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Impact of varying dissolved organic carbon load on sediment phosphorus release and its periodic mechanisms.
Zhang, Shiyao; Zeng, Yuhong; Liu, Runpei; Liu, Xiaoning; Xue, Yingwen.
Afiliação
  • Zhang S; State Key Laboratory of Water Resources Engineering and Management, Wuhan University, Wuhan, 430072, China.
  • Zeng Y; State Key Laboratory of Water Resources Engineering and Management, Wuhan University, Wuhan, 430072, China. Electronic address: yhzeng@whu.edu.cn.
  • Liu R; State Key Laboratory of Water Resources Engineering and Management, Wuhan University, Wuhan, 430072, China.
  • Liu X; State Key Laboratory of Water Resources Engineering and Management, Wuhan University, Wuhan, 430072, China.
  • Xue Y; School of Civil Engineering, Wuhan University, Wuhan, 430072, China.
Environ Res ; 259: 119558, 2024 Oct 15.
Article em En | MEDLINE | ID: mdl-38969317
ABSTRACT
Phosphorus (P) release from sediment poses a severe challenge for eutrophication management in the aquatic environment. The dissolved organic carbon (DOC) concentrations in riverine ecosystems have shown an increasing trend due to intensified climate change and anthropogenic activities, while their impact on sediment P cycling remains unclear. To investigate the effects of different DOC loads on sediment P release and the underlying mechanisms, we conducted a two-month experiment in 15 plexiglass tanks, with five gradient-increasing target DOC concentrations set according to reality control (S0), 5 mg/L (S5), 10 mg/L (S10), 15 mg/L (S15), and 20 mg/L (S20). The results demonstrated that i) DOC enrichment promoted the sediment P mobilization and release, with the underlying mechanisms exhibited periodic characteristics. ii) reduced dissolved oxygen (DO) concentration and stimulated alkaline phosphatase activity (APA) were likely the primary and sustained facilitating mechanisms. While after the termination of DOC load, elevated pH level was also considered a contributing factor when chlorophyll a (Chl a) ranged between 5.9 µg/L and 7.7 µg/L iii) ultimate concentration of total P (TP) in the overlying water depended on DOC load. After DOC addition was terminated, decreased TP concentrations were observed when DOC concentration was in the range of 5-15 mg/L, which may be attributed to the direct uptake of P by phytoplankton counteracting the minor promotion of P release induced by anoxic conditions. However, when DOC concentrations exceeded 15-20 mg/L, there were notable increments in TP concentrations. Our findings provide further insight into the response mechanisms of sediment P release to the increasing organic C load in natural ecosystems. The impact of broader C forms or C loads on sediment P cycling needs to be fully elucidated and even quantified in future studies, especially through large-scale field investigations to further clarify the coupled roles between C and P.
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Texto completo: 1 Base de dados: MEDLINE Assunto principal: Fósforo / Carbono / Sedimentos Geológicos Idioma: En Ano de publicação: 2024 Tipo de documento: Article

Texto completo: 1 Base de dados: MEDLINE Assunto principal: Fósforo / Carbono / Sedimentos Geológicos Idioma: En Ano de publicação: 2024 Tipo de documento: Article