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Detecting the leakage source of a reservoir using isotopes
Peng Yi1, Jing Yang1, Yongdong Wang2
1State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, Hohai University, Nanjing 210098, China; College of Hydrology and Water Resources, Hohai University, Nanjing 210098, China.
Identifying water reservoir leakage sources is crucial for dam safety. This study used multiple tracers like radon and isotopes to pinpoint leakage origins at the Pushihe pumped storage power station, confirming reservoir water as the primary source.
Area of Science:
- Environmental Science
- Hydrogeology
- Geochemistry
Background:
- Effective monitoring of water reservoir leakage is essential for understanding origins and implementing restoration.
- Leakage in water infrastructure can compromise structural integrity and lead to significant water loss.
Purpose of the Study:
- To identify the sources of water leakage in the Pushihe pumped storage power station.
- To evaluate the effectiveness of a multi-tracer approach for leakage source identification.
Main Methods:
- Utilized a combination of tracers: radon-222 (Rn), oxygen and hydrogen isotopes, anions (nitrate, sulfate, chloride), and temperature.
- Analyzed water samples from leakage points, the reservoir, and surrounding groundwater.
- Interpreted tracer data to differentiate water sources.
Main Results:
- Radon-222 activity levels suggested reservoir water as the primary leakage source.
- Oxygen and hydrogen isotope analysis indicated comparable values between reservoir and leakage water.
- Groundwater contributed up to 36% in specific locations, while reservoir water was dominant elsewhere.
- Anion analysis corroborated reservoir water as the main source of leakage.
Conclusions:
- A multi-tracer approach significantly improves the accuracy of identifying water reservoir leakage sources.
- Reservoir water is the dominant source of leakage in the Pushihe pumped storage power station.
- Findings provide a scientific basis for engineering solutions to ensure dam safety.
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