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使用SWAP和ANIMO模型对保加利亚一个试验田的水流和氮素运移进行模拟。

Simulation of water flow and nitrogen transport for a Bulgarian experimental plot using SWAP and ANIMO models.

作者信息

Marinov Dimitar, Querner Erik, Roelsma Jan

机构信息

Institute of Water Problems, Bulgarian Academy of Sciences, 1113 Sofia, Bulgaria.

出版信息

J Contam Hydrol. 2005 Apr;77(3):145-64. doi: 10.1016/j.jconhyd.2004.12.004.

Abstract

Unsaturated zone models are useful tools in predicting effects of measures and can be used to optimise agricultural practice aiming to minimise the impact on the environment. However, current soil models have a varying degree of abstraction level referring to simulated processes in time and space. In the framework of an EU funded project the SWAP (Soil-Water-Atmosphere-Plant) and ANIMO (Agricultural-Nutrient-Model) models were tested for an experimental arable plot in Bulgaria. SWAP was used to simulate water flow in the soil while ANIMO describes nitrogen movement and transformations. The objectives of this study are: (i) to show results of the combined application of water and nitrogen dynamics of originally Dutch models SWAP and ANIMO for specific Bulgarian soil and hydrological conditions; (ii) to calibrate and evaluate SWAP and ANIMO models by comparing numerical results with field measurements collected for an arable field in western Bulgaria and (iii) to analyse possible contamination of groundwater due to agricultural practice in the considered region. Further a short description of the experimental plot, as well as information about parameters of the investigated soil profiles, is provided. The obtained SWAP results evidenced that the model gives sufficient adaptation for soil water dynamics. The simulations of ANIMO for nitrogen cycle show greater divergence with observations but are satisfactory precise for the purposes of assessing land use impact on groundwater quality. In general, differences between model results and field measurements do not exceed 10-15%. For the experimental plot predictions indicate nitrate-N concentrations less then 5 mg/l in deeper soil compartments and low downward annual flux containing 0.133 kg N/ha. These results indicate that there is no serious pollution of the shallow groundwater table by nitrogen resulting from land use and agricultural activities.

摘要

非饱和带模型是预测措施效果的有用工具,可用于优化农业实践,以尽量减少对环境的影响。然而,当前的土壤模型在时空模拟过程方面具有不同程度的抽象水平。在一个欧盟资助项目的框架内,对保加利亚一块试验性耕地测试了SWAP(土壤-水-大气-植物)模型和ANIMO(农业养分模型)。SWAP用于模拟土壤中的水流,而ANIMO描述氮的迁移和转化。本研究的目的是:(i)展示最初为荷兰条件设计的SWAP和ANIMO模型的水氮动态联合应用针对保加利亚特定土壤和水文条件的结果;(ii)通过将数值结果与保加利亚西部一块耕地收集的实地测量数据进行比较,对SWAP和ANIMO模型进行校准和评估;以及(iii)分析所考虑区域农业实践可能对地下水造成的污染。此外,还提供了试验地块的简要描述以及所研究土壤剖面的参数信息。获得的SWAP结果表明,该模型对土壤水分动态有足够的适应性。ANIMO对氮循环的模拟结果与观测值有较大差异,但对于评估土地利用对地下水质量的影响而言精度令人满意。总体而言,模型结果与实地测量值之间的差异不超过10 - 15%。对于试验地块,预测表明较深土壤层中硝态氮浓度低于5毫克/升,年向下通量较低,为0.133千克氮/公顷。这些结果表明,土地利用和农业活动产生的氮并未对浅层地下水位造成严重污染。

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