College of Land Science and Technology, China Agricultural University, Beijing, 100083, People's Republic of China.
College of Water Conservancy and Civil Engineering, China Agricultural University, Beijing, 100083, People's Republic of China.
Environ Sci Pollut Res Int. 2022 Aug;29(37):56511-56524. doi: 10.1007/s11356-022-19835-2. Epub 2022 Mar 26.
Accurately quantifying the distribution of nitrogen (N) contaminants in a river ecosystem is an essential prerequisite for developing scientific water quality management strategy. In this study, we have conducted a series of field investigations along the Beiyun River to collect samples from multiple scales, including surface water, riverbed sediments, vadose zone, and aquifer, for evaluating the spatial distribution of N; besides, column simulation experiments were carried out to characterize the transport behavior of N in riverbed sediments. The surface water of the Beiyun River was detected to be eutrophic because of its elevated total N concentration, which is 33 times of the threshold value causing the potential eutrophication. The hydrodynamic dispersion coefficient (D) of riverbed sediments was estimated by CXTFIT 2.1, demonstrating that the D of upstream section was lower than that of midstream and downstream sections (D < D < D), with the estimated annual N leaching volume of 130,524, 241,776, and 269,808 L/(m·a), respectively. The average total N concentration in vadose zone and aquifer of upstream Sect. (297.88 mg/kg) was obviously lower than that of midstream Sect. (402.62 mg/kg) and downstream Sect. (447.02 mg/kg). Based on multi-scale investigation data, subsequently, water quality management strategies have been achieved, that is, limiting the discharge of N from the midstream and downstream banks to the river and setting up the impermeable layer in the downstream reaches to reduce infiltration. The findings of this study are of great significance for the improvement of river environmental quality and river management.
准确量化河流生态系统中氮 (N) 污染物的分布是制定科学水质管理策略的必要前提。本研究沿北运河流域进行了一系列现场调查,从多个尺度采集了地表水、河床沉积物、包气带和含水层的样本,以评估 N 的空间分布;此外,还进行了柱模拟实验,以表征 N 在河床沉积物中的运移行为。由于北运河水体中总氮浓度升高,导致水体处于富营养化状态,其总氮浓度是可能引发潜在富营养化的阈值的 33 倍。利用 CXTFIT 2.1 估算了河床沉积物的水动力弥散系数 (D),结果表明上游段的 D 低于中游和下游段 (D<D<D),估算的年 N 淋溶量分别为 130524、241776 和 269808 L/(m·a)。上游段包气带和含水层的总氮平均浓度(297.88 mg/kg)明显低于中游段(402.62 mg/kg)和下游段(447.02 mg/kg)。基于多尺度调查数据,随后制定了水质管理策略,即限制中、下游河岸向河流排放 N,并在下游河段设置防渗层以减少入渗。本研究的发现对改善河流环境质量和河流管理具有重要意义。