Bao Xin, Jiang Yan, Hu Yu-Cong
State Key Laboratory of Urban and Regional Ecology, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China.
University of Chinese Academy of Sciences, Beijing 100049, China.
Huan Jing Ke Xue. 2021 Jul 8;42(7):3316-3327. doi: 10.13227/j.hjkx.202009181.
In semi-arid and semi-humid areas, the occurrence of non-point source nutrient pollution is mainly driven by rainfall-runoff events, and nutrient loss under rainfall events determines annual total pollution load. Therefore, research on riverine nutrient dynamics under rainfall-runoff events in flood seasons is critical for simulating and controlling pollution load in semi-arid and semi-humid areas. The Chaohe River watershed, upstream watershed of Miyun Reservoir in Beijing was considered as study area, water quantity and quality of rainfall-runoff process at Gubeikou and Xiahui stations were monitored synchronously in flood seasons in 2018 and 2019. The results indicated the following:① Among the three rainfall events (E1, E2, and E3), E1 had the highest precipitation and rainfall intensity, and the corresponding discharge and pollutant concentrations were the highest. ② Under different rainfall events, the pollutant concentrations and their variations were different. The variations of concentrations of total nitrogen (TN), ammonia (NH-N), nitrate (NO-N), total phosphorus (TP), and total suspended solids (TSS) were similar to the discharge process under the heavy rainstorm event (E1) and the rainstorm event (E3). The concentrations of total nitrogen (TN), ammonia (NH-N), total phosphorus (TP), and total suspended solids (TSS) were similar to the discharge process under the heavy rain events (E2), but the variations of nitrate (NO-N) concentrations were opposite to those in the discharge process. ③ The concentrations and variations of different forms of pollutants were different under different rainfall events. Under the event of strong rainfall erosion (E1 and E2), the concentrations of particulate pollutants varied significantly, being positively correlated with that of total suspended solids (TSS). For the rainfall event that did not cause soil erosion (E3), the forms of nitrogen and phosphorus were dominated by total dissolved nitrogen (TDN) and total dissolved phosphorus (TDP) respectively, whose variations were mainly related to discharge. ④ The discharge and pollutant concentrations at each station varied under different rainfall events. Heavy rainfall erosion was more obvious at Gubeikou station, causing significant variations in discharge, TP, and TSS. Therefore, these results can be used to determine migration patterns of non-point source pollutants caused by rainfall-runoff events and provide references for water quality prediction and control in flood seasons.
在半干旱和半湿润地区,非点源养分污染的发生主要由降雨径流事件驱动,降雨事件下的养分流失决定了年度总污染负荷。因此,研究汛期降雨径流事件下河流水体养分动态对于模拟和控制半干旱和半湿润地区的污染负荷至关重要。以北京密云水库上游流域潮河流域为研究区域,于2018年和2019年汛期同步监测了古北口站和下会站降雨径流过程的水量和水质。结果表明:①在三次降雨事件(E1、E2和E3)中,E1的降水量和降雨强度最高,相应的流量和污染物浓度也最高。②在不同降雨事件下,污染物浓度及其变化情况不同。在暴雨事件(E1)和暴雨事件(E3)下,总氮(TN)、氨氮(NH-N)、硝态氮(NO-N)、总磷(TP)和总悬浮固体(TSS)浓度的变化与流量过程相似。在大雨事件(E2)下,总氮(TN)、氨氮(NH-N)、总磷(TP)和总悬浮固体(TSS)浓度与流量过程相似,但硝态氮(NO-N)浓度变化与流量过程相反。③不同降雨事件下不同形态污染物的浓度和变化情况不同。在强降雨侵蚀事件(E1和E2)下,颗粒态污染物浓度变化显著,与总悬浮固体(TSS)呈正相关。对于未造成土壤侵蚀的降雨事件(E3),氮和磷的形态分别以总溶解氮(TDN)和总溶解磷(TDP)为主,其变化主要与流量有关。④不同降雨事件下各站点的流量和污染物浓度各不相同。古北口站的强降雨侵蚀更为明显,导致流量、TP和TSS发生显著变化。因此,这些结果可用于确定降雨径流事件引起的非点源污染物迁移模式,为汛期水质预测和控制提供参考。