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Modelling the ecosystem effects of nitrogen deposition: Model of Ecosystem Retention and Loss of Inorganic Nitrogen (MERLIN

机译:氮沉降对生态系统影响的建模:生态系统保留和无机氮损失的模型(MERLIN

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A catchment-scale mass-balance model of linked carbonand nitrogen cycling in ecosystems has been developed for simulating leachinglosses of inorganic nitrogen. The model (MERLIN) considers linked bioticand abiotic processes affecting the cycling and storage of nitrogen. Themodel is aggregated in space and time and contains compartments intendedto be observable and/or interpretable at the plot or catchment scale. Thestructure of the model includes the inorganic soil, a plant compartmentand two soil organic compartments. Fluxes in and out of the ecosystem andbetween compartments are regulated by atmospheric deposition, hydrologicaldischarge, plant uptake, litter production, wood production, microbialimmobilization, mineralization, nitrification, and denitrification. Nitrogenfluxes are controlled by carbon productivity, the C:N ratios of organiccompartments and inorganic nitrogen in soil solution. Inputs required are:1) temporal sequences of carbon fluxes and pools- 2) time series of hydrologicaldischarge through the soils, 3) historical and current external sourcesof inorganic nitrogen; 4) current amounts of nitrogen in the plant andsoil organic compartments; 5) constants specifying the nitrogen uptakeand immobilization characteristics of the plant and soil organic compartments;and 6) soil characteristics such as depth, porosity, bulk density, andanion/cation exchange constants. Outputs include: 1) concentrations andfluxes of NO3 and NH4 in soil solution and runoff; 2) total nitrogen contentsof the organic and inorganic compartments; 3) C:N ratios of the aggregatedplant and soil organic compartments; and 4) rates of nitrogen uptake andimmobilization and nitrogen mineralization. The behaviour of the modelis assessed for a combination of land-use change and nitrogen depositionscenarios in a series of speculative simulations. The results of the simulationsare in broad agreement with observed and hypothesized behaviour of nitrogendynamics in growing forests receiving nitrogen deposition.
机译:建立了生态系统中碳氮循环相关的流域规模质量平衡模型,用于模拟无机氮的淋失。该模型(MERLIN)考虑了影响氮循环和存储的相关生物和非生物过程。该模型在空间和时间上聚合在一起,包含旨在在地块或集水区规模上可观察和/或解释的隔室。模型的结构包括无机土壤,植物区室和两个土壤有机区室。生态系统内外的通量和车厢之间的通量受大气沉积,水文排放,植物吸收,凋落物生产,木材生产,微水分解,矿化,硝化和反硝化的调节。氮通量由​​碳生产率,土壤溶液中有机隔室和无机氮的碳氮比控制。所需的输入是:1)碳通量和池的时间序列-2)通过土壤的水文排放的时间序列,3)无机氮的历史和当前外部来源; 4)植物和土壤有机隔间中当前的氮含量; 5)规定植物和土壤有机区氮吸收和固定特性的常数;和6)诸如深度,孔隙率,堆积密度和阴离子/阳离子交换常数的土壤特性。产出包括:1)土壤溶液和径流中NO 3 和NH 4 的浓度和通量; 2)有机和无机隔室的总氮含量; 3)聚集植物和土壤有机区室的碳氮比; 4)氮素吸收固定化和氮矿化的速率。在一系列推测性模拟中,针对土地利用变化和氮沉降情景的组合评估了模型的行为。模拟的结果与在接受氮沉降的生长森林中观察到的和假设的氮动力学行为基本一致。

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