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Parameters Estimation and Prediction of Water Movement and Solute Transport in Layered, Variably Saturated Soils Using the Ensemble Kalman Filter

机译:使用Ensemble Kalman滤波器估计和预测分层,可变饱和土的水运动和溶质运输

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The parameters of water movement and solute transport models are essential for the accurate simulation of soil moisture and salinity, particularly for layered soils in field conditions. Parameter estimation can be achieved using the inverse modeling method. However, this type of method cannot fully consider the uncertainties of measurements, boundary conditions, and parameters, resulting in inaccurate estimations of parameters and predictions of state variables. The ensemble Kalman filter (EnKF) is well-suited to data assimilation and parameter prediction in Situations with large numbers of variables and uncertainties. Thus, in this study, the EnKF was used to estimate the parameters of water movement and solute transport in layered, variably saturated soils. Our results indicate that when used in conjunction with the HYDRUS-1D software (University of California Riverside, California, CA, USA) the EnKF effectively estimates parameters and predicts state variables for layered, variably saturated soils. The assimilation of factors such as the initial perturbation and ensemble size significantly affected in the simulated results. A proposed ensemble size range of 50–100 was used when applying the EnKF to the highly nonlinear hydrological models of the present study. Although the simulation results for moisture did not exhibit substantial improvement with the assimilation, the simulation of the salinity was significantly improved through the assimilation of the salinity and relative solutetransport parameters. Reducing the uncertainties in measured data can improve the goodness-of-fit in the application of the EnKF method. Sparse field condition observation data also benefited from the accurate measurement of state variables in the case of EnKF assimilation. However, the application of the EnKF algorithm for layered, variably saturated soils with hydrological models requires further study, because it is a challenging and highly nonlinear problem.
机译:水运动和溶质传输模型的参数对于精确模拟土壤水分和盐度是必不可少的,特别是对于现场条件的分层土壤。可以使用逆建模方法实现参数估计。然而,这种方法不能完全考虑测量,边界条件和参数的不确定性,从而导致对状态变量的参数和预测的不准确估计。合奏卡尔曼滤波器(ENKF)非常适合于具有大量变量和不确定性的情况下的数据同化和参数预测。因此,在本研究中,ENKF用于估计水运动的参数并在层状的可变饱和土中溶质输送。我们的结果表明,当与Hydrus-1D软件(加利福尼亚州河滨大学,加利福尼亚州河滨大学)结合使用时,ENKF有效地估计了分层,可变饱和土壤的态变量和预测状态变量。诸如初始扰动和集合尺寸等因素的同化在模拟结果中显着影响。在将ENKF应用于本研究的高度非线性水文模型时,使用了50-100的所提出的集合尺寸范围。虽然水分的仿真结果没有随着同化的显着提高,但通过同化盐度和相对溶解度参数的同化显着改善了盐度的模拟。降低测量数据中的不确定性可以提高enkf方法的适应性。稀疏场条件观测数据也受益于ENKF同化的情况下的状态变量的准确测量。然而,enkf算法用于分层,可变饱和土壤与水文模型需要进一步研究,因为它是一个具有挑战性和高度的非线性问题。

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