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Soluble organic nitrogen cycling in soils after application of chemical/organic amendments and groundwater pollution implications

机译:应用化学/有机修饰剂后可溶性有机氮在土壤中的循环及其对地下水污染的影响

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Nitrogen (N) fertilizers have been extensively used to maintain soil fertility in intensively agricultural soils, creating serious environmental pollution. In this study, a 70-day incubation experiment was conducted to investigate the effects of different N fertilizers (urea, manure, straw) on N mineralization, soluble organic nitrogen (SON) dynamics and its leaching potential in typical agricultural soils of the Shandong Peninsula. The results showed that the addition of N fertilizers affected the SON pools and soil N mineralization in different ways owing to their various properties and interaction with soils. When comparing treatments, urea application was found to decrease SON content, whereas manure and straw addition increased the SON content after long-term incubation. Considering that SON content depended on a complicated formation process and consumption process, no direct link between SON content and N mineralization capacity was observed in different treatments. Additionally, we analyzed free amino acids (FAAs) in SON and found that FAA content was negatively correlated with N mineralization, except for the straw treatment. This suggested that FAAs were important substrates of N mineralization in soils. In addition, the composition of SON was determined by 3-dimensional excitation-emission matrix and ultraviolet-visible absorbance spectrophotometer after long-term incubation. The PIII+v/PI+II+IV ratio, SUVA(254), and A(253)/A(203) ratio decreased after fertilizer application. This indicated that fertilizer addition decreased the SON humification degree and increased SON leaching. Therefore, SON should be taken into account when optimizing fertilization management and evaluating the risk of N leaching in groundwater systems.
机译:氮肥已被广泛用于维持集约化农业土壤中的土壤肥力,从而造成严重的环境污染。在这项研究中,进行了70天的温育实验,以研究不同氮肥(尿素,肥料,稻草)对山东半岛典型农业土壤中氮矿化,可溶性有机氮(SON)动态及其浸出潜力的影响。 。结果表明,氮肥的不同性质以及与土壤的相互作用,对SON库和土壤氮矿化的影响不同。比较处理方法时,发现尿素的施用会降低SON含量,而粪肥和秸秆的添加会在长期孵育后提高SON含量。考虑到SON含量取决于复杂的形成过程和消耗过程,因此在不同处理方法中均未观察到SON含量与氮矿化能力之间的直接联系。此外,我们分析了SON中的游离氨基酸(FAA),发现除秸秆处理外,FAA含量与N矿化成负相关。这表明FAA是土壤中N矿化的重要底物。另外,在长期孵育后,通过3维激发-发射矩阵和紫外可见吸收分光光度计确定SON的组成。施肥后PIII + v / PI + II + IV比,SUVA(254)和A(253)/ A(203)比降低。这表明肥料的添加降低了SON的增湿度并增加了SON的浸出。因此,在优化施肥管理和评估地下水系统中氮淋失的风险时,应考虑SON。

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