“…Because of the alkalescent water environment in the Wetland Baiyangdian, neither ammonia volatilization nor chemo‐denitrification are significant (Zhao et al, 2012). Monthly variations in TN and TP amounts in the water can be calculated through the following equations (Xu, Yang, et al, 2016). where TN t and TP t denote the TN and TP amounts (t) in the wetland water during month t (1–12), respectively; TN in, t and TP in, t denote the TN and TP amounts (t) that flow into water during month t ; TN o, t and TP o, t denote the TN and TP amounts (t) discharged through outflow; TN e, t , TN p, t , and TN b, t denote the TN amount (t) removed from water through retention in sediment, macrophyte uptake, and biological denitrification, respectively; TP e, t and TP p, t denote the TP amount (t) removed through retention in sediment and macrophyte uptake, respectively.…”