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Super typhoon induced high silica export from Arakawa River, Japan
Atsushi Kubo1, Natsuki Yamahira2
1Department of Geosciences, Shizuoka University, 856 Ohya, Suruga-ku, Shizuoka city, Shizuoka Prefecture, 422-8529, Japan. kubo.atsushi@shizuoka.ac.jp.
Summary
Sewage treatment plants are the main source of dissolved silicate (DSi) in rivers during normal conditions. However, extreme flooding events significantly increase particulate silica (PSi) and DSi loading, surpassing annual amounts.
Area of Science:
- Environmental Chemistry
- Riverine Geochemistry
- Water Quality Monitoring
Background:
- Sewage treatment plants (STP) are recognized as significant contributors to dissolved silicate (DSi) in riverine systems.
- Understanding silica dynamics, including both dissolved (DSi) and particulate (PSi) forms, is crucial for aquatic ecosystem health.
- The impact of extreme weather events, such as typhoons, on nutrient loading in rivers requires detailed investigation.
Purpose of the Study:
- To quantify dissolved silicate (DSi) and particulate silica (PSi) concentrations and loading in the Arakawa River.
- To identify the primary sources of DSi, particularly the role of sewage treatment plant (STP) effluents.
- To assess the impact of extreme flooding events, exemplified by super Typhoon Hagibis, on silica dynamics in the river.
Main Methods:
- Continuous monitoring of DSi and PSi concentrations in the Arakawa River and STP effluents over a one-year period (October 2018 - October 2019).
- Inclusion of data from a major flooding event following super Typhoon Hagibis.
- Calculation of silica loading rates under ordinary and flooding conditions.
Main Results:
- STP effluents were identified as the dominant source of DSi during periods of ordinary water levels.
- During flooding, DSi concentrations decreased by approximately 25%, while PSi concentrations increased over sixteenfold compared to normal conditions.
- Silica loading during flooding events, driven by both elevated DSi and PSi, significantly exceeded the calculated annual loading under normal conditions.
Conclusions:
- Riverine silica loading is highly influenced by hydrological events, with flooding dramatically altering the DSi/PSi ratio and total load.
- STPs play a key role in DSi input during non-flood periods, but extreme events introduce substantial particulate silica.
- Effective management strategies for riverine silica require consideration of both chronic inputs from STPs and episodic loading during major flood events.
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