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A conceptual–numerical model to simulate hydraulic head in aquifers that are hydraulically connected to surface water bodies (pages 1435–1448)

机译:模拟液压头液压液体液压液体液体液压头的概念 - 数值模型(第1435-1448页)

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In this paper, we present a conceptual-numerical model that can be deduced from a calibrated finite difference groundwaterflowmodel, which provides a parsimonious approach to simulate and analyze hydraulic heads and surface water body–aquiferinteraction for linear aquifers (linear response of head to stresses). The solution of linear groundwater-flow problems usingeigenvalue techniques can be formulated with a simple explicit state equation whose structure shows that the surface waterbody–aquifer interaction phenomenon can be approached as the drainage of a number of independent linear reservoirs. Thehydraulic head field could be also approached by the summation of the head fields, estimated for those reservoirs, definedover the same domain set by the aquifer limits, where the hydraulic head field in each reservoir is proportional to a specificsurface (an eigenfunction of an eigenproblem, or an eigenvector in discrete cases). All the parameters and initial conditions ofeach linear reservoir can be mathematically defined in a univocal way from the calibrated finite difference model, preservingits characteristics (geometry, boundary conditions, hydrodynamic parameters (heterogeneity), and spatial distribution of thestresses). We also demonstrated that, in practical cases, an accurate solution can be obtained with a reduced number oflinear reservoirs. The reduced computational cost of these solutions can help to integrate the groundwater component withinconjunctive use management models. Conceptual approximation also facilitates understanding of the physical phenomenonand analysis of the factors that influence it. A simple synthetic aquifer has been employed to show how the conceptual modelcan be built for different spatial discretizations, the parameters required, and their influence on the simulation of hydraulichead fields and stream–aquifer flow exchange variables. A real-world case was also solved to test the accuracy of the proposedapproaches, by comparing its solution with that obtained using finite-difference MODFLOW code. Copyright  2011 JohnWiley & Sons, Ltd.
机译:在本文中,我们提出了一种可以从校准的有限差异地下室推导的概念数模型模型,为模拟和分析液压头和地表水体 - 含水层提供了一种解析的方法线性含水层的相互作用(头部对压力的线性响应)。线性地下水流动问题的解决方法特征值技术可以用简单的明确态等式配制,其结构显示地表水身体含水层相互作用现象可以接近多个独立线性储层的排水。这液压头领域也可以通过头部的总和,估计为那些储层,定义通过含水层限制的相同域,每个储存器中的液压头场与特定的液压头部成比例表面(在离散情况下,特征问题的特征函数或特征向量)。所有参数和初始条件每个线性储存器可以从校准的有限差模具,保留以单一的方式以单一的方式进行数学定义其特点(几何,边界条件,流体动力学参数(异质性)和空间分布强调)。我们还证明,在实际情况下,可以获得缩小数量的准确解决方案线性水库。这些解决方案的降低的计算成本可以有助于将地下水部件整合在内结合使用管理模式。概念近似还有助于了解物理现象影响其影响因素的分析。一款简单的合成含水层已被用于展示概念模型的方式可以构建不同的空间离散化,所需的参数,以及它们对液压仿真的影响头部字段和流含水层流量交换变量。还解决了真实的案例来测试提议的准确性通过将其解决方案与使用有限差分模块代码获得的解决方案进行比较。版权所有2011 JohnWiley&Sons,Ltd。

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