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Understanding nitrogen transfer dynamics in a small agricultural catchment: Comparison of a distributed (TNT2) and a semi distributed (SWAT) modeling approaches

机译:了解小型农业流域中氮的迁移动态:分布式(TNT2)和半分布式(SWAT)建模方法的比较

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摘要

The coupling of an hydrological and a crop model is an efficient approach to study the impact of the interactionsudbetween agricultural practices and catchment physical characteristics on stream water quality.udWe analyzed the consequences of using different modeling approaches of the processes controlling theudnitrogen (N) dynamics in a small agricultural catchment monitored for 15 years. Two agro-hydrologicaludmodels were applied: the fully distributed model TNT2 and the semi-distributed SWAT model. Using theudsame input dataset, the calibration process aimed at reproducing the same annual water and N balance inudboth models, to compare the spatial and temporal variability of the main N processes. The models simulateduddifferent seasonal cycles for soil N. The main processes involved were N mineralization and denitrification.udTNT2 simulated marked seasonal variations with a net increase of mineralization in autumn,udafter a transient immobilization phase due to the burying of the straw with low C:N ratio. SWAT predicteduda steady humus mineralization with an increase when straws are buried and a decrease afterwards.udDenitrification was mainly occuring in autumn in TNT2 because of the dynamics of Nudavailability in soil and of the climatic and hydrological conditions. SWAT predicts denitrification in winter,udwhen mineral N is available in soil layers. The spatial distribution of these two processes was differentudas well: less denitrification in bottom land and close to ditches in TNT2, as a result of N transferuddynamics. Both models simulate correctly global trend and inter-annual variability of N losses in smalludagricultural catchment when a sufficient amount data is available for calibration. However, N processesudand their spatial interactions are simulated very differently, in particular soil mineralization and denitrification.udThe use of such tools for prediction must be considered with care, unless a proper calibration andudvalidation of the different N processes is carried out.
机译:水文模型和作物模型的耦合是研究农业实践与流域物理特征之间的相互作用对河流水质的影响的有效方法。 ud我们分析了采用不同建模方法控制氮气的后果(N)监测了15年的小型农业流域的动态。应用了两种农业水文 ud模型:完全分布式模型TNT2和半分布式SWAT模型。使用 udsame输入数据集,校准过程旨在在两个模型中重现相同的年度水和N平衡,以比较主要N个过程的时空变异性。该模型模拟了土壤氮的不同季节循环。涉及的主要过程是氮的矿化和反硝化。 udTNT2模拟了秋季明显的季节变化,秋季矿化净增加,由于土壤被秸秆掩埋而暂时固定化之后。 C:N比低。 SWAT预测稳定的腐殖质矿化作用,当秸秆被埋时增加,随后减少。 ud由于土壤中N有效性的变化以及气候和水文条件的变化,反硝化作用主要发生在TNT2的秋季。当土壤层中存在矿物质氮时,特警预测冬天会反硝化。这两个过程的空间分布差异非常大:由于N转移超动力学的结果,底部土地的反硝化作用较少,而TNT2中的沟渠则接近。当有足够数量的数据可用于校准时,这两个模型都可以正确模拟小型农业流域氮素损失的总体趋势和年际变化。但是,对N个过程及其空间相互作用的模拟非常不同,特别是在土壤矿化和反硝化过程中。 ud必须谨慎考虑使用此类工具进行预测,除非对不同N个过程进行了适当的校准和验证。

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