In-situ study on nutrient release fluxes from shallow lake sediments under wind-driven waves

An in-situ benthic device to measure nutrient fluxes across the sediment-water interface has been developed and successfully used to study both static and dynamic fluxes of nutrients in Dianshan Lake, China. The result shows that the surface sediments of Dianshan Lake were resuspended under wind-dri...

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Published inJournal of hydrodynamics. Series B Vol. 28; no. 2; pp. 247 - 254
Main Author 孙远军 卢士强 林卫青 王道增 樊靖郁 李柱
Format Journal Article
LanguageEnglish
Published Singapore Elsevier Ltd 01.04.2016
Springer Singapore
Shanghai Academy of Environmental Sciences,Shanghai 201200,China%Institute of Applied Mathematics and Mechanics and Shanghai Key Laboratory of Mechanics in Energy Engineering,Shanghai University,Shanghai 200072,China%School of Environmental Science and Engineering,Tongji University,Shanghai 200092,China
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ISSN1001-6058
1878-0342
DOI10.1016/S1001-6058(16)60626-1

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Summary:An in-situ benthic device to measure nutrient fluxes across the sediment-water interface has been developed and successfully used to study both static and dynamic fluxes of nutrients in Dianshan Lake, China. The result shows that the surface sediments of Dianshan Lake were resuspended under wind-driven waves. DOC entered into overlying water only when sediments were resuspended. The average DOC flux was 105.78 mg/(mEd), while the static and dynamic POC fluxes were 48.22 mg/(mEd) and 10 273.20 mg/(m2d), respectively. Ammonia and nitrate had no significant release, and the dynamic flux of TN was 87.11 mg/(m2d). The release of phosphorus was the most evident, and the dynamic fluxes of SRP and DTP were 20.22 mg/(m2d) and 21.78 mg/(mEd), 2.2 and 2.0 times higher than the static fluxes, respectively. Dissolved phosphorus was released mainly as SRP, and phosphorus release from the sediments in Dianshan Lake cannot be ignored.
Bibliography:An in-situ benthic device to measure nutrient fluxes across the sediment-water interface has been developed and successfully used to study both static and dynamic fluxes of nutrients in Dianshan Lake, China. The result shows that the surface sediments of Dianshan Lake were resuspended under wind-driven waves. DOC entered into overlying water only when sediments were resuspended. The average DOC flux was 105.78 mg/(mEd), while the static and dynamic POC fluxes were 48.22 mg/(mEd) and 10 273.20 mg/(m2d), respectively. Ammonia and nitrate had no significant release, and the dynamic flux of TN was 87.11 mg/(m2d). The release of phosphorus was the most evident, and the dynamic fluxes of SRP and DTP were 20.22 mg/(m2d) and 21.78 mg/(mEd), 2.2 and 2.0 times higher than the static fluxes, respectively. Dissolved phosphorus was released mainly as SRP, and phosphorus release from the sediments in Dianshan Lake cannot be ignored.
shallow lake, wind-induced wave, hydraulic disturbance, nutrient fluxes, in-situ experiment
Yuan-jun SUN , Shi-qiang LU , Wei-qing LIN , Dao-zeng WANG, Jing-yu FAN, Zhu LI( 1. Shanghai Academy of Environmental Sciences, Shanghai 201200, China ;2. Institute of Applied Mathematics and Mechanics and Shanghai Key Laboratory of Mechanics in Energy Engineering, Shanghai University, Shanghai 200072, China 3. School of Environmental Science and Engineering, Tongji University, Shanghai 200092, China)
31-1563
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ISSN:1001-6058
1878-0342
DOI:10.1016/S1001-6058(16)60626-1