Ditches function as vital biogeochemical buffers that mediate phosphorus (P) transport from agricultural landscapes to downstream water bodies. However, their capacity to retain or release P is highly sensitive to hydrodynamic forces, particularly flow velocity. In this study, we employed a controlled ditch mesocosm to investigate the effects of contrasting flow velocities (V3: 3 cm s−1; V10: 10 cm s−1) on P dynamics. Total P (TP) concentrations in the water column declined under both treatments, with the maximum TP removal rate reaching 209 μmol P m−2 h−1 at 12 h under V3, compared to 184 μmol P m−2 h−1 under V10. Particulate P (PP) behavior exhibited flow-dependence: sedimentation dominated under V3, while V10 induced sediment resuspension and elevated PP concentrations. High flow conditions also stimulated alkaline phosphatase (ALP) activity and microbial diversity in suspended particulate matter (SPM), accelerating organic P (OP) mineralization. Diffusive P flux across the sediment–water interface was significantly greater under V10 (0.58 pg s−1 cm−2) than V3 (0.38 pg s−1 cm−2), driven by shear stress and redox fluctuations. Sediment-derived P resuspension increased nearly ninefold under V10 (7.54 mg m−2 h−1) relative to V3 (0.88 mg m−2 h−1). These findings demonstrate that flow velocity governs the balance between P retention and release through interacting physical and microbial processes, offering new insight into the design and management of ecologically engineered ditch systems.
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