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Inverse modelling in estimating soil hydraulic functions: a Genetic Algorithm approach

机译:估算土壤水力函数的逆模型:遗传算法

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The practical application of simulationmodels in the field is sometimes hindered by the difficulty of deriving the soilhydraulic properties of the study area. The procedure so-called inversemodelling has been investigated in many studies to address the problem wheremost of the studies were limited to hypothetical soil profile and soil coresamples in the laboratory. Often, the numerical approach called forward-backwardsimulation is employed to generate synthetic data then added with random errorsto mimic the real-world condition. Inverse modelling is used to backtrack theexpected values of the parameters. This study explored the potential of aGenetic Algorithm (GA) to estimate inversely the soil hydraulic functions in theunsaturated zone. Lysimeter data from a wheat experiment in India were used inthe analysis. Two cases were considered: (1) a numerical case where theforward-backward approach was employed and (2) the experimental case where thereal data from the lysimeter experiment were used. Concurrently, the use of soilwater, evapotranspiration (ET) and the combination of both were investigated ascriteria in the inverse modelling. Results showed that using soil water as acriterion provides more accurate parameter estimates than using ET. However,from a practical point of view, ET is more attractive as it can be obtained withreasonable accuracy on a regional scale from remote sensing observations. Theexperimental study proved that the forward-backward approach does not take intoaccount the effects of model errors. The formulation of the problem is found tobe critical for a successful parameter estimation. The sensitivity of parametersto the objective function and their zone of influence in the soil column aremajor determinants in the solution. Generally, their effects sometimes lead tonon-uniqueness in the solution but to some extent are partly handled by GA.Overall, it was concluded that the GA approach is promising to the inverseproblem in the unsaturated zone. style="line-height: 20px;">Keywords. Genetic Algorithm, inverse modelling, Mualem-Van Genuchten parameters, unsaturated zone, evapotranspiration, soil water
机译:模拟模型在该领域的实际应用有时会因难以获得研究区域的土壤水力特性而受到阻碍。在许多研究中都对所谓的逆建模过程进行了研究,以解决大多数研究仅限于实验室中假设的土壤剖面和土壤岩心样品的问题。通常,采用称为前向后向仿真的数值方法来生成综合数据,然后将其添加随机误差以模拟现实情况。逆建模用于回溯参数的预期值。这项研究探索了遗传算法(GA)潜在地反演非饱和带土壤水力功能的潜力。分析中使用了来自印度小麦实验的蒸渗仪数据。考虑了两种情况:(1)采用向前-向后方法的数值情况;(2)使用来自溶渗仪实验的实际数据的实验情况。同时,在逆模型中,研究了土壤水,蒸散量(ET)的使用以及两者的组合。结果表明,与使用ET相比,使用土壤水作为指标可以提供更准确的参数估计。但是,从实际的角度来看,ET更具吸引力,因为它可以从遥感观测结果中以合理的精度在区域范围内获得。实验研究证明,前后进近方法没有考虑模型误差的影响。发现问题的提出对于成功的参数估计至关重要。参数对目标函数的敏感性及其在土柱中的影响区域是解决方案中的主要决定因素。通常,它们的影响有时会导致解决方案中的非唯一性,但在某种程度上是由遗传算法处理的。总体而言,结论是遗传算法的方法有望解决非饱和区中的逆问题。 style =“ line-height:20px;“> 关键字。 遗传算法,逆模型,Mualem-Van Genuchten参数,非饱和带,蒸散量,土壤水分

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