Assessing the Impacts of Reservoirs on Riverine Dissolved Organic Matter: Insights From the Largest Reservoir in the Pearl River

Author:

Yi Yuanbi123ORCID,Li Si‐Liang1ORCID,Zhong Jun1ORCID,Wang Kai4,Merder Julian5ORCID,Bao Hongyan6ORCID,Qi Yulin1ORCID,He Ding27ORCID,Xu Sheng1ORCID,Dittmar Thorsten38ORCID,Liu Cong‐Qiang19

Affiliation:

1. Institute of Surface‐Earth System Science School of Earth System Science Tianjin University Tianjin China

2. Department of Ocean Science and Center for Ocean Research in Hong Kong and Macau The Hong Kong University of Science and Technology Hong Kong China

3. ICBM‐MPI Bridging Group for Marine Geochemistry Institute for Chemistry and Biology of the Marine Environment Carl von Ossietzky University Oldenburg Germany

4. Department of Ocean Science and Engineering Southern University of Science and Technology Shenzhen China

5. Department of Global Ecology Carnegie Institution for Science Stanford CA USA

6. State Key Laboratory of Marine Environmental Science College of Ocean and Earth Sciences Xiamen University Xiamen China

7. State Key Laboratory of Marine Pollution City University of Hong Kong Hong Kong China

8. Helmholtz Institute for Functional Marine Biodiversity Carl von Ossietzky University Oldenburg Germany

9. Haihe Laboratory of Sustainable Chemical Transformations Tianjin China

Abstract

AbstractExtensive reservoir construction has fragmented more than 70% of the world's rivers, significantly impacting river connectivity and carbon cycling. However, the response of riverine dissolved organic matter (DOM) to reservoir influence and its potential downstream effects remains unclear. In this study, we employed multiple analytical techniques, including Fourier transform ion cyclotron resonance mass spectrometry, radiocarbon dating, and environmental factor analysis, to investigate the dynamic changes in DOM and its controlling factors under different hydrological management regimes in the LongTan Reservoir, the largest reservoir in the Pearl River, which is the second largest river in China by water discharge. Our results indicate that the molecular diversity of riverine DOM is reduced in the reservoir. Oxygen‐rich and heteroatomic compounds, such as those containing nitrogen, sulfur, and phosphorus, are preferentially removed through enhanced photo‐ and biodegradation processes in the reservoir, particularly during the storage period. This leads to DOM that is enriched with oxygen‐poor compounds and shows a biodegraded Δ14C value downstream. This study highlights that the composition of riverine DOM is significantly altered by the reservoir, but these effects could potentially be mitigated by optimizing the outlet location.

Funder

National Natural Science Foundation of China

Publisher

American Geophysical Union (AGU)

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