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Assessment of water balance simulations for large-scale weighing lysimeters

机译:评估大型称重测渗仪的水平衡模拟

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摘要

A challenge of soil water transport modelling is the assessment of various uncertainties resulting from input data, from parameterisation of soil hydraulic characteristics and from estimation of sink terms like plant water uptake and soil evaporation. The objective of this study is to evaluate different modelling approaches for the estimation of soil hydraulic characteristics and evapotranspiration. A dataset from a lysimeter study in South-Germany with rotative crop vegetations over 5 years was used to perform the analysis. The pedotransfer functions that were used to estimate parameters for the representation of soil water retention and hydraulic conductivity have shown to be appropriate for water flow simulations. Although the simulated annual percolation amount is not very sensitive to the used soil hydraulic characteristics for the chosen boundary conditions, the diurnal percolation dynamics are highly sensitive to the soil hydraulic characteristics. The results show a strong dependence of simulated percolation on the used potential evpotranspiration (ETp) model. The Penman, Penman-Monteith and Haude approach overestimate the measured cumulative actual evapotranspiration in the present study. The measured outflow from the Lysimeters can be correctly simulated, if a modified Haude approach is used. However, in the simulation of daily evapotranspiration fluxes the physically based Penman-Monteith approach has higher correlation with measurements than the empirical approach of Haude. For the tested lysimeter data we show that depending on ETp model choice the simulated percolation amounts vary between 52% and 126% of the measured amounts. Compared to this, the influence of the parameterisation of the soil hydraulic characteristics is small with a variation of up to 5% of the measured outflow. (c) 2006 Elsevier B.V. All rights reserved.
机译:土壤水运模型的挑战是评估各种不确定性,这些不确定性是由输入数据,土壤水力特征的参数化以及诸如植物水吸收和土壤蒸发等汇项的估算所致。这项研究的目的是评估不同的建模方法,以估算土壤的水力特征和蒸散量。使用来自德国南部的蒸渗仪研究的数据集,对5年以上的作物轮作植被进行了分析。用来估计代表土壤保水率和水力传导率的参数的pedotransfer函数已显示适用于水流模拟。尽管对于选定的边界条件,模拟的年渗流量对使用的土壤水力特性不是很敏感,但昼夜渗流动力学对土壤水力特性高度敏感。结果表明,模拟渗滤强烈依赖于使用的潜在蒸散量(ETp)模型。 Penman,Penman-Monteith和Haude方法高估了本研究中测得的累积实际蒸散量。如果使用改进的Haude方法,则可以正确模拟测渗仪流出的流量。但是,在模拟日常蒸散通量时,基于物理的Penman-Monteith方法与测量的相关性高于Haude的经验方法。对于测试的溶渗仪数据,我们表明,根据ETp模型的选择,模拟的渗滤量在测得的量的52%和126%之间变化。与此相比,土壤水力特性参数化的影响很小,变化量最多为实测流出量的5%。 (c)2006 Elsevier B.V.保留所有权利。

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