锰
磷
中国
动员
地球化学
环境科学
沉积物
地质学
地理
考古
冶金
地貌学
材料科学
作者
Quan Chen,Jingfu Wang,Meng-Qiang Zhu,Haibo Qin,Peng Liao,Zhi-Tong Lu,Pengcheng Ju,Jing-an Chen
标识
DOI:10.1016/j.scitotenv.2024.176564
摘要
Eutrophication has become one of the greatest threats to aquatic ecosystems. The release of phosphorus (P) from sediments exerts a critical role on eutrophication level. Both manganese (Mn) and iron (Fe), sensitive to redox conditions, own strong affinity for P. Numerous works have demonstrated that Fe was a key factor to drive P cycle in sediments. However, the role of Mn on P mobilization remains largely unexplored. Herein, the mechanism of P mobilization driven by Mn were investigated in a seasonal anoxic reservoir. Diffusive gradients in thin films (DGT) results, from both field investigations and laboratory incubations, showed P was synchronously distributed and significantly positive correlated (r
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