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Modification of the MONERIS Nutrient Emission Model for a Lowland Country (Hungary) to Support River Basin Management Planning in the Danube River Basin

机译:修改低地国家(匈牙利)的野生营养发射模型,以支持多瑙河流域河流域管理规划

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The contamination of waters with nutrients, especially nitrogen and phosphorus originating from various diffuse and point sources, has become a worldwide issue in recent decades. Due to the complexity of the processes involved, watershed models are gaining an increasing role in their analysis. The goal set by the EU Water Framework Directive (to reach "good status" of all water bodies) requires spatially detailed information on the fate of contaminants. In this study, the watershed nutrient model MONERIS was applied to the Hungarian part of the Danube River Basin. The spatial resolution was 1078 water bodies (mean area of 86 km(2)); two subsequent 4 year periods (2009-2012 and 2013-2016) were modeled. Various elements/parameters of the model were adjusted and tested against surface and subsurface water quality measurements conducted all over the country, namely (i) the water balance equations (surface and subsurface runoff), (ii) the nitrogen retention parameters of the subsurface pathways (excluding tile drainage), (iii) the shallow groundwater phosphorus concentrations, and (iv) the surface water retention parameters. The study revealed that (i) digital-filter-based separation of surface and subsurface runoff yielded different values of these components, but this change did not influence nutrient loads significantly; (ii) shallow groundwater phosphorus concentrations in the sandy soils of Hungary differ from those of the MONERIS default values; (iii) a significant change of the phosphorus in-stream retention parameters was needed to approach measured in-stream phosphorus load values. Local emissions and pathways were analyzed and compared with previous model results.
机译:近几十年来污染营养成分,尤其是来自各种漫射和点来源的氮素和磷,已成为全球问题。由于所涉及的过程的复杂性,流域模型在分析中取得了越来越大的作用。欧盟水框架指令设定的目标(达到所有水体的“良好状态”)需要有关污染物的命运的空间详细信息。在这项研究中,流域营养模型Moneris应用于多瑙河流域的匈牙利部分。空间分辨率为1078个水体(平均面积86公里(2));建模两个后续4年期(2009-2012和2013-2016)。调整和测试模型的各种元素/参数,对整个国家进行的表面和地下水质测量进行了调整和测试,即(i)水平方程(表面和地下径流),(ii)地下途径的氮保留参数(不包括瓦片排水),(iii)浅层地下水磷浓度,(iv)表面水保留参数。该研究表明,(i)基于数字滤波器的表面和地下径流的分离产生了这些组分的不同值,但这种变化不会显着影响营养载荷; (ii)匈牙利砂土中的浅层地下水磷浓度不同于蒙尾默认值的土壤; (iii)需要在流中磷载荷值测量的流中磷含磷载荷值的显着变化。分析了当地排放和途径,并与先前的模型结果进行了比较。

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