The hydrodynamics, water temperature, and water quality model for the Dan River and Renzhuang Reservoir continuum were developed using field monitoring data and the Environmental Fluid Dynamics Code (EFDC). An in-situ water discharge experiment enabled the calculation of water propagation time using a simulated flood progression method and the hydrodynamics module of EFDC. Based on these model results, degradation coefficients for chemical oxygen demand, biochemical oxygen demand, nitrogen (N), phosphorus (P), fluoride, arsenic were determined, revealing significantly higher values when the wetland barrage was opening. According to field monitoring and EFDC model outputs, the water environment capacity (WEC) of total nitrogen (TN) in Dan River was even negative, with the WEC of TN and total phosphorus (TP) in Renzhuang Reservoir being very low at 147 kg/d and 1490 kg/d, respective. Furthermore, the water environment carrying capacity (WECC) was found to be extremely low (~0.2 %) and limited by TN and TP. The results demonstrated that the spatiotemporal variations of water quality presented by the EFDC model facilitate an intuitive and comprehensive observation of water quality compliance rates over time and space, providing valuable references for decision-makers. The WEC and WECC of the study area underscored the urgency of N and P coordination control.
Keywords: Dan River; Degradation coefficient; Renzhuang Reservoir; Water environmental carrying capacity; Water quality; Wetland.
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