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Inverse Modelling to Estimate Soil Hydraulic Properties at the Field Scale

机译:逆向建模以估计田间尺度的土壤水力特性

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摘要

Field-scale estimation of soil hydraulic parameters is important for simulating water movement, particularly in the vadose zone. The accuracy of soil hydraulic parameters significantly affects the output of models using these parameters as input variables. A new approach for an inverse method, often referred to as inverse modelling, was presented to calibrate soil hydraulic parameters. The new method is based on the use of uniform design theory to generate uncertainty estimates of the soil hydraulic parameters. The uncalibrated and calibrated soil hydraulic parameters were evaluated by comparing the predicted and measured soil water contents using the HYDRUS-1D model. The results show that the calibrated soil hydraulic parameters that were inversely estimated by uniform design theory were accurate and reasonable. In addition, the results provided recommendations for improving the estimation of soil hydraulic parameters when there are no available observation data for calibrating and optimizing soil hydraulic parameters.
机译:土壤水力参数的现场尺度估计对于模拟水的运动非常重要,特别是在蒸发带。土壤水力参数的精度会显著影响使用这些参数作为输入变量的模型的输出。提出了一种反演方法的新方法,通常称为逆建模,用于校准土壤水力参数。新方法基于统一设计理论对土壤水力参数进行不确定性估计。通过使用HYDRUS-1D模型比较预测和测量的土壤含水量,对未校准和校准的土壤水力参数进行评估。结果表明:采用统一设计理论反演估计的标定土体水力参数准确合理;此外,研究结果为在没有可用观测数据用于校准和优化土壤水力参数的情况下改进土壤水力参数估计提供了建议。

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