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Widespread dissolved oxygen supersaturation in Chinese warming lakes.
Dianwei Zhang1, Wenqiang Zhang2, Weidong Wang2
1Laboratory of Environmental Biotechnology, Research Center for Eco-Environmental Sciences, Research Center· for Eco-Environmental Sciences, Chinese Academy of Sciences, P. O. Box·2871, Beijing, 100085, PR China; University of Chinese Academy of Sciences, Beijing, 100049, PR China.
Dissolved oxygen supersaturation is common in lakes, peaking in summer with daily fluctuations. Temperature and algal biomass drive this phenomenon, which can mask deeper water hypoxia.
Area of Science:
- Aquatic ecology
- Limnology
- Environmental science
Background:
- Dissolved oxygen (DO) supersaturation, once rare, is now a widespread lake phenomenon.
- Long-term data reveal average DO saturation exceeding 100%, with frequent supersaturation events.
Purpose of the Study:
- To analyze the drivers and patterns of DO supersaturation in lakes.
- To understand the ecological implications of DO supersaturation for lake ecosystems.
Main Methods:
- Analysis of long-term time series data.
- Application of non-parametric statistical tests and Generalized Additive Mixed Models (GAMM).
Main Results:
- DO supersaturation occurs mainly from June to September, with a distinct diurnal "roller-coaster" pattern.
- Temperature has a dual effect: decreasing solubility but increasing photosynthesis-driven DO production.
- pH and algal biomass are key factors promoting DO supersaturation.
Conclusions:
- DO supersaturation is a complex phenomenon with significant seasonal and diurnal oscillations.
- Surface supersaturation can mask underlying hypoxia in deeper water layers.
- Findings support science-based lake management and conservation strategies.
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