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使用HYDRUS-1D模型对积水条件下原状黄土入渗的VG模型参数进行敏感性分析。

Sensitivity analysis of VG model parameters for infiltration in undisturbed loess under ponding conditions using the HYDRUS-1D model.

作者信息

Wang Xuejiu, Huang Zhiquan, Qin Hu, Dai Fuchu

机构信息

Henan Vocational College of Water Conservancy and Environment, Zhengzhou, 450008, China.

College of Geosciences and Engineering, North China University of Water Resources and Electric Power, Zhengzhou, 450046, China.

出版信息

Sci Rep. 2025 Jul 12;15(1):25204. doi: 10.1038/s41598-025-11058-y.

Abstract

It is difficult for remolded loess to reproduce the infiltration law of water in natural loess, resulting in inaccurate parameters of the Van-Genuchten model (VG model) obtained by inversion, which subsequently affects the changes in the moisture field during slope stability numerical simulations. To address this gap, a large-scale undisturbed loess soil column with a diameter of 60 cm and a height of 100 cm was artificially excavated for a water infiltration test under ponding conditions. Based on the test results, the VG model parameters were inverted by the Hydrus-1D software. The simulation accuracy was evaluated using the root mean square error (RMSE) and the Nash-Sutcliffe efficiency coefficient (NSE). Based on the inverted VG model parameters, the single-factor perturbation method was employed to calculate different VG model parameters under a disturbance amplitude of ± 20%. The numerical simulations were carried out to investigate the wetting front arrival times at different depths under varying disturbance parameters. Finally, the sensitivity of soil water characteristic parameters was analyzed. The results indicated that the measured water contents in the column closely matched the simulated values, with minimal errors, as evidenced by the RMSE ranging from 0.010 to 0.019. Except for the NSE values at 10 cm and 20 cm depths, which were below 0.900, all other depths exhibited NSE values greater than 0.900, indicating satisfactory simulation performance. The influence of soil water characteristic parameters on simulation results was θs > ks > n > α > θr. The disturbances in θs and α were negatively correlated, while disturbances in ks, n, and θr were positively correlated. Parameter disturbances less influenced the infiltration laws of water in shallow soils. However, as soil column depth increased, sensitivity to parameter changes gradually increased, leading to a greater impact on simulation results. The research findings provide technical support for evaluating and preventing water-induced landslide hazards.

摘要

重塑黄土难以再现天然黄土中的水分入渗规律,导致反演得到的Van - Genuchten模型(VG模型)参数不准确,进而影响边坡稳定性数值模拟过程中水分场的变化。为弥补这一空白,人工挖掘了直径60 cm、高100 cm的大型原状黄土土柱,进行积水条件下的水分入渗试验。基于试验结果,利用Hydrus - 1D软件反演VG模型参数。采用均方根误差(RMSE)和纳什 - 萨特克利夫效率系数(NSE)评估模拟精度。基于反演得到的VG模型参数,采用单因素扰动法计算扰动幅度为±20%时不同的VG模型参数。进行数值模拟以研究不同扰动参数下不同深度处湿润锋到达时间。最后,分析了土壤水分特征参数的敏感性。结果表明,土柱中实测含水量与模拟值紧密匹配,误差极小,RMSE范围为0.010至0.019。除10 cm和20 cm深度处的NSE值低于0.900外,其他所有深度的NSE值均大于0.900,表明模拟性能良好。土壤水分特征参数对模拟结果的影响为θs>ks>n>α>θr。θs和α的扰动呈负相关,而ks、n和θr的扰动呈正相关。参数扰动对浅层土壤中水分入渗规律的影响较小。然而,随着土柱深度增加,对参数变化的敏感性逐渐增大,对模拟结果的影响也更大。研究结果为评估和预防水致滑坡灾害提供了技术支持。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5258/12255665/7ca95b09e5cf/41598_2025_11058_Fig1_HTML.jpg

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