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From meso- to macro-scale dynamic water quality modelling for the assessment of land use change scenarios

机译:从中尺度到宏观尺度的动态水质建模,以评估土地利用变化情景

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The implementation of the European Water Framework Directive requires reliable tools to predict the water quality situations in streams caused by planned land use changes at the scale of large regional river basins. This paper presents the results of modelling the in-stream nitrogen load and concentration within the macro-scale basin of the Saale river (24,167 km(2)) using a semi-distributed process-based ecohydrological dynamic model SWIM (Soil and Water Integrated Model). The simulated load and concentration at the last gauge of the basin show that SWIM is capable to provide a satisfactory result for a large basin. The uncertainty analysis indicates the importance of realistic input data for agricultural management, and that the calibration of parameters can compensate the uncertainty in the input data to a certain extent. A hypothesis about the distributed nutrient retention parameters for macro-scale basins was tested aimed in improvement of the simulation results at the intermediate gauges and the outlet. To verify the hypothesis, the retention parameters were firstly proved to have a reasonable representation of the denitrification conditions in six meso-scale catchments. The area of the Saale region was classified depending on denitrification conditions in soil and groundwater into three classes (poor, neutral and good), and the distributed parameters were applied. However, the hypothesis about the usefulness of distributed retention parameters for macro-scale basins was not confirmed. Since the agricultural management is different in the sub-regions of the Saale basin, land use change scenarios were evaluated for two meso-scale subbasins of the Saale. The scenario results show that the optimal agricultural land use and management are essential for the reduction in nutrient load and improvement of water quality to meet the objectives of the European Water Framework Directive and in view of the regional development plans for future.
机译:《欧洲水框架指令》的实施需要可靠的工具来预测大型区域河流流域范围内因计划的土地利用变化而引起的河流水质状况。本文介绍了使用基于过程的半分布式生态水文学动态模型SWIM(水土流失综合模型)对萨勒河(24,167 km(2))宏观尺度流域内河床内氮负荷和浓度进行建模的结果)。在盆地最后一个标尺上模拟的载荷和浓度表明,SWIM能够为大型盆地提供令人满意的结果。不确定性分析表明了实际输入数据对农业管理的重要性,并且参数的校准可以在一定程度上补偿输入数据中的不确定性。测试了关于大型流域养分保留参数分布的假设,旨在改善中间水位和出口处的模拟结果。为了验证该假设,首先证明保留参数能够合理代表六个中尺度集水区的反硝化条件。根据土壤和地下水中的反硝化条件,将萨累地区的区域分为三类(差,中性和良),并应用分布参数。然而,关于宏观尺度盆地分布保留参数有用性的假设尚未得到证实。由于萨勒河流域次区域的农业管理方式不同,因此对萨勒的两个中尺度子流域的土地利用变化方案进行了评估。情景结果表明,为了满足欧洲水框架指令的目标以及未来的区域发展计划,最佳的农业土地利用和管理对于减少营养负荷和改善水质至关重要。

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