8b75d4aaabcd6d0f42021-11-25T19:15:23ZEffects of Seasonal Thermal Stratification on Nitrogen Transformation and Diffusion at the Sediment-Water Interface in a Deep Canyon Artificial Reservoir of Wujiang River Basin10.3390/w132231942073-4441https://doaj.org/article/5ffad47f45f949a8b75d4aaabcd6d0f42021-11-01T00:00:00Zhttps://www.mdpi.com/2073-4441/13/22/3194https://doaj.org/toc/2073-4441Watershed-scale nitrogen pollution in aquatic systems has become a worldwide concern due to its continuous impact on water quality deterioration, while the knowledge of key influencing factors dominating nitrogen transportation and transformation at the sediment-water interface (SWI) remains limited, especially in impounded rivers with an artificial reservoir. Hence, for a better understanding of the effects of thermal stratification on nitrogen transformation, we investigated the nitrogen species and isotopes in the sediment of a deep reservoir in Southwest China. Our results confirmed a significant difference in nitrogen species and isotopic composition in sediment between those in the thermal stratification period and non-thermal stratification period and indicated that the sediment biogeochemical process and transportation were clearly linked to the variations in water temperature and dissolved oxygen dominated by the process of thermal stratification. Significant seasonal differences in NH<sub>4</sub><sup>+</sup>-N and NO<sub>3</sub><sup>−</sup>-N in pore water of the upper layer (0–19 cm) revealed that nitrification exhausted NH<sub>4</sub><sup>+</sup> in the non-stratified period (NSP), and a potential low mineralization rate appeared when compared with those in the stratified period (SP). Seasonal differences in nitrogen species and isotope fractionation of δ<sup>15</sup>N-PON (about 2.3‰ in SP) in the upper layer sediment indicated a higher anaerobic mineralization rate of organic matter in SP than that in NSP. The diffusion fluxes of NH<sub>4</sub><sup>+</sup>-N at SWI were 9.48 and 15.66 mg·m<sup>−2</sup>·d<sup>−1</sup> in NSP and SP, respectively, and annual NH<sub>4</sub><sup>+</sup>-N diffusion accounted for 21.8% of total storage in the reservoir. This study demonstrated that the nitrogen cycling processes, especially nitrification, denitrification, and mineralization, have been largely altered along with the changes in dissolved oxygen and that the diffusion of nitrogen species varied with the presence of the oxygen. The results contribute to the future study of watershed nitrogen budget evaluation and suggest that the endogenous nitrogen released from the sediment-water interface should be emphasized when aiming to fulfil water management policies in deep reservoirs.Yongmei HouXiaolong LiuSainan ChenJie RenLi BaiJun LiYongbo GuLai WeiMDPI AGarticlethermal stratificationnitrogen transformationsediment-water interfacereservoirNH<sub>4</sub><sup>+</sup> diffusionHydraulic engineeringTC1-978Water supply for domestic and industrial purposesTD201-500ENWater, Vol 13, Iss 3194, p 3194 (2021)
institution DOAJ
collection DOAJ
language EN
topic thermal stratification
nitrogen transformation
sediment-water interface
reservoir
NH<sub>4</sub><sup>+</sup> diffusion
Hydraulic engineering
TC1-978
Water supply for domestic and industrial purposes
TD201-500
spellingShingle thermal stratification
nitrogen transformation
sediment-water interface
reservoir
NH<sub>4</sub><sup>+</sup> diffusion
Hydraulic engineering
TC1-978
Water supply for domestic and industrial purposes
TD201-500
Yongmei Hou
Xiaolong Liu
Sainan Chen
Jie Ren
Li Bai
Jun Li
Yongbo Gu
Lai Wei
Effects of Seasonal Thermal Stratification on Nitrogen Transformation and Diffusion at the Sediment-Water Interface in a Deep Canyon Artificial Reservoir of Wujiang River Basin
description Watershed-scale nitrogen pollution in aquatic systems has become a worldwide concern due to its continuous impact on water quality deterioration, while the knowledge of key influencing factors dominating nitrogen transportation and transformation at the sediment-water interface (SWI) remains limited, especially in impounded rivers with an artificial reservoir. Hence, for a better understanding of the effects of thermal stratification on nitrogen transformation, we investigated the nitrogen species and isotopes in the sediment of a deep reservoir in Southwest China. Our results confirmed a significant difference in nitrogen species and isotopic composition in sediment between those in the thermal stratification period and non-thermal stratification period and indicated that the sediment biogeochemical process and transportation were clearly linked to the variations in water temperature and dissolved oxygen dominated by the process of thermal stratification. Significant seasonal differences in NH<sub>4</sub><sup>+</sup>-N and NO<sub>3</sub><sup>−</sup>-N in pore water of the upper layer (0–19 cm) revealed that nitrification exhausted NH<sub>4</sub><sup>+</sup> in the non-stratified period (NSP), and a potential low mineralization rate appeared when compared with those in the stratified period (SP). Seasonal differences in nitrogen species and isotope fractionation of δ<sup>15</sup>N-PON (about 2.3‰ in SP) in the upper layer sediment indicated a higher anaerobic mineralization rate of organic matter in SP than that in NSP. The diffusion fluxes of NH<sub>4</sub><sup>+</sup>-N at SWI were 9.48 and 15.66 mg·m<sup>−2</sup>·d<sup>−1</sup> in NSP and SP, respectively, and annual NH<sub>4</sub><sup>+</sup>-N diffusion accounted for 21.8% of total storage in the reservoir. This study demonstrated that the nitrogen cycling processes, especially nitrification, denitrification, and mineralization, have been largely altered along with the changes in dissolved oxygen and that the diffusion of nitrogen species varied with the presence of the oxygen. The results contribute to the future study of watershed nitrogen budget evaluation and suggest that the endogenous nitrogen released from the sediment-water interface should be emphasized when aiming to fulfil water management policies in deep reservoirs.
format article
author Yongmei Hou
Xiaolong Liu
Sainan Chen
Jie Ren
Li Bai
Jun Li
Yongbo Gu
Lai Wei
author_facet Yongmei Hou
Xiaolong Liu
Sainan Chen
Jie Ren
Li Bai
Jun Li
Yongbo Gu
Lai Wei
author_sort Yongmei Hou
title Effects of Seasonal Thermal Stratification on Nitrogen Transformation and Diffusion at the Sediment-Water Interface in a Deep Canyon Artificial Reservoir of Wujiang River Basin
title_short Effects of Seasonal Thermal Stratification on Nitrogen Transformation and Diffusion at the Sediment-Water Interface in a Deep Canyon Artificial Reservoir of Wujiang River Basin
title_full Effects of Seasonal Thermal Stratification on Nitrogen Transformation and Diffusion at the Sediment-Water Interface in a Deep Canyon Artificial Reservoir of Wujiang River Basin
title_fullStr Effects of Seasonal Thermal Stratification on Nitrogen Transformation and Diffusion at the Sediment-Water Interface in a Deep Canyon Artificial Reservoir of Wujiang River Basin
title_full_unstemmed Effects of Seasonal Thermal Stratification on Nitrogen Transformation and Diffusion at the Sediment-Water Interface in a Deep Canyon Artificial Reservoir of Wujiang River Basin
title_sort effects of seasonal thermal stratification on nitrogen transformation and diffusion at the sediment-water interface in a deep canyon artificial reservoir of wujiang river basin
publisher MDPI AG
publishDate 2021
url https://doaj.org/article/5ffad47f45f949a8b75d4aaabcd6d0f4
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