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首页> 外文期刊>Journal of Hydrology >Hydrological modelling of a re-wetted peatland on the basis of a limited dataset for water management
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Hydrological modelling of a re-wetted peatland on the basis of a limited dataset for water management

机译:基于有限的水管理数据集,对重新湿润的泥炭地进行水文模拟

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The valley mire 'Mittletes Trebeltal' in Mecklenburg-West Pomerania (northeast Germany) has recently been re-wetted in the course of an EU-funded conservation project. On the basis of geological cross-sections, a hydrological model applying the Boussinesq-equation has been developed to investigate the hydrological dynamics of the study area and to evaluate various management strategies. Modelled water levels corresponded well to measured ones. The optimised values of two of the main model parameters-the hydraulic conductivity and the proportions of vegetation types-agreed with measurement values, and, respectively, the real vegetation cover, while the third one, the specific yield, should pragmatically be used as a calibration parameter. Due to a proportion of around 30% of tall fen vegetation, the modelled evapotranspiration clearly exceeded grass evapotranspiration resulting in low groundwater levels in some parts of the fen during summer. Generally, the water levels are controlled by topographic features (i.e. former peat cuttings) and weather conditions during the summer months. When analyzing different management scenarios, even an optimal water supply (ditch water levels near the ground surface) could not raise the groundwater table to ecologically sound levels during summer. However, during winter, these ditch water levels enhanced flooding. The groundwater fluxes towards the river, and, respectively, towards the fen were low. The minor importance of these fluxes for the water balance was caused by very low hydraulic gradients. Therefore, it can be concluded that the risk of nutrient export from the fen into the river is very limited and compound transformations take place within the mire system itself. Hydrological analysis as a prerequisite for the assessment of nutrient and pollutant transport and transformation processes can be carried out-as a first approach-with simple models on the basis of a limited dataset. (c) 2006 Elsevier B.V. All rights reserved.
机译:梅克伦堡-前波美拉尼亚(东北德国)的山谷泥潭“ Mittletes Trebeltal”最近在欧盟资助的一项保护项目中重新湿润。在地质剖面的基础上,开发了一种采用Boussinesq方程的水文模型,以研究研究区的水文动态并评估各种管理策略。模拟的水位与测得的水位非常吻合。两个主要模型参数(水力传导率和植被类型比例)的最佳值分别与测量值和实际植被覆盖率相一致,而第三个参数(特定产量)应实用地用作校准参数。由于大约30%的芬植被比例较高,因此模拟的蒸散量明显超过了草类的蒸散量,导致夏季some部分地区的地下水位较低。通常,水位由地形特征(即以前的泥炭屑)和夏季的天气条件控制。在分析不同的管理方案时,即使是最佳的供水(靠近地面的沟渠水位)也无法在夏季将地下水位提高到生态上的合理水平。然而,在冬季,这些沟渠水位加剧了洪水泛滥。流入河流和the的地下水流量很低。这些通量对于水平衡的次要重要性是由非常低的水力梯度引起的。因此,可以得出结论,从the到河流的养分出口风险非常有限,并且在泥潭系统内部发生了复合转化。作为评估营养物和污染物迁移及转化过程的前提,可以进行水文分析(作为第一种方法),它是在有限数据集的基础上使用简单模型进行的。 (c)2006 Elsevier B.V.保留所有权利。

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