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Evaluation of water and nutrient dynamics in soil-crop systems using the eco-hydrological catchment model SWIM

机译:使用生态水文集水模型游泳评价土壤 - 作物系统中的水和养分动力学

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The process-based eco-hydrological spatially distributed catchment model SWIM (Soil and Water Integrated Model) was used to model water and nutrient dynamics in soil-crop systems. SWIM integrates hydrological processes, vegetation/crop growth, erosion, soil carbon, phosphorous and nitrogen dynamics at the river basin scale. A module for the turnover of soil organic matter was recently added by integrating the soil organic matter module of the forest growth model 4C into SWIM. As part of the model evaluation exercise described in this paper, SWIM was evaluated against data on soil temperature, soil hydrology, crop yield, soil nitrogen and long-term soil organic matter dynamics at the plot scale. The model was run predominantly without calibration except for parameterization data provided for the field plots (e.g. soil physical parameters). Soil temperature and soil water were simulated well, with modelling efficiency index (IA) 0.87-0.96 for soil temperature and 0.54—0.92 for soil water. Simulatedcrop yield compared satisfactory well to measured yield, with IA values ranging from 0.37 to 0.87. Some problems occurred for long-term simulations (51 years) due to the fact that SWIM does not consider technical management changes such as seed quality improvements. Soil nitrogen dynamics were represented satisfactory under the different crop rotation and fertilization regimes at the measurement sites. Modelling efficiency index varied between 0.18 and 0.79. The simulation of long-term soil carbon dynamics resulted in a good representation of the measurements under the different fertilization treatments. The long-term trend of soil organic carbon (SOC) could be successfully represented by SWIM with a modelling efficiency index between 0.46 and 0.69. Although SWIM was not designed as a plot or field scale agro-ecosystem model, it was able to reproduce the measured data for different plots, representing different edaphic, climatic and management conditions, in their temporal dynamics and magnitudes.
机译:基于过程的生态水文空间分布式集水模型游泳(土壤和水综合模型)用于模拟土壤作物系统中的水和营养动力学。游泳将水文过程,植被/作物生长,侵蚀,土壤碳,磷和氮动力学纳入河流级。最近通过将森林生长模型4C的土壤有机物质模块与游泳池集成来添加土壤有机物质的营业件的模块。作为本文描述的模型评估运动的一部分,在绘图标度下对土壤温度,土壤水文,作物产量,土壤氮和长期土壤有机物质动力学进行评估。除了为字段图提供的参数化数据(例如土壤物理参数)提供的参数化数据之外,该模型主要运行而没有校准。模拟土壤温度和土壤水分,采用效率指数(IA)为0.87-0.96,土壤温度为0.54-0.92。模拟克服率与测量产率相比令人满意的良好,IA值范围为0.37至0.87。长期模拟(51年)发生的一些问题是由于游泳不考虑技术管理的变化,例如种子质量改进。在测量部位的不同作物旋转和施肥制度下,土壤氮动力学在令人满意的令人满意。建模效率指数在0.18和0.79之间变化。长期土壤碳动力学的模拟导致不同施肥处理下测量的良好代表性。土壤有机碳(SOC)的长期趋势可以通过游泳成功地代表,其建模效率指数在0.46和0.69之间。虽然游泳不是设计为绘图或现场规模的农业生态系统模型,但它能够在其时间动态和大小的时间动态和幅度中复制不同地块的测量数据,代表不同的仿乳管,气候和管理条件。

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