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Inverse Modeling of Soil Hydraulic Parameters Based on a Hybrid of Vector-Evaluated Genetic Algorithm and Particle Swarm Optimization

机译:矢量评估遗传算法与粒子群算法相结合的土壤水力参数反演

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The accurate estimation of soil hydraulic parameters ( θ s , α , n , and K s ) of the van Genuchten–Mualem model has attracted considerable attention. In this study, we proposed a new two-step inversion method, which first estimated the hydraulic parameter θ s using objective function by the final water content, and subsequently estimated the soil hydraulic parameters α , n , and K s , using a vector-evaluated genetic algorithm and particle swarm optimization (VEGA-PSO) method based on objective functions by cumulative infiltration and infiltration rate. The parameters were inversely estimated for four types of soils (sand, loam, silt, and clay) under an in silico experiment simulating the tension disc infiltration at three initial water content levels. The results indicated that the method is excellent and robust. Because the objective function had multilocal minima in a tiny range near the true values, inverse estimation of the hydraulic parameters was difficu however, the estimated soil water retention curves and hydraulic conductivity curves were nearly identical to the true curves. In addition, the proposed method was able to estimate the hydraulic parameters accurately despite substantial measurement errors in initial water content, final water content, and cumulative infiltration, proving that the method was feasible and practical for field application.
机译:van Genuchten-Mualem模型的土壤水力参数(θs,α,n和K s)的准确估算引起了广泛的关注。在这项研究中,我们提出了一种新的两步反演方法,该方法首先使用目标函数根据最终含水量估算水力参数θs,然后使用向量矢量估算土壤水力参数α,n和K s。评估了基于目标函数的遗传算法和粒子群优化(VEGA-PSO)方法的累积渗透率和渗透率。在计算机模拟实验中,模拟了三种初始水含量下张力盘的入渗,对四种类型的土壤(沙,壤土,淤泥和粘土)的参数进行了逆估计。结果表明,该方法具有很好的鲁棒性。由于目标函数在接近真实值的微小范围内具有多局部最小值,因此很难对水力参数进行逆估计;然而,估计的土壤保水曲线和水力传导率曲线几乎与真实曲线相同。此外,尽管初始含水量,最终含水量和累积入渗存在较大测量误差,但该方法仍能够准确估算水力参数,证明该方法对于现场应用是可行和实用的。

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