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Using dual isotopes to identify sources and transformations of nitrogen in water catchments with different land uses, Loess Plateau of China

机译:利用双同位素识别不同土地利用方式集水区中氮的来源和转化,中国黄土高原

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摘要

Nitrogen pollution in rivers is a research hotspot in the field of biogeochemistry. However, the types and sources of pollution have historically been poorly understood in the water catchments of the Loess Plateau in China. In this study, we have chosen the main waterway and four lesser branches of the Jinghe River that vary by land use. We investigated the concentrations and isotopic signatures of nitrogen in river water. Our results revealed that nitrate was the dominant nitrogen type in river catchments of the Loess Plateau. The delta N-15 and delta O-18 values showed that NO3- ions in the studied river samples were derived from precipitation, manure, sewage, soil organic nitrogen, and synthetic NO3- fertilizer. The delta O-18-NO3- values during July 2012 (mean +/- SD=+18.1 +/- 1.5%) were higher than those during the September 2013 (mean +/- SD=+7.8 +/- 3.7%), which indicated that mixing with atmospheric NO3- resulted in the high delta O-18 values during July 2012. It appears that no intense nitrification and denitrification occurred in all five rivers according to the isotopic and chemical data. A Bayesian model was used to determine the contributions of four NO3- sources to all five rivers. Results showed that source contributions differ significantly between July and September, and the four potential NO3- sources also showed high variability between the different land use areas.
机译:河流中的氮污染是生物地球化学领域的研究热点。但是,历史上人们对中国黄土高原集水区的污染类型和来源知之甚少。在这项研究中,我们选择了he河的主要水道和四个较小的支流,这些支流随土地利用而变化。我们调查了河水中氮的浓度和同位素特征。我们的结果表明,硝酸盐是黄土高原河流集水区的主要氮类型。 δN-15和δO-18值表明,所研究的河流样本中的NO3-离子来自降水,肥料,污水,土壤有机氮和合成NO3-肥料。 2012年7月(平均值+/- SD = + 18.1 +/- 1.5%)的O-18-NO3-δ值高于2013年9月(平均值+/- SD = + 7.8 +/- 3.7%) ,这表明与大气中NO3-的混合导致2012年7月的O-18值较高。根据同位素和化学数据,所有5条河流似乎都没有发生强烈的硝化和反硝化作用。贝叶斯模型用于确定四个NO3排放源对所有五条河流的贡献。结果表明,来源贡献在7月和9月之间存在显着差异,并且四种潜在的NO3来源在不同土地利用区域之间也显示出很大的差异。

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