School of Environment, Beijing Normal University, Beijing 100875, China.
Chinese Research Academy of Environmental Sciences, Beijing 100012, China.
Sci Total Environ. 2014 Jun 15;484:10-8. doi: 10.1016/j.scitotenv.2014.03.018. Epub 2014 Mar 28.
Nitrate (NO3(-)) pollution is a severe problem in aquatic systems in Taihu Lake Basin in China. A dual isotope approach (δ(15)NNO3(-) and δ(18)ONO3(-)) was applied to identify diffused NO3(-) inputs in a stream in an agricultural field at the basin in 2013. The site-specific isotopic characteristics of five NO3(-) sources (atmospheric deposition, AD; NO3(-) derived from soil organic matter nitrification, NS; NO3(-) derived from chemical fertilizer nitrification, NF; groundwater, GW; and manure and sewage, M&S) were identified. NO3(-) concentrations in the stream during the rainy season [mean±standard deviation (SD)=2.5±0.4mg/L] were lower than those during the dry season (mean±SD=4.0±0.5mg/L), whereas the δ(18)ONO3(-) values during the rainy season (mean±SD=+12.3±3.6‰) were higher than those during the dry season (mean±SD=+0.9±1.9‰). Both chemical and isotopic characteristics indicated that mixing with atmospheric NO3(-) resulted in the high δ(18)O values during the rainy season, whereas NS and M&S were the dominant NO3(-) sources during the dry season. A Bayesian model was used to determine the contribution of each NO3(-) source to total stream NO3(-). Results showed that reduced N nitrification in soil zones (including soil organic matter and fertilizer) was the main NO3(-) source throughout the year. M&S contributed more NO3(-) during the dry season (22.4%) than during the rainy season (17.8%). AD generated substantial amounts of NO3(-) in May (18.4%), June (29.8%), and July (24.5%). With the assessment of temporal variation of diffused NO3(-) sources in agricultural field, improved agricultural management practices can be implemented to protect the water resource and avoid further water quality deterioration in Taihu Lake Basin.
硝酸盐(NO3(-))污染是中国太湖流域水体的一个严重问题。2013 年,采用双同位素方法(δ(15)NNO3(-)和 δ(18)ONO3(-)),对流域内农田溪流中扩散的 NO3(-)输入进行了识别。确定了五种 NO3(-)源(大气沉降、AD;土壤有机质硝化产生的 NO3(-)、NS;化肥硝化产生的 NO3(-)、NF;地下水、GW;以及粪肥和污水、M&S)的特定位置同位素特征。雨季(平均值±标准差(SD)=2.5±0.4mg/L)溪流中的 NO3(-)浓度低于旱季(平均值±SD=4.0±0.5mg/L),而雨季(平均值±SD=+12.3±3.6‰)的 δ(18)ONO3(-)值高于旱季(平均值±SD=+0.9±1.9‰)。化学和同位素特征均表明,雨季大气 NO3(-)的混合导致了高 δ(18)O 值,而 NS 和 M&S 是旱季的主要 NO3(-)源。贝叶斯模型用于确定每个 NO3(-)源对总溪流 NO3(-)的贡献。结果表明,土壤区(包括土壤有机质和肥料)中氮的还原硝化是全年的主要 NO3(-)源。旱季(22.4%)M&S 贡献的 NO3(-)多于雨季(17.8%)。AD 在 5 月(18.4%)、6 月(29.8%)和 7 月(24.5%)产生了大量的 NO3(-)。通过评估农业区扩散的 NO3(-)源的时间变化,可以实施改进的农业管理实践,以保护水资源并避免太湖流域水质进一步恶化。