Soldatova Evgeniya, Guseva Natalia, Sun Zhanxue, Bychinsky Valeriy, Boeckx Pascal, Gao Bai
Research and Education Centre "Water", National Research Tomsk Polytechnic University, 30 Lenina Avenue, Tomsk 634050, Russia.
Research and Education Centre "Water", National Research Tomsk Polytechnic University, 30 Lenina Avenue, Tomsk 634050, Russia.
J Contam Hydrol. 2017 Jul;202:59-69. doi: 10.1016/j.jconhyd.2017.05.002. Epub 2017 May 17.
Nitrogen contamination of natural water is a typical problem for various territories throughout the world. One of the regions exposed to nitrogen pollution is located in the Poyang Lake basin. As a result of agricultural activity and dense population, the shallow groundwater of this area is characterised by a high concentration of nitrogen compounds, primarily NO, with the concentration varying from 0.1mg/L to 206mg/L. Locally, high ammonium content occurs in the shallow groundwater with low reduction potential Eh (<100mV). However, in general, the shallow groundwater of the Poyang Lake basin has Eh>100mV. To identify sources of nitrogen species and the factors that determine their behaviour, the dual stable isotope approach (δN and δО) and physical-chemical modelling were applied. Actual data were collected by sampling shallow groundwater from domestic water supply wells around the lake. The δО values from -4.1‰ to 13.9‰ with an average value of 5.3 permille indicate a significant influence of nitrification on nitrogen balance. The enrichment of nitrate with the N isotope indicates that manure and domestic sewage are the principal sources of nitrogen compounds. Inorganic nitrogen speciation and thermodynamic calculations demonstrate the high stability of nitrate in the studied groundwater. Computer simulation and field observations indicate the reducing conditions formed under joint effects of anthropogenic factors and appropriate natural conditions, such as the low-level topography in which decreased water exchange rate can occur. The simulation also demonstrates the growth in pH of the groundwater as a consequence of fertilisation, which, in turn, conduced to the clay mineral formation at lower concentrations of aqueous clay-forming components than the ones under the natural conditions.
天然水体的氮污染是世界各地区普遍存在的典型问题。鄱阳湖流域就是受氮污染影响的地区之一。由于农业活动和人口密集,该地区浅层地下水的特点是氮化合物浓度较高,主要是NO,浓度范围为0.1mg/L至206mg/L。在局部地区,浅层地下水中铵含量较高,还原电位Eh较低(<100mV)。然而,总体而言,鄱阳湖流域浅层地下水的Eh>100mV。为了确定氮物种的来源及其行为的决定因素,采用了双稳定同位素方法(δN和δО)以及物理化学建模。实际数据通过采集湖泊周边生活供水井的浅层地下水样本获得。δО值在-4.1‰至13.9‰之间,平均值为5.3‰,表明硝化作用对氮平衡有显著影响。硝酸盐的N同位素富集表明,粪便和生活污水是氮化合物的主要来源。无机氮形态分析和热力学计算表明,研究的地下水中硝酸盐具有很高的稳定性。计算机模拟和实地观测表明,在人为因素和适当的自然条件共同作用下形成了还原条件,例如低地形区域,那里的水交换率可能会降低。模拟还表明,施肥导致地下水pH值升高,这反过来又促使在比自然条件下更低的水相粘土形成组分浓度下形成粘土矿物。