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首页> 外文期刊>Hydrology and Earth System Sciences >Modelling of shallow water table dynamics using conceptual and physically based integrated surface-water-groundwater hydrologic models
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Modelling of shallow water table dynamics using conceptual and physically based integrated surface-water-groundwater hydrologic models

机译:浅水表动力学建模使用概念与物理基础的综合表面水地水土水文模型

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摘要

We present a new conceptual scheme of the interaction between unsaturated and saturated zones of the MOBIDIC (MOdello Bilancio Idrologico DIstributo e Continuo) hydrological model which is applicable to shallow water table conditions. First, MODFLOWwas coupled to MOBIDIC as the physically based alternative to the conceptual groundwater component of the MOBIDIC-MODFLOW. Then, assuming a hydrostatic equilibrium moisture profile in the unsaturated zone, a dynamic specific yield that is dependent on the water table level was added to MOBIDIC-MODFLOW, and calculation of the groundwater recharge in MOBIDIC was revisited using a power-type equation based on the infiltration rate, soil moisture deficit, and a calibration parameter linked to the initial water table depth, soil type, and rainfall intensity. Using the water table fluctuation (WTF) method for a homogeneous soil column, the parameter of the proposed groundwater recharge equation was determined for four soil types, i. e. sand, loamy sand, sandy loam, and loam under a pulse of rain with different intensities. The fidelity of the introduced modifications in MOBIDIC-MODFLOW was assessed by comparison of the simulated water tables against those of MIKE SHE, a physically based integrated hydrological modelling system simulating surface and groundwater flow, in two numerical experiments: a two-dimensional case of a hypothetical watershed in a vertical plane (constant slope) under a 1 cm dm(-1) uniform rainfall rate and a quasireal three-dimensional watershed under 1 month of a measured daily rainfall hyetograph. The comparative analysis confirmed that the simplified approach can mimic simple and complex groundwater systems with an acceptable level of accuracy. In addition, the computational efficiency of the proposed approach (MIKE SHE took 180 times longer to solve the three-dimensional case than the MOBIDIC-MODFLOW framework) demonstrates its applicability to real catchment case studies.
机译:我们提出了一种新的概念方案,其制剂(Modello Bilancio Idrologico Distronto E Con​​tinuo)水文模型的不饱和和饱和区之间的相互作用,适用于浅水表条件。首先,Modflowwas耦合到Modidic作为Mobidic-Modflow的概念性地下水部件的物理上的替代品。然后,假设不饱和区中的静水平衡水分曲线,将依赖于水位水平的动态特异性产率加入到Modidic-Modflow中,并且使用基于电力型方程重访的地下水补给的计算渗透率,土壤湿度缺陷和校准参数与初始水位深度,土壤类型和降雨强度相关联。使用用于均匀土柱的水位波动(WTF)方法,确定了四种土壤类型的所提出的地下水补给方程的参数。 e。沙,壤土,沙质壤土,和壤土在雨水下,具有不同的强度。通过将模拟水表与迈克辛的那些进行比较,在两个数值实验中比较了模拟水表,通过对迈克希的那些模拟水表模拟表面和地下水流量来评估所引入的Modic-Modflow的保证。假设的流域在垂直平面(恒定斜坡)下1厘米DM(-1)均匀的降雨率和1个月的每日降雨职谱系的Quasireal三维流域。比较分析证实,简化的方法可以采用可接受的精度模仿简单和复杂的地下水系统。此外,所提出的方法的计算效率(Mike她花了180倍以达到比MobiDic-Modflow框架的三维案例)展示了其对真实集水案例研究的适用性。

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